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Subfamily?
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<taxonomicName id="BAFBD0E6FF89360D34F1F958FD93E890" authority="Jell, 1969" authorityName="Jell" authorityYear="1969" box="[254,602,1734,1763]" family="Disphyllidae" kingdom="Animalia" order="Stauriida" pageId="5" pageNumber="552" rank="subFamily" subFamily="Paradisphyllinae">
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Paradisphyllinae
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<bibRefCitation id="196AD694FF89360D35D1F958FD93E890" author="Jell, J. S." box="[478,602,1734,1763]" pageId="5" pageNumber="552" pagination="50 - 73" refId="ref7928" refString="Jell, J. S. 1969. Septal microstructure and classification of the Phillipsastraeidae. In: K. S. W. Campbell (ed.), Stratigraphy and Palaeontology. Essays in Honour of Dorothy Hill, 50 - 73. Australian National University Press, Canberra." type="book chapter" year="1969">Jell, 1969</bibRefCitation>
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<paragraph id="7D44AB65FF89360D3469F96CFAC4ECB2" blockId="5.[102,775,1698,2026]" lastBlockId="5.[812,1485,232,705]" pageId="5" pageNumber="552">
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<emphasis id="4F8F7777FF89360D3469F96CFF01E979" box="[102,200,1778,1802]" italics="true" pageId="5" pageNumber="552">Remarks</emphasis>
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.—The Paradisphyllinae are a group of predominantly Lower Devonian corals which include genera characterized by fine monacanth septal trabeculae, arranged in a fan like system because of their slightly everted calices (
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<bibRefCitation id="196AD694FF89360D36D5F8CCFF6BE9F9" author="Hill, D." pageId="5" pageNumber="552" pagination="1 - 378" refId="ref7808" refString="Hill, D. 1981. Coelenterata. Supplement I. Rugosa and Tabulata. In: C. Teichert (ed.), Treatise on Invertebrate Paleontology, Part F. 1, I - IX + 1 - 378. Boulder, Colorado." type="book chapter" year="1981">Hill 1981</bibRefCitation>
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: F271). The subfamily is further defined as a group of genera with fusiform or carinate septa and steeply arched dissepimentarial floors (
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<bibRefCitation id="196AD694FF89360D3571F82CFDD5E9B9" author="Jell, J. S." box="[382,540,1970,1994]" pageId="5" pageNumber="552" pagination="50 - 73" refId="ref7928" refString="Jell, J. S. 1969. Septal microstructure and classification of the Phillipsastraeidae. In: K. S. W. Campbell (ed.), Stratigraphy and Palaeontology. Essays in Honour of Dorothy Hill, 50 - 73. Australian National University Press, Canberra." type="book chapter" year="1969">Jell 1969: 67</bibRefCitation>
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) and was separated from the
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<taxonomicName id="BAFBD0E6FF89360D34D9F84CFEACE999" authorityName="Hill" authorityYear="1939" box="[214,357,2002,2026]" class="Anthozoa" family="Disphyllidae" higherTaxonomySource="GBIF" kingdom="Animalia" pageId="5" pageNumber="552" phylum="Cnidaria" rank="family">Disphyllidae</taxonomicName>
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because of their upward spreading trabeculae. The closely related Hexagonariinae are separated by their arrangement of monacanth trabeculae, which show a half−fan in longitudinal section and a different calice morphology, which is not strongly evert. The taxonomic value of external− or calice−forms of corals is generally regarded as not very high, and the proposed separation of a subfamily based on differences in external morphology is therefore questionable (
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<bibRefCitation id="196AD694FF89360D37C0FE56FBACEF92" author="Sorauf, J. E." box="[975,1125,456,481]" pageId="5" pageNumber="552" pagination="323 - 338" refId="ref8789" refString="Sorauf, J. E. 1994. Hexagonaria and the Hexagonariinae (Disphyllidae, Rugosa): Devoniancolonialcorals. In: E. Landing (ed.), Studiesinstratigraphy and paleontology in honor of Donald W. Fisher, Bulletin of the New York State Museum 481: 323 - 338." type="journal article" year="1994">Sorauf 1994</bibRefCitation>
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). Although carinae are highly variable in the Paradisphyllinae they are usually developed as yardarm−like structures. Some species show only slightly carinate or peripherally incomplete septa of swollen trabeculae, which may give an impression of constituting a string of pearls. Athorough revision of the Hexagonariinae and dis − cussion of their separation from the Paradisphyllinae has been given recently by
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<bibRefCitation id="196AD694FF89360D303EFD36FAC3ECB2" author="Sorauf, J. E." box="[1073,1290,680,705]" pageId="5" pageNumber="552" pagination="323 - 338" refId="ref8789" refString="Sorauf, J. E. 1994. Hexagonaria and the Hexagonariinae (Disphyllidae, Rugosa): Devoniancolonialcorals. In: E. Landing (ed.), Studiesinstratigraphy and paleontology in honor of Donald W. Fisher, Bulletin of the New York State Museum 481: 323 - 338." type="journal article" year="1994">Sorauf (1994: 333)</bibRefCitation>
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||||
.
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||||
</paragraph>
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<paragraph id="7D44AB65FF89360D3723FD4AFCAEED58" blockId="5.[812,1485,723,811]" pageId="5" pageNumber="552">
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<emphasis id="4F8F7777FF89360D3723FD4AFC79EC98" box="[812,944,724,747]" italics="true" pageId="5" pageNumber="552">Occurrence</emphasis>
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.—Widely distributed in the Upper Silurian to Middle Devonian of
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<collectingCountry id="05ECEBF5FF89360D3019FD6DFBB6ED78" box="[1046,1151,755,779]" name="Australia" pageId="5" pageNumber="552">Australia</collectingCountry>
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, Western North America, and Asia.
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</paragraph>
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</treatment>
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<taxonomicName id="BAFBD0E6FF8A360E3723F81BFA95E9D1" authorityName="gen. et" authorityYear="2003" box="[812,1372,1925,1954]" class="Anthozoa" family="Disphyllidae" genus="Cantabriastraea" higherTaxonomySource="GBIF" kingdom="Animalia" order="Stauriida" pageId="6" pageNumber="555" phylum="Cnidaria" rank="species" species="cantabrica" status="gen. et">
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<emphasis id="4F8F7777FF8A360E3723F81BFB5AE9D1" box="[812,1171,1925,1954]" italics="true" pageId="6" pageNumber="553">Cantabriastraea cantabrica</emphasis>
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sp. nov.
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</taxonomicName>
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</paragraph>
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<figureCitation id="E5C0B7E0FF8A360E3723F833FC54E9B0" box="[812,925,1965,1987]" captionStart="Fig" captionStartId="5.[102,135,1320,1339]" captionTargetBox="[102,775,228,1277]" captionTargetId="figure-576@5.[102,776,228,1277]" captionTargetPageId="5" captionText="Fig. 6. Cantabriastraea cantabrica gen. et sp. nov. A. Cross section of holotype DPO 14780. B. Longitudinal section of the same. Both × 2. Specimen from the Upper Emsian of Colle." pageId="6" pageNumber="553">Figs. 6A, B</figureCitation>
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,
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<figureCitation id="E5C0B7E0FF8A360E37A8F833FC2DE9B0" box="[935,996,1965,1987]" captionStart="Fig" captionStartId="6.[812,845,1576,1595]" captionTargetBox="[813,1484,234,1546]" captionTargetId="figure-543@6.[813,1485,234,1546]" captionTargetPageId="6" captionText="Fig. 7. Cantabriastraea cantabrica gen. et sp. nov. A. Colony DPO 14811 consisting of a large protocorallite disrupted by nonparricidal, marginal increase in distal view (A1); septa appear as broad and flat ridges which are stronglyretiformtowardstheperiphery.Undersideofthesamecolony(A2), partly encrusted by Aulopora sp.; × 2. B. Colony DPO 14813. B1. Colony underside showing a single protocorallite turned to the left. B2. Upper surface of the same colony; × 1. All specimens from the Upper Emsian of Colle." pageId="6" pageNumber="553">7A–D</figureCitation>
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,
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<figureCitation id="E5C0B7E0FF8A360E37E1F833FBEAE9B0" box="[1006,1059,1965,1987]" captionStart="Fig" captionStartId="8.[102,135,1813,1832]" captionText="Fig. 8. Cantabriastraea cantabrica gen. et sp. nov. A. Cross section of colony DPO 14789 with medium sized corallites. B. Cross section of colony DPO 1790. Corallites are very large and show highly variable development of carinate septa. C. Protocorallite of colony DPO 14788. D. Cross section of small colony DPO 14783. Septa are strongly thickened especially at dissepimentarium/tabularium boundary. E. Longitudinal section DPO 14786. Note strongly arched series of dissepiment−layers and convex tabulae. F. Cross section of colony−fragment DPO 14830 with development of juvenile corallites by marginal increase on lower right side of large protocorallite. G. Longitudinal section DPO 14790. H. Cross section of colony DPO 14787, consisting of a large protocorallite and four juvenile offsets developed by marginal increase. Undilated major septa do not reach to corallite axis. I. Longitudinal section of colony DPO 14787. J. Corallites of colony DPO 14790 (compare Fig. 8B), with strongly carinate septa breaking down into discrete trabeculae, becoming retiform. A–C, E–I, × 2; D × 3; J × 2.5. All specimens from the Upper Emsian of Colle." pageId="6" pageNumber="553">8A–J</figureCitation>
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,
|
||||
<figureCitation id="E5C0B7E0FF8A360E3023F833FBA7E9B0" box="[1068,1134,1965,1987]" captionStart="Fig" captionStartId="8.[102,135,731,750]" captionTargetBox="[556,1486,229,1340]" captionTargetId="figure-389@8.[556,1486,229,1340]" captionTargetPageId="8" captionText="Fig. 9. A. Cantabriastraea cantabrica gen. et sp. nov., specimen DPO 14789. A1. Cross sec− tion of tabularium and inner dissepimentarium. Trabeculae are oriented perpendicular to the rows of dissepiments; × 15. A2. Detail of A1; trabeculae intercalate between existing ones or bifurcate; × 20. A3. Septa in cross section with strong dilations in inner dissepimentarium caused by thickening of trabeculae. Towards the periphery (left side) septa become irregular carinate and may split into discrete trabeculae; × 24. B, C. Tabulophyllum bonarense sp. nov. B. Wall of corallite DPO 14673 in cross sec− tion. Thickenings of wall and lonsdaleoid dis− sepiments show a fibrous structure caused by thickened septal bases; × 24. C. Thin septa of corallite DPO 14686 (compare with Fig. 4G) inserting on lonsdaleoid dissepiments (dark lines in lower part of picture). Central part to− wards the axis (top of picture) is strongly af− fected by cement; × 24. All specimens from the Upper Emsian of Colle." pageId="6" pageNumber="553">9 A–C</figureCitation>
|
||||
.
|
||||
</paragraph>
|
||||
</subSubSection>
|
||||
<subSubSection id="35E1F8EEFF8A36013723F84DFD50E89D" lastPageId="9" lastPageNumber="556" pageId="6" pageNumber="553" type="materials_examined">
|
||||
<paragraph id="7D44AB65FF8A36003723F84DFBB8EBDD" blockId="6.[812,1111,2003,2025]" lastBlockId="8.[59,1485,1395,1795]" lastPageId="8" lastPageNumber="555" pageId="6" pageNumber="553">
|
||||
<materialsCitation id="CD93A138FF8A36003723F84DFBB8EBDD" county="Bonar" lastPageId="8" lastPageNumber="555" latitude="42.844997" location="Colle" longLatPrecision="19" longitude="1.5602777" municipality="Tabulae" pageId="6" pageNumber="553" specimenCount="1" typeStatus="holotype">
|
||||
<emphasis id="4F8F7777FF8A360E3723F84DFC4DE99A" box="[812,900,2003,2025]" italics="true" pageId="6" pageNumber="553">
|
||||
<typeStatus id="A24015C7FF8A360E3723F84DFC4DE99A" box="[812,900,2003,2025]" pageId="6" pageNumber="553" type="holotype">Holotype</typeStatus>
|
||||
</emphasis>
|
||||
: DPO 14780 (
|
||||
<figureCitation id="E5C0B7E0FF8A360E301FF84DFB82E99A" box="[1040,1099,2003,2025]" captionStart="Fig" captionStartId="5.[102,135,1320,1339]" captionTargetBox="[102,775,228,1277]" captionTargetId="figure-576@5.[102,776,228,1277]" captionTargetPageId="5" captionText="Fig. 6. Cantabriastraea cantabrica gen. et sp. nov. A. Cross section of holotype DPO 14780. B. Longitudinal section of the same. Both × 2. Specimen from the Upper Emsian of Colle." pageId="6" pageNumber="553">Fig. 6</figureCitation>
|
||||
).
|
||||
<emphasis id="4F8F7777FF8436003469FAEAFF2AEBFA" box="[102,227,1395,1417]" italics="true" pageId="8" pageNumber="555">Type locality</emphasis>
|
||||
:
|
||||
<location id="7824FDBEFF84360034FEFAEDFEEEEBFA" LSID="urn:lsid:plazi:treatment:F5521A73FF8A36013723F81BFD50E89D:7824FDBEFF84360034FEFAEDFEEEEBFA" box="[241,295,1395,1417]" county="Bonar" latitude="42.844997" longLatPrecision="19" longitude="1.5602777" municipality="Tabulae" name="Colle" pageId="8" pageNumber="555">Colle</location>
|
||||
, ca.
|
||||
<locationDeviation id="6CF6B247FF843600355CFAEDFDC1EBFA" box="[339,520,1395,1417]" location="Bonar" pageId="8" pageNumber="555">
|
||||
<quantity id="BA030680FF843600355CFAEDFE4CEBFA" box="[339,389,1395,1417]" metricMagnitude="3" metricUnit="m" metricValue="5.0" pageId="8" pageNumber="555" unit="km" value="5.0">5 km</quantity>
|
||||
SE of Boñar
|
||||
</locationDeviation>
|
||||
,
|
||||
<location id="7824FDBEFF843600361DFAEDFD6BEBFA" LSID="urn:lsid:plazi:treatment:F5521A73FF8A36013723F81BFD50E89D:7824FDBEFF843600361DFAEDFD6BEBFA" box="[530,674,1395,1417]" county="Bonar" latitude="42.844997" longLatPrecision="19" longitude="1.5602777" municipality="Tabulae" name="Province Leon" pageId="8" pageNumber="555">Province León</location>
|
||||
;
|
||||
<location id="7824FDBEFF84360036A2FAEDFD15EBFA" LSID="urn:lsid:plazi:treatment:F5521A73FF8A36013723F81BFD50E89D:7824FDBEFF84360036A2FAEDFD15EBFA" box="[685,732,1395,1417]" county="Bonar" latitude="42.844997" longLatPrecision="19" longitude="1.5602777" municipality="Tabulae" name="Hoja" pageId="8" pageNumber="555">Hoja</location>
|
||||
104 3.5–
|
||||
<quantity id="BA030680FF8436003750FAEBFC6EEBFE" box="[863,935,1397,1421]" metricMagnitude="-3" metricUnit="m" metricValue="5.0" pageId="8" pageNumber="555" unit="mm" value="5.0">5 mm</quantity>
|
||||
.
|
||||
<collectingMunicipality id="9D20311FFF84360037B8FAEBFBD8EBFE" box="[951,1041,1397,1421]" pageId="8" pageNumber="555">Tabulae</collectingMunicipality>
|
||||
complete and slightly arched (13–18 (
|
||||
<collectingCounty id="9425D3E9FF8436003462FA11FF62EBD6" box="[109,171,1423,1445]" pageId="8" pageNumber="555">Boñar</collectingCounty>
|
||||
),
|
||||
<geoCoordinate id="18CFCDA2FF84360034B2FA11FEE8EBD6" box="[189,289,1423,1445]" degrees="1" direction="east" minutes="33" orientation="longitude" pageId="8" pageNumber="555" precision="15" seconds="37" value="1.5602777">1°33’37’’E</geoCoordinate>
|
||||
/
|
||||
<geoCoordinate id="18CFCDA2FF8436003525FA11FE61EBD6" box="[298,424,1423,1445]" degrees="42" direction="north" minutes="50" orientation="latitude" pageId="8" pageNumber="555" precision="15" seconds="42" value="42.844997">42°50’42’’N</geoCoordinate>
|
||||
. tabulae per
|
||||
<quantity id="BA030680FF84360037A0FA08FC39EBDD" box="[943,1008,1430,1454]" metricMagnitude="-3" metricUnit="m" metricValue="5.0" pageId="8" pageNumber="555" unit="mm" value="5.0">5 mm</quantity>
|
||||
vertically).
|
||||
</materialsCitation>
|
||||
</paragraph>
|
||||
<caption id="2984FBEDFF8436003469FD45FEF7EB49" pageId="8" pageNumber="555" startId="8.[102,135,731,750]" targetBox="[556,1486,229,1340]" targetPageId="8" targetType="figure">
|
||||
<paragraph id="7D44AB65FF8436003469FD45FDC3EC9C" blockId="8.[102,524,731,1339]" box="[102,522,731,751]" pageId="8" pageNumber="555">
|
||||
Fig. 9.
|
||||
<emphasis id="4F8F7777FF84360034A6FD45FF70EC9D" bold="true" box="[169,185,731,750]" pageId="8" pageNumber="555">A</emphasis>
|
||||
.
|
||||
<taxonomicName id="BAFBD0E6FF84360034C8FD45FDC3EC9C" authorityName="gen. et" authorityYear="2003" box="[199,522,731,751]" class="Anthozoa" family="Disphyllidae" genus="Cantabriastraea" higherTaxonomySource="GBIF" kingdom="Animalia" pageId="8" pageNumber="555" phylum="Cnidaria" rank="species" species="cantabrica" status="gen. et">
|
||||
<emphasis id="4F8F7777FF84360034C8FD45FE0CEC9D" box="[199,453,731,750]" italics="true" pageId="8" pageNumber="555">Cantabriastraea cantabrica</emphasis>
|
||||
gen. et
|
||||
</taxonomicName>
|
||||
</paragraph>
|
||||
<paragraph id="7D44AB65FF8436003469FD66FDC5ED55" blockId="8.[102,524,731,1339]" pageId="8" pageNumber="555">
|
||||
sp. nov., specimen DPO 14789. A
|
||||
<subScript id="E17FA920FF8436003595FC9EFE6BED7D" attach="left" box="[410,418,768,782]" fontSize="6" pageId="8" pageNumber="555">1</subScript>
|
||||
. Cross section of tabularium and inner dissepimentarium.
|
||||
</paragraph>
|
||||
<paragraph id="7D44AB65FF8436003469FCB1FDC3ED2C" blockId="8.[102,524,731,1339]" pageId="8" pageNumber="555">
|
||||
Trabeculae are oriented perpendicular to the rows of dissepiments; × 15. A
|
||||
<subScript id="E17FA920FF8436003571FCCAFE4FED11" attach="left" box="[382,390,852,866]" fontSize="6" pageId="8" pageNumber="555">2</subScript>
|
||||
. Detail of A
|
||||
<subScript id="E17FA920FF84360035F3FCCAFDCDED11" attach="left" box="[508,516,852,866]" fontSize="6" pageId="8" pageNumber="555">1</subScript>
|
||||
;
|
||||
</paragraph>
|
||||
<paragraph id="7D44AB65FF8436003469FCF9FDC5EA75" blockId="8.[102,524,731,1339]" pageId="8" pageNumber="555">
|
||||
trabeculae intercalate between existing ones or bifurcate; × 20. A
|
||||
<subScript id="E17FA920FF8436003508FC12FEC6EDE9" attach="right" box="[263,271,908,922]" fontSize="6" pageId="8" pageNumber="555">3</subScript>
|
||||
. Septa in cross section with strong dilations in inner dissepimentarium caused by thickening of trabeculae. Towards the periphery (left side) septa become irregular carinate and may split into discrete trabeculae;
|
||||
</paragraph>
|
||||
<paragraph id="7D44AB65FF8436003469FB8EFDC5EA50" blockId="8.[102,524,731,1339]" box="[102,524,1039,1059]" pageId="8" pageNumber="555">
|
||||
× 24.
|
||||
<emphasis id="4F8F7777FF8436003495FB91FF60EA51" bold="true" box="[154,169,1039,1058]" pageId="8" pageNumber="555">B</emphasis>
|
||||
,
|
||||
<emphasis id="4F8F7777FF84360034BAFB91FF0CEA51" bold="true" box="[181,197,1039,1058]" pageId="8" pageNumber="555">C</emphasis>
|
||||
.
|
||||
<taxonomicName id="BAFBD0E6FF84360034DEFB91FE74EA51" authorityName="Schröder & Soto" authorityYear="2003" box="[209,445,1039,1058]" class="Anthozoa" family="Chonophyllidae" genus="Tabulophyllum" higherTaxonomySource="GBIF" kingdom="Animalia" pageId="8" pageNumber="555" phylum="Cnidaria" rank="species" species="bonarense" status="sp. nov.">
|
||||
<emphasis id="4F8F7777FF84360034DEFB91FE74EA51" box="[209,445,1039,1058]" italics="true" pageId="8" pageNumber="555">Tabulophyllum bonarense</emphasis>
|
||||
</taxonomicName>
|
||||
<taxonomicNameLabel id="54BCCA0CFF84360035CCFB8EFDC5EA50" box="[451,524,1040,1059]" pageId="8" pageNumber="555" rank="species">sp. nov.</taxonomicNameLabel>
|
||||
</paragraph>
|
||||
<paragraph id="7D44AB65FF8436003469FBB5FDC3EADD" blockId="8.[102,524,731,1339]" pageId="8" pageNumber="555">
|
||||
<emphasis id="4F8F7777FF8436003469FBB5FFBCEA4D" bold="true" box="[102,117,1067,1086]" pageId="8" pageNumber="555">B</emphasis>
|
||||
. Wall of corallite DPO 14673 in cross section. Thickenings of wall and lonsdaleoid dissepiments show a fibrous structure caused by thickened septal bases; × 24.
|
||||
<emphasis id="4F8F7777FF843600357BFBE1FE4DEAE1" bold="true" box="[372,388,1151,1170]" pageId="8" pageNumber="555">C</emphasis>
|
||||
. Thin septa of corallite DPO 14686 (compare with Fig. 4G)
|
||||
</paragraph>
|
||||
<paragraph id="7D44AB65FF8436003469FB29FDC2EB6D" blockId="8.[102,524,731,1339]" pageId="8" pageNumber="555">inserting on lonsdaleoid dissepiments (dark lines in lower part of picture). Central part towards the axis (top of picture) is strongly affected by cement; × 24. All specimens from the</paragraph>
|
||||
<paragraph id="7D44AB65FF8436003469FAB6FEF7EB49" blockId="8.[102,524,731,1339]" box="[102,318,1319,1339]" pageId="8" pageNumber="555">Upper Emsian of Colle.</paragraph>
|
||||
</caption>
|
||||
<paragraph id="7D44AB65FF8436003469FA29FCCFEBBF" blockId="8.[59,1485,1395,1795]" box="[102,774,1462,1484]" pageId="8" pageNumber="555">
|
||||
<emphasis id="4F8F7777FF8436003469FA29FF2DEBBF" box="[102,228,1462,1484]" italics="true" pageId="8" pageNumber="555">Type horizon</emphasis>
|
||||
: Lower Devonian, Emsian, La Vid Group, upper part of
|
||||
</paragraph>
|
||||
<paragraph id="7D44AB65FF8436003723FA58FCCFEB9B" blockId="8.[59,1485,1395,1795]" pageId="8" pageNumber="555">
|
||||
<emphasis id="4F8F7777FF8436003723FA58FC64EBAE" box="[812,941,1478,1501]" italics="true" pageId="8" pageNumber="555">Description</emphasis>
|
||||
.—Coralla are typically small, with a diameter of the Valporquero Formation (COL A−1) and lowermost part of the
|
||||
</paragraph>
|
||||
<paragraph id="7D44AB65FF8436013469FA70FD62E8B2" blockId="8.[59,1485,1395,1795]" lastBlockId="9.[102,775,232,1729]" lastPageId="9" lastPageNumber="556" pageId="8" pageNumber="555">
|
||||
Coladilla Formation (COL B−3).
|
||||
<quantity id="BA030680FF8436003723FA78FC49EB8E" box="[812,896,1510,1534]" metricMagnitude="-2" metricUnit="m" metricValue="6.0" metricValueMax="7.0" metricValueMin="5.0" pageId="8" pageNumber="555" unit="cm" value="6.0" valueMax="7.0" valueMin="5.0">5–7 cm</quantity>
|
||||
at a maximum height of
|
||||
<quantity id="BA030680FF8436003094FA78FB1AEB8E" box="[1179,1235,1510,1534]" metricMagnitude="-2" metricUnit="m" metricValue="5.0" pageId="8" pageNumber="555" unit="cm" value="5.0">5 cm</quantity>
|
||||
and have a distinctive
|
||||
<emphasis id="4F8F7777FF8436003469F98FFE8AE855" box="[102,323,1552,1574]" italics="true" pageId="8" pageNumber="555">Derivation of the name</emphasis>
|
||||
: The name derives from the Cantabrian Moun− growth form of a flat cake. Small colonies are mushroom tains. shaped and comprise only a few corallites (
|
||||
<figureCitation id="E5C0B7E0FF8436003106F9B6FA97E833" box="[1289,1374,1576,1600]" captionStart="Fig" captionStartId="6.[812,845,1576,1595]" captionTargetBox="[813,1484,234,1546]" captionTargetId="figure-543@6.[813,1485,234,1546]" captionTargetPageId="6" captionText="Fig. 7. Cantabriastraea cantabrica gen. et sp. nov. A. Colony DPO 14811 consisting of a large protocorallite disrupted by nonparricidal, marginal increase in distal view (A1); septa appear as broad and flat ridges which are stronglyretiformtowardstheperiphery.Undersideofthesamecolony(A2), partly encrusted by Aulopora sp.; × 2. B. Colony DPO 14813. B1. Colony underside showing a single protocorallite turned to the left. B2. Upper surface of the same colony; × 1. All specimens from the Upper Emsian of Colle." pageId="8" pageNumber="555">Fig. 7C</figureCitation>
|
||||
), whereas
|
||||
<emphasis id="4F8F7777FF8436003469F9D0FF0EE810" box="[102,199,1614,1635]" italics="true" pageId="8" pageNumber="555">
|
||||
<typeStatus id="A24015C7FF8436003469F9D0FF0EE810" box="[102,199,1614,1635]" pageId="8" pageNumber="555" type="paratype">Paratypes</typeStatus>
|
||||
</emphasis>
|
||||
:
|
||||
<specimenCount id="6BFD60ECFF84360034DAF9D0FE93E817" box="[213,346,1614,1636]" count="34" pageId="8" pageNumber="555" type="generic">34 specimens</specimenCount>
|
||||
, DPO 14781–14804, 14809–14814, 14828– adultcoloniestypicallyhaveaslightlydomedsurface.Growth 14830. starts with the development of a single, cylindrical
|
||||
<emphasis id="4F8F7777FF8436003469F910FF11E8D6" box="[102,216,1678,1701]" italics="true" pageId="8" pageNumber="555">protoDiagnosis</emphasis>
|
||||
.—Type species of
|
||||
<taxonomicName id="BAFBD0E6FF84360035BDF910FDA2E8D5" authorityName="Schroeder & Soto" authorityYear="2003" box="[434,619,1678,1702]" class="Anthozoa" family="Disphyllidae" genus="Cantabriastraea" higherTaxonomySource="GBIF" kingdom="Animalia" pageId="8" pageNumber="555" phylum="Cnidaria" rank="genus">
|
||||
<emphasis id="4F8F7777FF84360035BDF910FDA2E8D5" box="[434,619,1678,1702]" italics="true" pageId="8" pageNumber="555">Cantabriastraea</emphasis>
|
||||
</taxonomicName>
|
||||
with corallite corallite, reaching a maximum diameter of
|
||||
<quantity id="BA030680FF8436003115F915FA9DE8D0" box="[1306,1364,1675,1699]" metricMagnitude="-2" metricUnit="m" metricValue="2.0" pageId="8" pageNumber="555" unit="cm" value="2.0">2 cm</quantity>
|
||||
(
|
||||
<figureCitation id="E5C0B7E0FF8436003169F915FA09E8D0" box="[1382,1472,1675,1699]" captionStart="Fig" captionStartId="8.[102,135,1813,1832]" captionText="Fig. 8. Cantabriastraea cantabrica gen. et sp. nov. A. Cross section of colony DPO 14789 with medium sized corallites. B. Cross section of colony DPO 1790. Corallites are very large and show highly variable development of carinate septa. C. Protocorallite of colony DPO 14788. D. Cross section of small colony DPO 14783. Septa are strongly thickened especially at dissepimentarium/tabularium boundary. E. Longitudinal section DPO 14786. Note strongly arched series of dissepiment−layers and convex tabulae. F. Cross section of colony−fragment DPO 14830 with development of juvenile corallites by marginal increase on lower right side of large protocorallite. G. Longitudinal section DPO 14790. H. Cross section of colony DPO 14787, consisting of a large protocorallite and four juvenile offsets developed by marginal increase. Undilated major septa do not reach to corallite axis. I. Longitudinal section of colony DPO 14787. J. Corallites of colony DPO 14790 (compare Fig. 8B), with strongly carinate septa breaking down into discrete trabeculae, becoming retiform. A–C, E–I, × 2; D × 3; J × 2.5. All specimens from the Upper Emsian of Colle." pageId="8" pageNumber="555">Fig. 8C</figureCitation>
|
||||
). diameter of
|
||||
<quantity id="BA030680FF84360034E0F930FE92E8B6" box="[239,347,1710,1734]" metricMagnitude="-2" metricUnit="m" metricValue="1.05" metricValueMax="1.3" metricValueMin="0.8" pageId="8" pageNumber="555" unit="mm" value="10.5" valueMax="13.0" valueMin="8.0">8–13 mm</quantity>
|
||||
and 19–24 major septa, which do not This corallite is increasingly replaced by offsets developed by reach the corallite axis. Diameter of tabularium ranges from nonparricidal, marginal increase (
|
||||
<figureCitation id="E5C0B7E0FF8436003094F953FAC5E895" box="[1179,1292,1741,1766]" captionStart="Fig" captionStartId="8.[102,135,1813,1832]" captionText="Fig. 8. Cantabriastraea cantabrica gen. et sp. nov. A. Cross section of colony DPO 14789 with medium sized corallites. B. Cross section of colony DPO 1790. Corallites are very large and show highly variable development of carinate septa. C. Protocorallite of colony DPO 14788. D. Cross section of small colony DPO 14783. Septa are strongly thickened especially at dissepimentarium/tabularium boundary. E. Longitudinal section DPO 14786. Note strongly arched series of dissepiment−layers and convex tabulae. F. Cross section of colony−fragment DPO 14830 with development of juvenile corallites by marginal increase on lower right side of large protocorallite. G. Longitudinal section DPO 14790. H. Cross section of colony DPO 14787, consisting of a large protocorallite and four juvenile offsets developed by marginal increase. Undilated major septa do not reach to corallite axis. I. Longitudinal section of colony DPO 14787. J. Corallites of colony DPO 14790 (compare Fig. 8B), with strongly carinate septa breaking down into discrete trabeculae, becoming retiform. A–C, E–I, × 2; D × 3; J × 2.5. All specimens from the Upper Emsian of Colle." pageId="8" pageNumber="555">Fig. 8F, H</figureCitation>
|
||||
) and transformed
|
||||
<emphasis id="4F8F7777FF8436003434F974FF9EE970" box="[59,87,1770,1795]" italics="true" pageId="8" pageNumber="555">Ą</emphasis>
|
||||
to colonial growth. Apical portions of those protocorallites are not preserved. Some fragments show an attachment to corallite fragments of
|
||||
<taxonomicName id="BAFBD0E6FF853601352AFEB6FD7EEF32" authority="Soto" authorityName="Soto" box="[293,695,296,321]" class="Magnoliopsida" family="Aizoaceae" genus="Synaptophyllum" kingdom="Plantae" order="Caryophyllales" pageId="9" pageNumber="556" phylum="Tracheophyta" rank="species" species="multiseptatum">
|
||||
<emphasis id="4F8F7777FF853601352AFEB6FDB3EF33" box="[293,634,296,320]" italics="true" pageId="9" pageNumber="556">Synaptophyllum multiseptatum</emphasis>
|
||||
Soto
|
||||
</taxonomicName>
|
||||
, which has obviously been used as hardground. Colony surface is usually well preserved and calices show an everted calicular plane with a deeply depressed and flat central part (
|
||||
<figureCitation id="E5C0B7E0FF85360136A6FE16FFB4EFB2" captionStart="Fig" captionStartId="6.[812,845,1576,1595]" captionTargetBox="[813,1484,234,1546]" captionTargetId="figure-543@6.[813,1485,234,1546]" captionTargetPageId="6" captionText="Fig. 7. Cantabriastraea cantabrica gen. et sp. nov. A. Colony DPO 14811 consisting of a large protocorallite disrupted by nonparricidal, marginal increase in distal view (A1); septa appear as broad and flat ridges which are stronglyretiformtowardstheperiphery.Undersideofthesamecolony(A2), partly encrusted by Aulopora sp.; × 2. B. Colony DPO 14813. B1. Colony underside showing a single protocorallite turned to the left. B2. Upper surface of the same colony; × 1. All specimens from the Upper Emsian of Colle." pageId="9" pageNumber="556">Fig. 7A, D</figureCitation>
|
||||
). Growth form is astreoid−thamnasterioid, but septa are rarely confluent and limitations of corallites are usually marked by break down of septa. There are no true corallite walls. Calical centres are
|
||||
<quantity id="BA030680FF8536013582FD97FE33EC53" box="[397,506,521,545]" metricMagnitude="-2" metricUnit="m" metricValue="1.05" metricValueMax="1.3" metricValueMin="0.8" pageId="9" pageNumber="556" unit="mm" value="10.5" valueMax="13.0" valueMin="8.0">8–13 mm</quantity>
|
||||
apart, but can reach to
|
||||
<quantity id="BA030680FF8536013469FDB7FF7CEC33" box="[102,181,553,577]" metricMagnitude="-2" metricUnit="m" metricValue="1.7" pageId="9" pageNumber="556" unit="mm" value="17.0">17 mm</quantity>
|
||||
in juvenile coralla consisting of only a protocorallite and few smalloffsets(
|
||||
<figureCitation id="E5C0B7E0FF8536013555FDD6FE66EC12" box="[346,431,584,609]" captionStart="Fig" captionStartId="8.[102,135,1813,1832]" captionText="Fig. 8. Cantabriastraea cantabrica gen. et sp. nov. A. Cross section of colony DPO 14789 with medium sized corallites. B. Cross section of colony DPO 1790. Corallites are very large and show highly variable development of carinate septa. C. Protocorallite of colony DPO 14788. D. Cross section of small colony DPO 14783. Septa are strongly thickened especially at dissepimentarium/tabularium boundary. E. Longitudinal section DPO 14786. Note strongly arched series of dissepiment−layers and convex tabulae. F. Cross section of colony−fragment DPO 14830 with development of juvenile corallites by marginal increase on lower right side of large protocorallite. G. Longitudinal section DPO 14790. H. Cross section of colony DPO 14787, consisting of a large protocorallite and four juvenile offsets developed by marginal increase. Undilated major septa do not reach to corallite axis. I. Longitudinal section of colony DPO 14787. J. Corallites of colony DPO 14790 (compare Fig. 8B), with strongly carinate septa breaking down into discrete trabeculae, becoming retiform. A–C, E–I, × 2; D × 3; J × 2.5. All specimens from the Upper Emsian of Colle." pageId="9" pageNumber="556">Fig. 8H</figureCitation>
|
||||
). Morphology ofsepta ishighly variable within a colony as well as in individual corallites.
|
||||
<collectingRegion id="BF3F6587FF8536013469FD17FF6AECD2" box="[102,163,649,673]" country="Spain" name="Ceuta" pageId="9" pageNumber="556">Septa</collectingRegion>
|
||||
are usually thin near the corallite boundary, but moderately thickened and may bear numerous irregular carinae or lateralspines(vepreculae)intheirmiddlepart(
|
||||
<figureCitation id="E5C0B7E0FF8536013662FD56FD71EC93" box="[621,696,712,736]" captionStart="Fig" captionStartId="8.[102,135,731,750]" captionTargetBox="[556,1486,229,1340]" captionTargetId="figure-389@8.[556,1486,229,1340]" captionTargetPageId="8" captionText="Fig. 9. A. Cantabriastraea cantabrica gen. et sp. nov., specimen DPO 14789. A1. Cross sec− tion of tabularium and inner dissepimentarium. Trabeculae are oriented perpendicular to the rows of dissepiments; × 15. A2. Detail of A1; trabeculae intercalate between existing ones or bifurcate; × 20. A3. Septa in cross section with strong dilations in inner dissepimentarium caused by thickening of trabeculae. Towards the periphery (left side) septa become irregular carinate and may split into discrete trabeculae; × 24. B, C. Tabulophyllum bonarense sp. nov. B. Wall of corallite DPO 14673 in cross sec− tion. Thickenings of wall and lonsdaleoid dis− sepiments show a fibrous structure caused by thickened septal bases; × 24. C. Thin septa of corallite DPO 14686 (compare with Fig. 4G) inserting on lonsdaleoid dissepiments (dark lines in lower part of picture). Central part to− wards the axis (top of picture) is strongly af− fected by cement; × 24. All specimens from the Upper Emsian of Colle." pageId="9" pageNumber="556">Fig.9C</figureCitation>
|
||||
).Close to the dissepimentarium boundary they are usually strongly thickened and may be in lateral contact (
|
||||
<figureCitation id="E5C0B7E0FF8536013637FC96FD5AED52" box="[568,659,776,801]" captionStart="Fig" captionStartId="8.[102,135,1813,1832]" captionText="Fig. 8. Cantabriastraea cantabrica gen. et sp. nov. A. Cross section of colony DPO 14789 with medium sized corallites. B. Cross section of colony DPO 1790. Corallites are very large and show highly variable development of carinate septa. C. Protocorallite of colony DPO 14788. D. Cross section of small colony DPO 14783. Septa are strongly thickened especially at dissepimentarium/tabularium boundary. E. Longitudinal section DPO 14786. Note strongly arched series of dissepiment−layers and convex tabulae. F. Cross section of colony−fragment DPO 14830 with development of juvenile corallites by marginal increase on lower right side of large protocorallite. G. Longitudinal section DPO 14790. H. Cross section of colony DPO 14787, consisting of a large protocorallite and four juvenile offsets developed by marginal increase. Undilated major septa do not reach to corallite axis. I. Longitudinal section of colony DPO 14787. J. Corallites of colony DPO 14790 (compare Fig. 8B), with strongly carinate septa breaking down into discrete trabeculae, becoming retiform. A–C, E–I, × 2; D × 3; J × 2.5. All specimens from the Upper Emsian of Colle." pageId="9" pageNumber="556">Fig. 8D</figureCitation>
|
||||
). Carinate septa show a strong tendency to break down into discrete trabeculae giving septa a spongy, retiform morphology. Isolated groups of trabeculae are usually connected by numerous sections of lateral dissepiments, which gives the impression of very broad septa (
|
||||
<figureCitation id="E5C0B7E0FF853601352AFC36FE4CEDB2" box="[293,389,936,961]" captionStart="Fig" captionStartId="6.[812,845,1576,1595]" captionTargetBox="[813,1484,234,1546]" captionTargetId="figure-543@6.[813,1485,234,1546]" captionTargetPageId="6" captionText="Fig. 7. Cantabriastraea cantabrica gen. et sp. nov. A. Colony DPO 14811 consisting of a large protocorallite disrupted by nonparricidal, marginal increase in distal view (A1); septa appear as broad and flat ridges which are stronglyretiformtowardstheperiphery.Undersideofthesamecolony(A2), partly encrusted by Aulopora sp.; × 2. B. Colony DPO 14813. B1. Colony underside showing a single protocorallite turned to the left. B2. Upper surface of the same colony; × 1. All specimens from the Upper Emsian of Colle." pageId="9" pageNumber="556">Figs. 7A</figureCitation>
|
||||
,
|
||||
<figureCitation id="E5C0B7E0FF8536013580FC37FE63EDB2" box="[399,426,937,961]" captionStart="Fig" captionStartId="8.[102,135,1813,1832]" captionText="Fig. 8. Cantabriastraea cantabrica gen. et sp. nov. A. Cross section of colony DPO 14789 with medium sized corallites. B. Cross section of colony DPO 1790. Corallites are very large and show highly variable development of carinate septa. C. Protocorallite of colony DPO 14788. D. Cross section of small colony DPO 14783. Septa are strongly thickened especially at dissepimentarium/tabularium boundary. E. Longitudinal section DPO 14786. Note strongly arched series of dissepiment−layers and convex tabulae. F. Cross section of colony−fragment DPO 14830 with development of juvenile corallites by marginal increase on lower right side of large protocorallite. G. Longitudinal section DPO 14790. H. Cross section of colony DPO 14787, consisting of a large protocorallite and four juvenile offsets developed by marginal increase. Undilated major septa do not reach to corallite axis. I. Longitudinal section of colony DPO 14787. J. Corallites of colony DPO 14790 (compare Fig. 8B), with strongly carinate septa breaking down into discrete trabeculae, becoming retiform. A–C, E–I, × 2; D × 3; J × 2.5. All specimens from the Upper Emsian of Colle." pageId="9" pageNumber="556">8J</figureCitation>
|
||||
). Trabecularthickening ofsepta (
|
||||
<figureCitation id="E5C0B7E0FF8536013461FC56FF0AED92" box="[110,195,968,993]" captionStart="Fig" captionStartId="8.[102,135,731,750]" captionTargetBox="[556,1486,229,1340]" captionTargetId="figure-389@8.[556,1486,229,1340]" captionTargetPageId="8" captionText="Fig. 9. A. Cantabriastraea cantabrica gen. et sp. nov., specimen DPO 14789. A1. Cross sec− tion of tabularium and inner dissepimentarium. Trabeculae are oriented perpendicular to the rows of dissepiments; × 15. A2. Detail of A1; trabeculae intercalate between existing ones or bifurcate; × 20. A3. Septa in cross section with strong dilations in inner dissepimentarium caused by thickening of trabeculae. Towards the periphery (left side) septa become irregular carinate and may split into discrete trabeculae; × 24. B, C. Tabulophyllum bonarense sp. nov. B. Wall of corallite DPO 14673 in cross sec− tion. Thickenings of wall and lonsdaleoid dis− sepiments show a fibrous structure caused by thickened septal bases; × 24. C. Thin septa of corallite DPO 14686 (compare with Fig. 4G) inserting on lonsdaleoid dissepiments (dark lines in lower part of picture). Central part to− wards the axis (top of picture) is strongly af− fected by cement; × 24. All specimens from the Upper Emsian of Colle." pageId="9" pageNumber="556">Fig. 9C</figureCitation>
|
||||
) increases towards the tabularium border where they are flanked by numerous coarse carinae. However, there are colonies or corallites with very weak or even smooth septa, which are not affected by any septal degeneration (
|
||||
<figureCitation id="E5C0B7E0FF85360136AFFBB6FD33EA32" box="[672,762,1064,1089]" captionStart="Fig" captionStartId="8.[102,135,1813,1832]" captionText="Fig. 8. Cantabriastraea cantabrica gen. et sp. nov. A. Cross section of colony DPO 14789 with medium sized corallites. B. Cross section of colony DPO 1790. Corallites are very large and show highly variable development of carinate septa. C. Protocorallite of colony DPO 14788. D. Cross section of small colony DPO 14783. Septa are strongly thickened especially at dissepimentarium/tabularium boundary. E. Longitudinal section DPO 14786. Note strongly arched series of dissepiment−layers and convex tabulae. F. Cross section of colony−fragment DPO 14830 with development of juvenile corallites by marginal increase on lower right side of large protocorallite. G. Longitudinal section DPO 14790. H. Cross section of colony DPO 14787, consisting of a large protocorallite and four juvenile offsets developed by marginal increase. Undilated major septa do not reach to corallite axis. I. Longitudinal section of colony DPO 14787. J. Corallites of colony DPO 14790 (compare Fig. 8B), with strongly carinate septa breaking down into discrete trabeculae, becoming retiform. A–C, E–I, × 2; D × 3; J × 2.5. All specimens from the Upper Emsian of Colle." pageId="9" pageNumber="556">Fig. 8H</figureCitation>
|
||||
). Particularly septa in corallites of small colonies and protocorallites(
|
||||
<figureCitation id="E5C0B7E0FF85360134D6FBF6FEE0EAF2" box="[217,297,1128,1153]" captionStart="Fig" captionStartId="8.[102,135,1813,1832]" captionText="Fig. 8. Cantabriastraea cantabrica gen. et sp. nov. A. Cross section of colony DPO 14789 with medium sized corallites. B. Cross section of colony DPO 1790. Corallites are very large and show highly variable development of carinate septa. C. Protocorallite of colony DPO 14788. D. Cross section of small colony DPO 14783. Septa are strongly thickened especially at dissepimentarium/tabularium boundary. E. Longitudinal section DPO 14786. Note strongly arched series of dissepiment−layers and convex tabulae. F. Cross section of colony−fragment DPO 14830 with development of juvenile corallites by marginal increase on lower right side of large protocorallite. G. Longitudinal section DPO 14790. H. Cross section of colony DPO 14787, consisting of a large protocorallite and four juvenile offsets developed by marginal increase. Undilated major septa do not reach to corallite axis. I. Longitudinal section of colony DPO 14787. J. Corallites of colony DPO 14790 (compare Fig. 8B), with strongly carinate septa breaking down into discrete trabeculae, becoming retiform. A–C, E–I, × 2; D × 3; J × 2.5. All specimens from the Upper Emsian of Colle." pageId="9" pageNumber="556">Fig. 8C</figureCitation>
|
||||
)are weakly carinate. Majorsepta vary from
|
||||
<quantity id="BA030680FF8536013469FB17FF03EAD3" box="[102,202,1160,1185]" metricMagnitude="-1" metricUnit="m" metricValue="5.461" metricValueMax="6.096" metricValueMin="4.826" pageId="9" pageNumber="556" unit="in" value="21.5" valueMax="24.0" valueMin="19.0">19–24 in</quantity>
|
||||
number, but can reach up to
|
||||
<quantity id="BA030680FF8536013615FB17FD9CEAD3" box="[538,597,1160,1185]" metricMagnitude="-1" metricUnit="m" metricValue="7.874" pageId="9" pageNumber="556" unit="in" value="31.0">31 in</quantity>
|
||||
a protocorallite (
|
||||
<figureCitation id="E5C0B7E0FF8536013461FB36FF0FEAB2" box="[110,198,1192,1217]" captionStart="Fig" captionStartId="8.[102,135,1813,1832]" captionText="Fig. 8. Cantabriastraea cantabrica gen. et sp. nov. A. Cross section of colony DPO 14789 with medium sized corallites. B. Cross section of colony DPO 1790. Corallites are very large and show highly variable development of carinate septa. C. Protocorallite of colony DPO 14788. D. Cross section of small colony DPO 14783. Septa are strongly thickened especially at dissepimentarium/tabularium boundary. E. Longitudinal section DPO 14786. Note strongly arched series of dissepiment−layers and convex tabulae. F. Cross section of colony−fragment DPO 14830 with development of juvenile corallites by marginal increase on lower right side of large protocorallite. G. Longitudinal section DPO 14790. H. Cross section of colony DPO 14787, consisting of a large protocorallite and four juvenile offsets developed by marginal increase. Undilated major septa do not reach to corallite axis. I. Longitudinal section of colony DPO 14787. J. Corallites of colony DPO 14790 (compare Fig. 8B), with strongly carinate septa breaking down into discrete trabeculae, becoming retiform. A–C, E–I, × 2; D × 3; J × 2.5. All specimens from the Upper Emsian of Colle." pageId="9" pageNumber="556">Fig. 8C</figureCitation>
|
||||
). Although there are rhopaloid septa in some corallites, they are generally very slender within the tabularium and do not reach the corallite axis, so that a small axial space of 3.5–
|
||||
<quantity id="BA030680FF8536013498FA96FF1CEB53" box="[151,213,1288,1312]" metricMagnitude="-3" metricUnit="m" metricValue="5.0" pageId="9" pageNumber="556" unit="mm" value="5.0">5 mm</quantity>
|
||||
remains free, which is traversed by rare sections of tabulae. Minor septa barely extend into the tabularium. Sections of axially convex dissepiments are numerous, but are increasingly replaced by irregular or lateral dissepiments towards the periphery. Diameter of tabularia ranges from 3.5–5 mmand includespredominantly complete and slightly convex tabulae which are arranged above one another or are supplemented with peripheral tabellae. There are 13–30 tabulae/cm corallite length. The boundary to the dissepimentarium is characterized by steeply inclined globular dissepiments and accordingwiththeevertedcalice,thedissepimentallayersarestrongly arched (
|
||||
<figureCitation id="E5C0B7E0FF85360134B2F9F6FEFBE8F2" box="[189,306,1640,1665]" captionStart="Fig" captionStartId="8.[102,135,1813,1832]" captionText="Fig. 8. Cantabriastraea cantabrica gen. et sp. nov. A. Cross section of colony DPO 14789 with medium sized corallites. B. Cross section of colony DPO 1790. Corallites are very large and show highly variable development of carinate septa. C. Protocorallite of colony DPO 14788. D. Cross section of small colony DPO 14783. Septa are strongly thickened especially at dissepimentarium/tabularium boundary. E. Longitudinal section DPO 14786. Note strongly arched series of dissepiment−layers and convex tabulae. F. Cross section of colony−fragment DPO 14830 with development of juvenile corallites by marginal increase on lower right side of large protocorallite. G. Longitudinal section DPO 14790. H. Cross section of colony DPO 14787, consisting of a large protocorallite and four juvenile offsets developed by marginal increase. Undilated major septa do not reach to corallite axis. I. Longitudinal section of colony DPO 14787. J. Corallites of colony DPO 14790 (compare Fig. 8B), with strongly carinate septa breaking down into discrete trabeculae, becoming retiform. A–C, E–I, × 2; D × 3; J × 2.5. All specimens from the Upper Emsian of Colle." pageId="9" pageNumber="556">Fig. 8E, G</figureCitation>
|
||||
). They are commonly traversed by fanning monacanth trabeculae, which are arranged perpendicular to the dissepiments and may show bifurcations (
|
||||
<figureCitation id="E5C0B7E0FF8536013626F936FD57E8B2" box="[553,670,1704,1729]" captionStart="Fig" captionStartId="8.[102,135,731,750]" captionTargetBox="[556,1486,229,1340]" captionTargetId="figure-389@8.[556,1486,229,1340]" captionTargetPageId="8" captionText="Fig. 9. A. Cantabriastraea cantabrica gen. et sp. nov., specimen DPO 14789. A1. Cross sec− tion of tabularium and inner dissepimentarium. Trabeculae are oriented perpendicular to the rows of dissepiments; × 15. A2. Detail of A1; trabeculae intercalate between existing ones or bifurcate; × 20. A3. Septa in cross section with strong dilations in inner dissepimentarium caused by thickening of trabeculae. Towards the periphery (left side) septa become irregular carinate and may split into discrete trabeculae; × 24. B, C. Tabulophyllum bonarense sp. nov. B. Wall of corallite DPO 14673 in cross sec− tion. Thickenings of wall and lonsdaleoid dis− sepiments show a fibrous structure caused by thickened septal bases; × 24. C. Thin septa of corallite DPO 14686 (compare with Fig. 4G) inserting on lonsdaleoid dissepiments (dark lines in lower part of picture). Central part to− wards the axis (top of picture) is strongly af− fected by cement; × 24. All specimens from the Upper Emsian of Colle." pageId="9" pageNumber="556">Fig. 9A, B</figureCitation>
|
||||
).
|
||||
</paragraph>
|
||||
<caption id="2984FBEDFF8436003469F88BFC48E99B" pageId="8" pageNumber="555" startId="8.[102,135,1813,1832]" targetType="figure">
|
||||
<paragraph id="7D44AB65FF8436003469F88BFC48E99B" blockId="8.[102,1485,1813,2025]" pageId="8" pageNumber="555">
|
||||
Fig. 8.
|
||||
<taxonomicName id="BAFBD0E6FF84360034AAF88BFE2DE95A" authorityName="gen. et" authorityYear="2003" box="[165,484,1813,1833]" class="Anthozoa" family="Disphyllidae" genus="Cantabriastraea" higherTaxonomySource="GBIF" kingdom="Animalia" pageId="8" pageNumber="555" phylum="Cnidaria" rank="species" species="cantabrica" status="gen. et">
|
||||
<emphasis id="4F8F7777FF84360034AAF88BFE6BE95B" box="[165,418,1813,1832]" italics="true" pageId="8" pageNumber="555">Cantabriastraea cantabrica</emphasis>
|
||||
<taxonomicNameLabel id="54BCCA0CFF84360035A7F888FE2DE95A" box="[424,484,1814,1833]" pageId="8" pageNumber="555" rank="species">gen. et</taxonomicNameLabel>
|
||||
</taxonomicName>
|
||||
sp. nov.
|
||||
<emphasis id="4F8F7777FF8436003639F88BFD8FE95B" bold="true" box="[566,582,1813,1832]" pageId="8" pageNumber="555">A</emphasis>
|
||||
. Cross section of colony DPO 14789 with medium sized corallites.
|
||||
<emphasis id="4F8F7777FF84360030A4F88BFB73E95B" bold="true" box="[1195,1210,1813,1832]" pageId="8" pageNumber="555">B</emphasis>
|
||||
. Cross section of colony DPO 1790. Corallites are very large and show highly variable development of carinate septa.
|
||||
<emphasis id="4F8F7777FF8436003772F8AEFC44E930" bold="true" box="[893,909,1840,1859]" pageId="8" pageNumber="555">C</emphasis>
|
||||
. Protocorallite of colony DPO 14788.
|
||||
<emphasis id="4F8F7777FF84360030E5F8AFFB33E937" bold="true" box="[1258,1274,1841,1860]" pageId="8" pageNumber="555">D</emphasis>
|
||||
. Cross section of small colony DPO 14783. Septa are strongly thickened especially at dissepimentarium/tabularium boundary.
|
||||
<emphasis id="4F8F7777FF843600300BF8D2FBDAE92C" bold="true" box="[1028,1043,1868,1887]" pageId="8" pageNumber="555">E</emphasis>
|
||||
. Longitudinal section DPO 14786. Note strongly arched series of dissepiment−layers and convex tabulae.
|
||||
<emphasis id="4F8F7777FF843600366EF8F6FDA6E908" bold="true" box="[609,623,1896,1915]" pageId="8" pageNumber="555">F</emphasis>
|
||||
. Cross section of colony−fragment DPO 14830 with development of juvenile corallites by marginal increase on lower right side of large protocorallite.
|
||||
<emphasis id="4F8F7777FF843600366FF81DFDBBE9E5" bold="true" box="[608,626,1923,1942]" pageId="8" pageNumber="555">G</emphasis>
|
||||
. Longitudinal section DPO 14790.
|
||||
<emphasis id="4F8F7777FF84360037BFF81DFC0BE9E5" bold="true" box="[944,962,1923,1942]" pageId="8" pageNumber="555">H</emphasis>
|
||||
. Cross section of colony DPO 14787, consisting of a large protocorallite and four juvenile offsets developed by marginal increase. Undilated major septa do not reach to corallite axis.
|
||||
<emphasis id="4F8F7777FF84360030B0F801FB01E9C1" bold="true" box="[1215,1224,1951,1970]" pageId="8" pageNumber="555">I</emphasis>
|
||||
. Longitudinal section of colony DPO 14787.
|
||||
<emphasis id="4F8F7777FF8436003508F824FEDBE9BE" bold="true" box="[263,274,1978,1997]" pageId="8" pageNumber="555">J</emphasis>
|
||||
. Corallites of colony DPO 14790 (compare Fig. 8B), with strongly carinate septa breaking down into discrete trabeculae, becoming retiform. A–C, E–I, × 2; D × 3; J × 2.5. All specimens from the Upper Emsian of Colle.
|
||||
</paragraph>
|
||||
</caption>
|
||||
<paragraph id="7D44AB65FF8536013469F949FD50E89D" blockId="9.[102,665,1750,1775]" box="[102,665,1750,1775]" pageId="9" pageNumber="556">
|
||||
<emphasis id="4F8F7777FF8536013469F949FF23E89D" box="[102,234,1751,1774]" italics="true" pageId="9" pageNumber="556">Occurrence</emphasis>
|
||||
.—Only known from the
|
||||
<typeStatus id="A24015C7FF8536013609F949FDFFE89C" box="[518,566,1751,1775]" pageId="9" pageNumber="556">type</typeStatus>
|
||||
locality.
|
||||
</paragraph>
|
||||
</subSubSection>
|
||||
</treatment>
|
||||
</document>
|
193
data/F5/52/1A/F5521A73FF8D360A3469FB5EFE0CEFF3.xml
Normal file
193
data/F5/52/1A/F5521A73FF8D360A3469FB5EFE0CEFF3.xml
Normal file
|
@ -0,0 +1,193 @@
|
|||
<document id="526AFF49A5AC39BFF409F205BF3DF6D1" ID-ISSN="1732-2421" IM.bibliography_approvedBy="felipe" IM.illustrations_approvedBy="felipe" IM.materialsCitations_approvedBy="felipe" IM.metadata_approvedBy="karina" IM.tables_approvedBy="karina" IM.taxonomicNames_approvedBy="karina" IM.treatments_approvedBy="karina" checkinTime="1723062031241" checkinUser="felipe" docAuthor="Schröder, Stefan & Soto, Francisco" docDate="2003" docId="F5521A73FF8D360A3469FB5EFE0CEFF3" docLanguage="en" docName="ActaPalaeontolPol.48.4.547-558.pdf" docOrigin="Acta Palaeontologica Polonica 48 (4)" docStyle="DocumentStyle:93F5927C23D90727DE855278A6F17B37.1:ActaPalaeontolPol.2002-2009.journal_article" docStyleId="93F5927C23D90727DE855278A6F17B37" docStyleName="ActaPalaeontolPol.2002-2009.journal_article" docStyleVersion="1" docTitle="Tabulophyllum Fenton and Fenton 1924" docType="treatment" docVersion="1" lastPageNumber="548" masterDocId="096B620BFF8C3608340FFF9EFFC9EE73" masterDocTitle="Lower Devonian (Emsian) rugose corals from the Cantabrian Mountains, northern Spain" masterLastPageNumber="558" masterPageNumber="547" pageNumber="548" updateTime="1724879130370" updateUser="karina" zenodo-license-document="CC-BY-4.0">
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<mods:titleInfo id="A0F6567AF093585A71A8A94BC9EF9DAB">
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<mods:title id="DE4546F3F3794399CCE0A0A1B10628F5">Lower Devonian (Emsian) rugose corals from the Cantabrian Mountains, northern Spain</mods:title>
|
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</mods:titleInfo>
|
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<mods:namePart id="2F945C83098102F8F1F77289F3E534D4">Schröder, Stefan</mods:namePart>
|
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|
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<mods:roleTerm id="6BA91DB96F05955C94C233E40EF82099">Author</mods:roleTerm>
|
||||
</mods:role>
|
||||
<mods:namePart id="C13F2CBFB0E84823E96A152471E1A10E">Soto, Francisco</mods:namePart>
|
||||
</mods:name>
|
||||
<mods:typeOfResource id="133C88EFCFC14BB2F7C8FBDC6E2B05A1">text</mods:typeOfResource>
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<mods:titleInfo id="0BD3252F923B1D91CDB9EEF6B95065C9">
|
||||
<mods:title id="1C6C2B2CB0FBD0A1CCB1284CB744437C">Acta Palaeontologica Polonica</mods:title>
|
||||
</mods:titleInfo>
|
||||
<mods:part id="7B5A34205591C4873AB678B8FBEACDBF">
|
||||
<mods:date id="8D9F720E77B4BA411EC404B49DE491CE">2003</mods:date>
|
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<mods:detail id="3E26602A01FDB81280A8134124C48079" type="pubDate">
|
||||
<mods:number id="76E166F23B090DFEB695D0268D2FCF23">2003-09-30</mods:number>
|
||||
</mods:detail>
|
||||
<mods:detail id="DE9333B0B6B50AF89C3DB51C68F97358" type="volume">
|
||||
<mods:number id="6E4AC17B291B4C2F1E31271325A31694">48</mods:number>
|
||||
</mods:detail>
|
||||
<mods:detail id="FAFE0200404A9A0F617B8908C2B2CDE4" type="issue">
|
||||
<mods:number id="40D9CCAF9CCC58EB14AD021C28A4D771">4</mods:number>
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||||
</mods:detail>
|
||||
<mods:extent id="570F3B121C77AD5B24E878D3E0A21E37" unit="page">
|
||||
<mods:start id="B452E170EE2B96C5267DD1CA24254A5E">547</mods:start>
|
||||
<mods:end id="1557630250646C9F3E48542D1B25B308">558</mods:end>
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</mods:extent>
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<mods:classification id="A7DFB9456FD15D623DD532C7A6929C88">journal article</mods:classification>
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||||
<mods:identifier id="D6462658965BC840F1EC9C834426CC52" type="ISSN">1732-2421</mods:identifier>
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||||
</mods:mods>
|
||||
<treatment id="F5521A73FF8D360A3469FB5EFE0CEFF3" LSID="urn:lsid:plazi:treatment:F5521A73FF8D360A3469FB5EFE0CEFF3" httpUri="http://treatment.plazi.org/id/F5521A73FF8D360A3469FB5EFE0CEFF3" lastPageId="2" lastPageNumber="548" pageId="1" pageNumber="548">
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<subSubSection id="35E1F8EEFF8D36093469FB5EFD00EAAE" box="[102,713,1216,1245]" pageId="1" pageNumber="548" type="nomenclature">
|
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<paragraph id="7D44AB65FF8D36093469FB5EFD00EAAE" blockId="1.[102,775,1072,1306]" box="[102,713,1216,1245]" pageId="1" pageNumber="548">
|
||||
Genus
|
||||
<taxonomicName id="BAFBD0E6FF8D360934CFFB5EFD00EAAE" authority="Fenton and Fenton, 1924" authorityName="Fenton and Fenton" authorityYear="1924" box="[192,713,1216,1245]" class="Anthozoa" family="Chonophyllidae" genus="Tabulophyllum" higherTaxonomySource="GBIF" kingdom="Animalia" order="Stauriida" pageId="1" pageNumber="548" phylum="Cnidaria" rank="genus">
|
||||
<emphasis id="4F8F7777FF8D360934CFFB5EFE4BEAAE" box="[192,386,1216,1245]" italics="true" pageId="1" pageNumber="548">Tabulophyllum</emphasis>
|
||||
<bibRefCitation id="196AD694FF8D36093586FB5FFD00EAAE" author="Fenton, C. L. & Fenton, M. A." box="[393,713,1216,1245]" pageId="1" pageNumber="548" pagination="1 - 260" refId="ref7469" refString="Fenton, C. L. and Fenton, M. A. 1924. The stratigraphy and fauna of the Hackberry Stage of the Upper Devonian. Contributions of the Museum of Geology, University of Michigan 1: 1 - 260." type="journal article" year="1924">Fenton and Fenton, 1924</bibRefCitation>
|
||||
</taxonomicName>
|
||||
</paragraph>
|
||||
</subSubSection>
|
||||
<subSubSection id="35E1F8EEFF8D360A3469FB77FE0CEFF3" lastPageId="2" lastPageNumber="549" pageId="1" pageNumber="548" type="materials_examined">
|
||||
<paragraph id="7D44AB65FF8D36093469FB77FEDDEB69" blockId="1.[102,775,1072,1306]" pageId="1" pageNumber="548">
|
||||
<emphasis id="4F8F7777FF8D36093469FB77FF29EA8E" box="[102,224,1256,1278]" italics="true" pageId="1" pageNumber="548">
|
||||
<typeStatus id="A24015C7FF8D36093469FB77FF5CEA8D" box="[102,149,1257,1278]" pageId="1" pageNumber="548">Type</typeStatus>
|
||||
species
|
||||
</emphasis>
|
||||
(by original designation):
|
||||
<taxonomicName id="BAFBD0E6FF8D360935EDFB76FED9EB69" authority="Fenton and Fenton, 1924" authorityName="Fenton and Fenton" authorityYear="1924" class="Anthozoa" family="Chonophyllidae" genus="Tabulophyllum" higherTaxonomySource="GBIF" kingdom="Animalia" pageId="1" pageNumber="548" phylum="Cnidaria" rank="species" species="rectum">
|
||||
<emphasis id="4F8F7777FF8D360935EDFB76FD77EA8D" box="[482,702,1256,1278]" italics="true" pageId="1" pageNumber="548">Tabulophyllum rectum</emphasis>
|
||||
<bibRefCitation id="196AD694FF8D360936CBFB76FED9EB69" author="Fenton, C. L. & Fenton, M. A." pageId="1" pageNumber="548" pagination="1 - 260" refId="ref7469" refString="Fenton, C. L. and Fenton, M. A. 1924. The stratigraphy and fauna of the Hackberry Stage of the Upper Devonian. Contributions of the Museum of Geology, University of Michigan 1: 1 - 260." type="journal article" year="1924">Fenton and Fenton, 1924</bibRefCitation>
|
||||
</taxonomicName>
|
||||
.
|
||||
</paragraph>
|
||||
<paragraph id="7D44AB65FF8D36093469FAB4FE2CEB31" blockId="1.[102,485,1322,1346]" box="[102,485,1322,1346]" pageId="1" pageNumber="548">
|
||||
<emphasis id="4F8F7777FF8D36093469FAB4FF11EB32" box="[102,216,1322,1345]" italics="true" pageId="1" pageNumber="548">Diagnosis</emphasis>
|
||||
.—See
|
||||
<bibRefCitation id="196AD694FF8D36093525FAB4FE28EB31" author="Sorauf, J. E." box="[298,481,1322,1346]" pageId="1" pageNumber="548" pagination="397 - 412" refId="ref8715" refString="Sorauf, J. E. 1989. The Devonian rugose coral genus Tabulophyllum Fenton andFenton, 1924. In: N. J. McMillan, A. F. Embry, andD. J. Glass (eds.), Devonian of the World (Proceedings of the Second International SymposiumontheDevonianSystemCalgary, Canada), Canadian Society of Petroleum Geologists, Memoir 14 (3): 397 - 412." type="journal article" year="1989">Sorauf 1989: 33</bibRefCitation>
|
||||
.
|
||||
</paragraph>
|
||||
<paragraph id="7D44AB65FF8D36093469FACCFD52E81A" blockId="1.[102,775,1362,2026]" pageId="1" pageNumber="548">
|
||||
<emphasis id="4F8F7777FF8D36093469FACCFF01EB19" box="[102,200,1362,1386]" italics="true" pageId="1" pageNumber="548">Remarks</emphasis>
|
||||
.—In general, only solitary corals are currently assigned to the genus
|
||||
<taxonomicName id="BAFBD0E6FF8D3609354BFAECFE27EBF9" authorityName="Fenton and Fenton" authorityYear="1924" box="[324,494,1394,1418]" class="Anthozoa" family="Chonophyllidae" genus="Tabulophyllum" higherTaxonomySource="GBIF" kingdom="Animalia" pageId="1" pageNumber="548" phylum="Cnidaria" rank="genus">
|
||||
<emphasis id="4F8F7777FF8D3609354BFAECFE27EBF9" box="[324,494,1394,1418]" italics="true" pageId="1" pageNumber="548">Tabulophyllum</emphasis>
|
||||
</taxonomicName>
|
||||
, and the classification of colonial forms as
|
||||
<taxonomicName id="BAFBD0E6FF8D3609353CFA0CFE14EBD9" authorityName="Fenton and Fenton" authorityYear="1924" box="[307,477,1426,1450]" class="Anthozoa" family="Chonophyllidae" genus="Tabulophyllum" higherTaxonomySource="GBIF" kingdom="Animalia" pageId="1" pageNumber="548" phylum="Cnidaria" rank="genus">
|
||||
<emphasis id="4F8F7777FF8D3609353CFA0CFE14EBD9" box="[307,477,1426,1450]" italics="true" pageId="1" pageNumber="548">Tabulophyllum</emphasis>
|
||||
</taxonomicName>
|
||||
by
|
||||
<bibRefCitation id="196AD694FF8D36093605FA0CFD0EEBD9" author="Soshkina, E. D. & Soskina, E. D." box="[522,711,1426,1450]" pageId="1" pageNumber="548" pagination="1 - 127" refId="ref9062" refString="Soshkina, E. D. [Soskina, E. D.] 1952. Determination book of Devonian tetracorals [in Russian]. Trudy Paleontologiceskogo Instituta, Akade - mia Nauk SSSR 39: 1 - 127." type="journal article" year="1952">Soshkina (1952)</bibRefCitation>
|
||||
, Bulvanker (1958) and
|
||||
<bibRefCitation id="196AD694FF8D3609354CFA2CFE2CEBB9" author="Ivaniya, V. A. & Ivania, V. A." box="[323,485,1458,1482]" pageId="1" pageNumber="548" refId="ref7855" refString="Ivaniya, V. A. [Ivania, V. A.] 1965. Devonskie korally Rugosa Saano- Altajskoj gornoj oblasti. 398 pp. TomskijGosudarstvennyj Universitet, Tomsk." type="book" year="1965">Ivaniya (1965</bibRefCitation>
|
||||
,
|
||||
<bibRefCitation id="196AD694FF8D360935FBFA2CFDE4EBB9" author="Ivaniya, V. A. & Ivania, V. A." box="[500,557,1458,1482]" pageId="1" pageNumber="548" refId="ref7887" refString="Ivaniya, V. A. [Ivania, V. A.] 1980. Devonskie cetyrehlucevye korally Salaira i Severnogo Kuzbassa (sistematika, biostratigrafi a, ekologia). 140 pp. Izdatel'stvo Tomskogo Universiteta, Tomsk." type="book" year="1980">1980</bibRefCitation>
|
||||
) has been rejected (
|
||||
<bibRefCitation id="196AD694FF8D36093462FA4CFE44EB99" author="McLean, R. A. & Pedder, A. E. H." box="[109,397,1490,1514]" pageId="1" pageNumber="548" pagination="131 - 173" refId="ref8267" refString="McLean, R. A. and Pedder, A. E. H. 1987. Frasnian rugose corals of western Canada. Part 2: The genus Smithiphyllum. Palaeontographica A 195 (4 - 6): 131 - 173." type="journal article" year="1987">McLean and Pedder 1987</bibRefCitation>
|
||||
;
|
||||
<bibRefCitation id="196AD694FF8D36093598FA4CFDEAEB99" author="Sorauf, J. E." box="[407,547,1490,1514]" pageId="1" pageNumber="548" pagination="397 - 412" refId="ref8715" refString="Sorauf, J. E. 1989. The Devonian rugose coral genus Tabulophyllum Fenton andFenton, 1924. In: N. J. McMillan, A. F. Embry, andD. J. Glass (eds.), Devonian of the World (Proceedings of the Second International SymposiumontheDevonianSystemCalgary, Canada), Canadian Society of Petroleum Geologists, Memoir 14 (3): 397 - 412." type="journal article" year="1989">Sorauf 1989</bibRefCitation>
|
||||
). The new species of
|
||||
<taxonomicName id="BAFBD0E6FF8D36093469FA6CFED9E879" authorityName="Fenton and Fenton" authorityYear="1924" box="[102,272,1522,1546]" class="Anthozoa" family="Chonophyllidae" genus="Tabulophyllum" higherTaxonomySource="GBIF" kingdom="Animalia" pageId="1" pageNumber="548" phylum="Cnidaria" rank="genus">
|
||||
<emphasis id="4F8F7777FF8D36093469FA6CFED9E879" box="[102,272,1522,1546]" italics="true" pageId="1" pageNumber="548">Tabulophyllum</emphasis>
|
||||
</taxonomicName>
|
||||
described herein is apparently solitary but displays a distinctive growth known as “quasi−colonial” and such solitary species with few lateral offsets should also be included in the generic concept of
|
||||
<taxonomicName id="BAFBD0E6FF8D360935E5F9CCFD5DE819" authorityName="Fenton and Fenton" authorityYear="1924" box="[490,660,1618,1642]" class="Anthozoa" family="Chonophyllidae" genus="Tabulophyllum" higherTaxonomySource="GBIF" kingdom="Animalia" pageId="1" pageNumber="548" phylum="Cnidaria" rank="genus">
|
||||
<emphasis id="4F8F7777FF8D360935E5F9CCFD5DE819" box="[490,660,1618,1642]" italics="true" pageId="1" pageNumber="548">Tabulophyllum</emphasis>
|
||||
</taxonomicName>
|
||||
.
|
||||
</paragraph>
|
||||
<caption id="2984FBEDFF8D36093723F9AAFCA1E80C" pageId="1" pageNumber="548" startId="1.[812,845,1588,1607]" targetBox="[876,903,974,1544]" targetPageId="1" targetType="figure">
|
||||
<paragraph id="7D44AB65FF8D36093723F9AAFCA1E80C" blockId="1.[812,1485,1588,1663]" pageId="1" pageNumber="548">
|
||||
Fig. 2. Stratigraphical section at Colle (Lower Devonian), with location of beds where the studied rugose corals occur (modified from
|
||||
<bibRefCitation id="196AD694FF8D3609314CF9CEFC94E80C" author="Garcia-Alcalde, J. L." pageId="1" pageNumber="548" pagination="159 - 176" refId="ref7601" refString="Garcia-Alcalde, J. L. 1999. Terebratulidos (Braquiopodos) delEmsiensesuperior de Colle (Sabero, Leon, N de Espana). Trabajos de Geologia 21: 159 - 176." type="journal article" year="1999">Garcia−Alcalde 1999</bibRefCitation>
|
||||
).
|
||||
</paragraph>
|
||||
</caption>
|
||||
<paragraph id="7D44AB65FF8D36093484F9ECFBD5E911" blockId="1.[102,775,1362,2026]" lastBlockId="1.[812,1485,1706,1890]" pageId="1" pageNumber="548">
|
||||
Similar structures are also known from the closely related kyphophyllid genus
|
||||
<taxonomicName id="BAFBD0E6FF8D36093557F90CFF68E8B9" authority="McLean and Pedder, 1984" authorityName="McLean and Pedder" authorityYear="1984" class="Anthozoa" family="Arachnophyllidae" genus="Tarphyphyllum" higherTaxonomySource="GBIF" kingdom="Animalia" pageId="1" pageNumber="548" phylum="Cnidaria" rank="genus">
|
||||
<emphasis id="4F8F7777FF8D36093557F90CFDCAE8D9" box="[344,515,1682,1706]" italics="true" pageId="1" pageNumber="548">Tarphyphyllum</emphasis>
|
||||
<bibRefCitation id="196AD694FF8D3609361EF90CFF68E8B9" author="McLean, R. A. & Pedder, A. E. H." pageId="1" pageNumber="548" pagination="1 - 38" refId="ref8223" refString="McLean, R. A. and Pedder, A. E. H. 1984. Frasnian rugose corals of western Canada. Part 1: Chonophyllidae and Kyphophyllidae. Palaeontographica A 184 (1 - 3): 1 - 38." type="journal article" year="1984">McLean and Pedder, 1984</bibRefCitation>
|
||||
</taxonomicName>
|
||||
. Its type species
|
||||
<taxonomicName id="BAFBD0E6FF8D36093553F92CFD13E8B9" authority="McLean and Pedder, 1984" authorityName="McLean and Pedder" authorityYear="1984" box="[348,730,1714,1738]" class="Anthozoa" family="Arachnophyllidae" genus="Tarphyphyllum" higherTaxonomySource="GBIF" kingdom="Animalia" pageId="1" pageNumber="548" phylum="Cnidaria" rank="species" species="besti">
|
||||
<emphasis id="4F8F7777FF8D36093553F92CFE67E8B9" box="[348,430,1714,1738]" italics="true" pageId="1" pageNumber="548">T. besti</emphasis>
|
||||
<bibRefCitation id="196AD694FF8D360935BBF92CFD13E8B9" author="McLean, R. A. & Pedder, A. E. H." box="[436,730,1714,1738]" pageId="1" pageNumber="548" pagination="1 - 38" refId="ref8223" refString="McLean, R. A. and Pedder, A. E. H. 1984. Frasnian rugose corals of western Canada. Part 1: Chonophyllidae and Kyphophyllidae. Palaeontographica A 184 (1 - 3): 1 - 38." type="journal article" year="1984">McLean and Pedder, 1984</bibRefCitation>
|
||||
</taxonomicName>
|
||||
is a solitary species developing few offsets (
|
||||
<bibRefCitation id="196AD694FF8D3609362BF94CFF6BE979" author="McLean, R. A. & Pedder, A. E. H." pageId="1" pageNumber="548" pagination="1 - 38" refId="ref8223" refString="McLean, R. A. and Pedder, A. E. H. 1984. Frasnian rugose corals of western Canada. Part 1: Chonophyllidae and Kyphophyllidae. Palaeontographica A 184 (1 - 3): 1 - 38." type="journal article" year="1984">McLean and Pedder 1984</bibRefCitation>
|
||||
: pl. 11: 4, 7, 10), whereas
|
||||
<specimenCount id="6BFD60ECFF8D360935FCF96CFD41E979" box="[499,648,1778,1802]" count="1" pageId="1" pageNumber="548" type="generic" typeStatus="paratype">one paratype</specimenCount>
|
||||
is weakly branching to fasciculate (
|
||||
<bibRefCitation id="196AD694FF8D3609358AF88CFD78E959" author="McLean, R. A. & Pedder, A. E. H." box="[389,689,1810,1834]" pageId="1" pageNumber="548" pagination="1 - 38" refId="ref8223" refString="McLean, R. A. and Pedder, A. E. H. 1984. Frasnian rugose corals of western Canada. Part 1: Chonophyllidae and Kyphophyllidae. Palaeontographica A 184 (1 - 3): 1 - 38." type="journal article" year="1984">McLean and Pedder 1984</bibRefCitation>
|
||||
: pl. 10: 12). Internally
|
||||
<taxonomicName id="BAFBD0E6FF8D3609351CF8ACFE77E939" authorityName="McLean and Pedder" authorityYear="1984" box="[275,446,1842,1866]" class="Anthozoa" family="Arachnophyllidae" genus="Tarphyphyllum" higherTaxonomySource="GBIF" kingdom="Animalia" pageId="1" pageNumber="548" phylum="Cnidaria" rank="genus">
|
||||
<emphasis id="4F8F7777FF8D3609351CF8ACFE77E939" box="[275,446,1842,1866]" italics="true" pageId="1" pageNumber="548">Tarphyphyllum</emphasis>
|
||||
</taxonomicName>
|
||||
differs from
|
||||
<taxonomicName id="BAFBD0E6FF8D36093653F8ACFCCFE939" authorityName="Fenton and Fenton" authorityYear="1924" box="[604,774,1842,1866]" class="Anthozoa" family="Chonophyllidae" genus="Tabulophyllum" higherTaxonomySource="GBIF" kingdom="Animalia" pageId="1" pageNumber="548" phylum="Cnidaria" rank="genus">
|
||||
<emphasis id="4F8F7777FF8D36093653F8ACFCCFE939" box="[604,774,1842,1866]" italics="true" pageId="1" pageNumber="548">Tabulophyllum</emphasis>
|
||||
</taxonomicName>
|
||||
only in having a more strongly developed stereozone of dilated septa, masking the dissepiments, a more simple tabularium, and less numerous dissepiments. Because of the striking resemblances between both genera
|
||||
<bibRefCitation id="196AD694FF8D36093668F82CFF42E999" author="Sorauf, J. E." pageId="1" pageNumber="548" pagination="1 - 159" refId="ref8929" refString="Sorauf, J. E. 1998. Frasnian (Upper Devonian) rugose corals from the Lime Creek and Shell Rock Formations of Iowa. Bulletins of American Paleontology 113 (355): 1 - 159." type="journal article" year="1998">Sorauf (1998: 49)</bibRefCitation>
|
||||
suggests that
|
||||
<taxonomicName id="BAFBD0E6FF8D36093520F84CFE13E999" authorityName="McLean and Pedder" authorityYear="1984" box="[303,474,2002,2026]" class="Anthozoa" family="Arachnophyllidae" genus="Tarphyphyllum" higherTaxonomySource="GBIF" kingdom="Animalia" pageId="1" pageNumber="548" phylum="Cnidaria" rank="genus">
|
||||
<emphasis id="4F8F7777FF8D36093520F84CFE13E999" box="[303,474,2002,2026]" italics="true" pageId="1" pageNumber="548">Tarphyphyllum</emphasis>
|
||||
</taxonomicName>
|
||||
should rather be regarded as subgenus of
|
||||
<taxonomicName id="BAFBD0E6FF8D360937DBF934FBB7E8B1" authorityName="Fenton and Fenton" authorityYear="1924" box="[980,1150,1706,1730]" class="Anthozoa" family="Chonophyllidae" genus="Tabulophyllum" higherTaxonomySource="GBIF" kingdom="Animalia" pageId="1" pageNumber="548" phylum="Cnidaria" rank="genus">
|
||||
<emphasis id="4F8F7777FF8D360937DBF934FBB7E8B1" box="[980,1150,1706,1730]" italics="true" pageId="1" pageNumber="548">Tabulophyllum</emphasis>
|
||||
</taxonomicName>
|
||||
. Probably some of the weakly colonial species previously assigned to
|
||||
<taxonomicName id="BAFBD0E6FF8D3609312CF954FA04E891" authorityName="Fenton and Fenton" authorityYear="1924" box="[1315,1485,1738,1762]" class="Anthozoa" family="Chonophyllidae" genus="Tabulophyllum" higherTaxonomySource="GBIF" kingdom="Animalia" pageId="1" pageNumber="548" phylum="Cnidaria" rank="genus">
|
||||
<emphasis id="4F8F7777FF8D3609312CF954FA04E891" box="[1315,1485,1738,1762]" italics="true" pageId="1" pageNumber="548">Tabulophyllum</emphasis>
|
||||
</taxonomicName>
|
||||
should be removed to
|
||||
<taxonomicName id="BAFBD0E6FF8D3609303CF974FB17E971" authorityName="McLean and Pedder" authorityYear="1984" box="[1075,1246,1770,1794]" class="Anthozoa" family="Arachnophyllidae" genus="Tarphyphyllum" higherTaxonomySource="GBIF" kingdom="Animalia" pageId="1" pageNumber="548" phylum="Cnidaria" rank="genus">
|
||||
<emphasis id="4F8F7777FF8D3609303CF974FB17E971" box="[1075,1246,1770,1794]" italics="true" pageId="1" pageNumber="548">Tarphyphyllum</emphasis>
|
||||
</taxonomicName>
|
||||
. Colonial species of
|
||||
<taxonomicName id="BAFBD0E6FF8D36093723F894FC1EE951" authorityName="McLean and Pedder" authorityYear="1984" box="[812,983,1802,1826]" class="Anthozoa" family="Arachnophyllidae" genus="Tarphyphyllum" higherTaxonomySource="GBIF" kingdom="Animalia" pageId="1" pageNumber="548" phylum="Cnidaria" rank="genus">
|
||||
<emphasis id="4F8F7777FF8D36093723F894FC1EE951" box="[812,983,1802,1826]" italics="true" pageId="1" pageNumber="548">Tarphyphyllum</emphasis>
|
||||
</taxonomicName>
|
||||
may also be very difficult to separate from
|
||||
<taxonomicName id="BAFBD0E6FF8D36093723F8B4FB5CE931" authority="Birenheide, 1962" authorityName="Birenheide" authorityYear="1962" box="[812,1173,1834,1858]" class="Anthozoa" family="Endophyllidae" genus="Smithiphyllum" higherTaxonomySource="GBIF" kingdom="Animalia" pageId="1" pageNumber="548" phylum="Cnidaria" rank="genus">
|
||||
<emphasis id="4F8F7777FF8D36093723F8B4FC07E931" box="[812,974,1834,1858]" italics="true" pageId="1" pageNumber="548">Smithiphyllum</emphasis>
|
||||
<bibRefCitation id="196AD694FF8D360937DAF8B4FB5CE931" author="Birenheide, R." box="[981,1173,1834,1858]" pageId="1" pageNumber="548" pagination="41 - 99" refId="ref6959" refString="Birenheide, R. 1962. Revision der koloniebildenden Spongophyllidae und Stringophyllidae aus dem Devon. Senckenbergiana lethaea 43 (1): 41 - 99." type="journal article" year="1962">Birenheide, 1962</bibRefCitation>
|
||||
</taxonomicName>
|
||||
(
|
||||
<bibRefCitation id="196AD694FF8D360930ACF8B4FC82E911" author="McLean, R. A. & Pedder, A. E. H." pageId="1" pageNumber="548" pagination="1 - 38" refId="ref8223" refString="McLean, R. A. and Pedder, A. E. H. 1984. Frasnian rugose corals of western Canada. Part 1: Chonophyllidae and Kyphophyllidae. Palaeontographica A 184 (1 - 3): 1 - 38." type="journal article" year="1984">McLean and Pedder 1984: 28</bibRefCitation>
|
||||
;
|
||||
<bibRefCitation id="196AD694FF8D36093758F8D4FBC6E911" author="Sorauf, J. E." box="[855,1039,1866,1890]" pageId="1" pageNumber="548" pagination="1 - 159" refId="ref8929" refString="Sorauf, J. E. 1998. Frasnian (Upper Devonian) rugose corals from the Lime Creek and Shell Rock Formations of Iowa. Bulletins of American Paleontology 113 (355): 1 - 159." type="journal article" year="1998">Sorauf 1998: 49</bibRefCitation>
|
||||
).
|
||||
</paragraph>
|
||||
<paragraph id="7D44AB65FF8D360A3723F8ECFE0CEFF3" blockId="1.[812,1485,1906,2026]" lastBlockId="2.[102,774,232,384]" lastPageId="2" lastPageNumber="549" pageId="1" pageNumber="548">
|
||||
<emphasis id="4F8F7777FF8D36093723F8ECFC79E9FA" box="[812,944,1906,1929]" italics="true" pageId="1" pageNumber="548">Occurrence</emphasis>
|
||||
.—The stratigraphic occurrence of
|
||||
<taxonomicName id="BAFBD0E6FF8D3609317BF8ECFC4FE9D9" authorityName="Fenton and Fenton" authorityYear="1924" class="Anthozoa" family="Chonophyllidae" genus="Tabulophyllum" higherTaxonomySource="GBIF" kingdom="Animalia" pageId="1" pageNumber="548" phylum="Cnidaria" rank="genus">
|
||||
<emphasis id="4F8F7777FF8D3609317BF8ECFC4FE9D9" italics="true" pageId="1" pageNumber="548">Tabulophyllum</emphasis>
|
||||
</taxonomicName>
|
||||
is mainly Upper Devonian and the genus is globally distributed in the Frasnian. Only a few species are known from the Lower Devonian of
|
||||
<collectingCountry id="05ECEBF5FF8D36093072F84CFB2DE999" box="[1149,1252,2002,2026]" name="Australia" pageId="1" pageNumber="548">Australia</collectingCountry>
|
||||
and
|
||||
<collectingCountry id="05ECEBF5FF8D36093112F84CFAB4E999" box="[1309,1405,2002,2026]" name="Belgium" pageId="1" pageNumber="548">Belgium</collectingCountry>
|
||||
(
|
||||
<bibRefCitation id="196AD694FF8D360A3182F84CFF68EF72" author="Tsien, H. H." lastPageId="2" lastPageNumber="549" pageId="1" pageNumber="548" pagination="263 - 282" refId="ref9333" refString="Tsien, H. H. 1977. Especes du genre Tabulophyllum (Rugosa) dans le Devonien moyen et le Frasnien de la Belgique. Annales de la Societe Geologique de Belgique 99 (2): 263 - 282." type="journal article" year="1977">Tsien 1977</bibRefCitation>
|
||||
;
|
||||
<bibRefCitation id="196AD694FF8E360A34BEFF76FEEBEF72" author="Hill, D." box="[177,290,232,257]" pageId="2" pageNumber="549" pagination="13 - 22" refId="ref7772" refString="Hill, D. 1942. The Lower Devonian rugose corals from the Mt. Etna Limestone, Qld. Proceedings of the Royal Society of Queensland 54 (2): 13 - 22." type="journal article" year="1942">Hill 1942</bibRefCitation>
|
||||
;
|
||||
<bibRefCitation id="196AD694FF8E360A353DFF76FE0AEF72" author="Sorauf, J. E." box="[306,451,232,257]" pageId="2" pageNumber="549" pagination="397 - 412" refId="ref8715" refString="Sorauf, J. E. 1989. The Devonian rugose coral genus Tabulophyllum Fenton andFenton, 1924. In: N. J. McMillan, A. F. Embry, andD. J. Glass (eds.), Devonian of the World (Proceedings of the Second International SymposiumontheDevonianSystemCalgary, Canada), Canadian Society of Petroleum Geologists, Memoir 14 (3): 397 - 412." type="journal article" year="1989">Sorauf 1989</bibRefCitation>
|
||||
;
|
||||
<bibRefCitation id="196AD694FF8E360A35DCFF76FD9AEF73" author="Zhen, Y. Y." box="[467,595,232,256]" pageId="2" pageNumber="549" pagination="193 - 234" refId="ref9656" refString="Zhen, Y. Y. 1995. Late Emsian rugose corals from the Mount Podge area, Burdekin basin, north Queensland. Alcheringa 19: 193 - 234." type="journal article" year="1995">Zhen 1995</bibRefCitation>
|
||||
). However, the known Lower Devonian species assigned to
|
||||
<taxonomicName id="BAFBD0E6FF8E360A3653FE96FCCFEF53" authorityName="Fenton and Fenton" authorityYear="1924" box="[604,774,264,288]" class="Anthozoa" family="Chonophyllidae" genus="Tabulophyllum" higherTaxonomySource="GBIF" kingdom="Animalia" pageId="2" pageNumber="549" phylum="Cnidaria" rank="genus">
|
||||
<emphasis id="4F8F7777FF8E360A3653FE96FCCFEF53" box="[604,774,264,288]" italics="true" pageId="2" pageNumber="549">Tabulophyllum</emphasis>
|
||||
</taxonomicName>
|
||||
closely resemble the Upper Devonian forms in their general morphology, withlong majorsepta commonly interrupted by large lonsdaleoid dissepiments.
|
||||
</paragraph>
|
||||
</subSubSection>
|
||||
</treatment>
|
||||
</document>
|
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