171 lines
22 KiB
XML
171 lines
22 KiB
XML
<document id="B340D057D7C42CCA58969508AEBF398F" ID-DOI="10.1080/14772019.2017.1412362" ID-ISSN="1478-0941" ID-Zenodo-Dep="10883381" IM.bibliography_approvedBy="diego" IM.illustrations_approvedBy="diego" IM.materialsCitations_approvedBy="felipe" IM.metadata_approvedBy="felipe" IM.tables_approvedBy="diego" IM.taxonomicNames_approvedBy="diego" IM.treatments_approvedBy="diego" checkinTime="1711484105509" checkinUser="felipe" docAuthor="Georgieva, Magdalena N., Little, Crispin T. S., Watson, Jonathan S., Sephton, Mark A., Ball, Alexander D. & Glover, Adrian G." docDate="2019" docId="03C0814B9036FFB03F43F8F84F12FC77" docLanguage="en" docName="JSystPalaeontol.17.4.287-329.pdf" docOrigin="Journal of Systematic Palaeontology 17 (4)" docSource="http://dx.doi.org/10.1080/14772019.2017.1412362" docStyle="DocumentStyle:602474738E3D100F0F13788B53F61545.3:JSystPalaeontol.2016-.journal_article.open" docStyleId="602474738E3D100F0F13788B53F61545" docStyleName="JSystPalaeontol.2016-.journal_article.open" docStyleVersion="3" docTitle="Siboglinidae Caullery 1914" docType="treatment" docVersion="2" lastPageNumber="297" masterDocId="FFF9F933903CFFBB3E4CFFA14E0EFF1E" masterDocTitle="Identification of fossil worm tubes from Phanerozoic hydrothermal vents and cold seeps" masterLastPageNumber="329" masterPageNumber="287" pageNumber="296" updateTime="1712152197148" updateUser="diego" zenodo-license-document="CC-BY-4.0">
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<mods:title id="0934E89E234A8CFF0AF923EA286581E2">Identification of fossil worm tubes from Phanerozoic hydrothermal vents and cold seeps</mods:title>
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<mods:namePart id="9879DAFE18DDD355CDFD88DDFD812FB3">Georgieva, Magdalena N.</mods:namePart>
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<mods:affiliation id="58789E0230B3737B5548D77E340A2CD9">Department of Life Sciences, Natural History Museum, London, United Kingdom; & School of Earth and Environment, University of Leeds, Leeds, United Kingdom;</mods:affiliation>
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<mods:namePart id="A9C3254393A650B2CDE17FB269F57A05">Little, Crispin T. S.</mods:namePart>
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<mods:affiliation id="2BF3F77B63E8145652339B6D823D786E">School of Earth and Environment, University of Leeds, Leeds, United Kingdom;</mods:affiliation>
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<mods:namePart id="FB01B5CDAFEF142B9AB9B6D3DF2D807E">Watson, Jonathan S.</mods:namePart>
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<mods:affiliation id="617E6550C7C4A0328F34F6CAF22CA23E">Department of Earth Science and Engineering, Imperial College London, London, United Kingdom;</mods:affiliation>
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<mods:namePart id="781E906DAF09B0DA90C59CC3D3732772">Sephton, Mark A.</mods:namePart>
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<mods:affiliation id="2B6EB1754A3DA76E7DF6F3D15D152926">Department of Earth Science and Engineering, Imperial College London, London, United Kingdom;</mods:affiliation>
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<mods:namePart id="5F275745EDE57DC7A75BA4F28630373E">Ball, Alexander D.</mods:namePart>
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<mods:affiliation id="977970A7A81FB9D74D21A81F517BADC2">Core Research Laboratories, Natural History Museum, London, United Kingdom</mods:affiliation>
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<mods:namePart id="340AF73011914E49401930708B199FCE">Glover, Adrian G.</mods:namePart>
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<mods:affiliation id="CB8B92C05B67C673C3D02328594E6308">Department of Life Sciences, Natural History Museum, London, United Kingdom;</mods:affiliation>
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<mods:title id="38B1C5A2EF257A16459C0BA77B7B4C54">Journal of Systematic Palaeontology</mods:title>
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<mods:date id="D3E00BD7518131A62F878DD5768666B7">2019</mods:date>
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<mods:number id="538F2B61F401407E48441FF356013F36">2017-12-28</mods:number>
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<mods:identifier id="853F97690246CFD834A5FDDC103C3593" type="ISSN">1478-0941</mods:identifier>
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<treatment id="03C0814B9036FFB03F43F8F84F12FC77" LSID="urn:lsid:plazi:treatment:03C0814B9036FFB03F43F8F84F12FC77" httpUri="http://treatment.plazi.org/id/03C0814B9036FFB03F43F8F84F12FC77" lastPageId="11" lastPageNumber="297" pageId="10" pageNumber="296">
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<subSubSection id="C37363D69036FFB13F43F8F84C90F86E" box="[271,670,1881,1904]" pageId="10" pageNumber="296" type="nomenclature">
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<paragraph id="8BD6305D9036FFB13F43F8F84C90F86E" blockId="10.[271,670,1881,1904]" box="[271,670,1881,1904]" pageId="10" pageNumber="296">
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<heading id="D09E87319036FFB13F43F8F84C90F86E" box="[271,670,1881,1904]" centered="true" fontSize="10" level="2" pageId="10" pageNumber="296" reason="7">
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?Family
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<taxonomicName id="4C694BDE9036FFB13F21F8F84C90F86E" ID-CoL="84KRZ" authority="Caullery, 1914" authorityName="Caullery" authorityYear="1914" box="[365,670,1881,1904]" class="Polychaeta" family="Siboglinidae" isUncertain="true" kingdom="Animalia" order="Sabellida" pageId="10" pageNumber="296" phylum="Annelida" rank="family">
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<emphasis id="B91DEC4F9036FFB13F21F8F84FF4F86E" bold="true" box="[365,506,1881,1904]" pageId="10" pageNumber="296">Siboglinidae</emphasis>
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<bibRefCitation id="EFF84DAC9036FFB13C4CF8F84C90F86E" author="Caullery, M." box="[512,670,1881,1904]" pageId="10" pageNumber="296" pagination="2014 - 2017" refId="ref22158" refString="Caullery, M. 1914. Sur les Siboglinidae, type nouveau d'invert´ebr´es receuillis par l'exp´edition du Siboga. Comptes Rendus Hebdomadaires des Seances´de l'Academie´des Sciences, 158, 2014 - 2017." type="journal article" year="1914">Caullery, 1914</bibRefCitation>
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</taxonomicName>
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</heading>
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</paragraph>
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<subSubSection id="C37363D69036FFB13F1DF8D84C55F88E" box="[337,603,1913,1936]" pageId="10" pageNumber="296" type="vernacular_names">
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<paragraph id="8BD6305D9036FFB13F1DF8D84C55F88E" blockId="10.[337,603,1913,1968]" box="[337,603,1913,1936]" pageId="10" pageNumber="296">
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<emphasis id="B91DEC4F9036FFB13F1DF8D84C55F88E" bold="true" box="[337,603,1913,1936]" pageId="10" pageNumber="296">‘Murdock Creek tubes’</emphasis>
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</paragraph>
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</subSubSection>
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<subSubSection id="C37363D69036FFB13FE2F8384FF0F8AE" box="[430,510,1945,1968]" pageId="10" pageNumber="296" type="description">
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<paragraph id="8BD6305D9036FFB13FE2F8384FF0F8AE" blockId="10.[337,603,1913,1968]" box="[430,510,1945,1968]" pageId="10" pageNumber="296">
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(
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<figureCitation id="13522CD89036FFB13FFBF8384FFBF8AE" box="[439,501,1945,1968]" captionStart="Figure 5" captionStartId="10.[159,227,1419,1440]" captionTargetBox="[174,1451,184,1385]" captionTargetId="figure-186@10.[173,1453,183,1387]" captionTargetPageId="10" captionText="Figure 5. ‘Murdock Creek tubes’, WA-MC LACMIP loc. 6295, Early Oligocene, Washington State, USA. A, a single tube in hand specimen possibly bearing longitudinal wrinkles. B, detail of tube wall in transverse section with thick, multi-layered and delaminated tube wall. C, transverse section of tube which appears to have originally been flexible. D, detail of tube wall where a preserved tear occurs, revealing fibre endings (grey arrow). Scale bars: A = 5 mm; B = 150 µm; C = 100 µm; D = 50 µm." figureDoi="http://doi.org/10.5281/zenodo.10883391" httpUri="https://zenodo.org/record/10883391/files/figure.png" pageId="10" pageNumber="296">Fig. 5</figureCitation>
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)
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</paragraph>
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||
</subSubSection>
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<subSubSection id="C37363D69036FFB13D01F9B64DC0F852" pageId="10" pageNumber="296" type="materials_examined">
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<paragraph id="8BD6305D9036FFB13D01F9B64DD1F993" blockId="10.[845,1467,1559,1677]" pageId="10" pageNumber="296">
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<emphasis id="B91DEC4F9036FFB13D01F9B64DB9F930" bold="true" box="[845,951,1559,1582]" pageId="10" pageNumber="296">Material.</emphasis>
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WA-MC LACMIP loc. 6295, one spiralling tube (
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<figureCitation id="13522CD89036FFB13DDCF9964DE4F950" box="[912,1002,1591,1614]" captionStart="Figure 5" captionStartId="10.[159,227,1419,1440]" captionTargetBox="[174,1451,184,1385]" captionTargetId="figure-186@10.[173,1453,183,1387]" captionTargetPageId="10" captionText="Figure 5. ‘Murdock Creek tubes’, WA-MC LACMIP loc. 6295, Early Oligocene, Washington State, USA. A, a single tube in hand specimen possibly bearing longitudinal wrinkles. B, detail of tube wall in transverse section with thick, multi-layered and delaminated tube wall. C, transverse section of tube which appears to have originally been flexible. D, detail of tube wall where a preserved tear occurs, revealing fibre endings (grey arrow). Scale bars: A = 5 mm; B = 150 µm; C = 100 µm; D = 50 µm." figureDoi="http://doi.org/10.5281/zenodo.10883391" httpUri="https://zenodo.org/record/10883391/files/figure.png" pageId="10" pageNumber="296">Fig. 5A</figureCitation>
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), another tube with a
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<emphasis id="B91DEC4F9036FFB13AA2F9974B0DF950" bold="true" box="[1262,1283,1590,1614]" pageId="10" pageNumber="296">~</emphasis>
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||
90
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||
<superScript id="7C1C9D159036FFB13B52F9934B29F95D" attach="left" box="[1310,1319,1586,1603]" fontSize="7" pageId="10" pageNumber="296">º</superScript>
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||
bend, and a smaller tube observed in thin section only. Donated by J. L. Goedert.
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</paragraph>
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||
<paragraph id="8BD6305D9036FFB13D01F9144DC0F852" blockId="10.[845,1467,1717,1868]" pageId="10" pageNumber="296">
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||
<emphasis id="B91DEC4F9036FFB13D01F9144DD7F9D2" bold="true" box="[845,985,1717,1740]" pageId="10" pageNumber="296">Occurrence.</emphasis>
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Murdock Creek, Clallam County,
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<collectingRegion id="49ADFEBF9036FFB13B1FF9144DBCF9F2" country="United States of America" name="Washington" pageId="10" pageNumber="296">Washington State</collectingRegion>
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,
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<collectingCountry id="F37E70CD9036FFB13D8DF9744DF8F9F2" box="[961,1014,1749,1772]" name="United States of America" pageId="10" pageNumber="296">USA</collectingCountry>
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||
(
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<emphasis id="B91DEC4F9036FFB13A46F9754A11F9F2" bold="true" box="[1034,1055,1748,1772]" pageId="10" pageNumber="296">~</emphasis>
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||
48
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||
<superScript id="7C1C9D159036FFB13A76F9714A4DF9FF" attach="none" box="[1082,1091,1744,1761]" fontSize="7" pageId="10" pageNumber="296">º</superScript>
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9
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<emphasis id="B91DEC4F9036FFB13A19F9714A54F9FF" bold="true" box="[1109,1114,1744,1761]" pageId="10" pageNumber="296">
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<superScript id="7C1C9D159036FFB13A19F9714A54F9FF" attach="right" box="[1109,1114,1744,1761]" fontSize="7" pageId="10" pageNumber="296">'</superScript>
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</emphasis>
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||
N, 123
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<superScript id="7C1C9D159036FFB13AE4F9714ABFF9FF" attach="none" box="[1192,1201,1744,1761]" fontSize="7" pageId="10" pageNumber="296">º</superScript>
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52
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<emphasis id="B91DEC4F9036FFB13A9CF9714ADBF9FF" bold="true" box="[1232,1237,1744,1761]" pageId="10" pageNumber="296">
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||
<superScript id="7C1C9D159036FFB13A9CF9714ADBF9FF" attach="right" box="[1232,1237,1744,1761]" fontSize="7" pageId="10" pageNumber="296">'</superScript>
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</emphasis>
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W). Loose seep carbonate blocks. Pysht Formation, late Early Oligocene (
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<bibRefCitation id="EFF84DAC9036FFB13D18F8B44A63F832" author="Goedert, J. L. & Squires, R. L." box="[852,1133,1813,1836]" pageId="10" pageNumber="296" pagination="72 - 77" refId="ref22692" refString="Goedert, J. L. & Squires, R. L. 1993. First Oligocene records of Calyptogena (Bivalvia: Vesicomyidae). Veliger, 36, 72 - 77." type="journal article" year="1993">Goedert & Squires 1993</bibRefCitation>
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||
;
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||
<bibRefCitation id="EFF84DAC9036FFB13ACEF8B44B7EF832" author="Kiel, S. & Amano, K." box="[1154,1392,1813,1836]" pageId="10" pageNumber="296" pagination="589 - 602" refId="ref23652" refString="Kiel, S. & Amano, K. 2013. The earliest bathymodiolin mussels: an evaluation of Eocene and Oligocene taxa from deep-sea methane seep deposits in western Washington State, USA. Journal of Paleontology, 87, 589 - 602." type="journal article" year="2013">Kiel & Amano 2013</bibRefCitation>
|
||
;
|
||
<bibRefCitation id="EFF84DAC9036FFB13BC9F8B44DB0F852" author="Vinn, O. & Kupriyanova, E. K. & Kiel, S." pageId="10" pageNumber="296" pagination="35 - 41" refId="ref25765" refString="Vinn, O., Kupriyanova, E. K. & Kiel, S. 2013. Serpulids (Annelida, Polychaeta) at Cretaceous to modern hydrocarbon seeps: ecological and evolutionary patterns. Palaeogeography, Palaeoclimatology, Palaeoecology, 390, 35 - 41." type="journal article" year="2013">
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||
Vinn
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||
<emphasis id="B91DEC4F9036FFB13D01F8944D8DF852" box="[845,899,1845,1868]" italics="true" pageId="10" pageNumber="296">et al.</emphasis>
|
||
2013
|
||
</bibRefCitation>
|
||
).
|
||
</paragraph>
|
||
</subSubSection>
|
||
<subSubSection id="C37363D69036FFB03D01F8D24F55FEAA" lastPageId="11" lastPageNumber="297" pageId="10" pageNumber="296" type="description">
|
||
<paragraph id="8BD6305D9036FFB03D01F8D24F55FEAA" blockId="10.[845,1467,1907,1994]" lastBlockId="11.[159,781,189,436]" lastPageId="11" lastPageNumber="297" pageId="10" pageNumber="296">
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||
<emphasis id="B91DEC4F9036FFB13D01F8D24DD6F894" bold="true" box="[845,984,1907,1930]" pageId="10" pageNumber="296">Description.</emphasis>
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Carbonate tubes 0.7–3.0 mm in diameter, appearing non-branched, non-agglutinated and nontapering in the tube fragments observed. The spiralling tube (
|
||
<figureCitation id="13522CD89037FFB03EACFF1C4F3BFFCA" box="[224,309,189,212]" captionStart="Figure 5" captionStartId="10.[159,227,1419,1440]" captionTargetBox="[174,1451,184,1385]" captionTargetId="figure-186@10.[173,1453,183,1387]" captionTargetPageId="10" captionText="Figure 5. ‘Murdock Creek tubes’, WA-MC LACMIP loc. 6295, Early Oligocene, Washington State, USA. A, a single tube in hand specimen possibly bearing longitudinal wrinkles. B, detail of tube wall in transverse section with thick, multi-layered and delaminated tube wall. C, transverse section of tube which appears to have originally been flexible. D, detail of tube wall where a preserved tear occurs, revealing fibre endings (grey arrow). Scale bars: A = 5 mm; B = 150 µm; C = 100 µm; D = 50 µm." figureDoi="http://doi.org/10.5281/zenodo.10883391" httpUri="https://zenodo.org/record/10883391/files/figure.png" pageId="11" pageNumber="297">Fig. 5A</figureCitation>
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||
) appears to have coarse longitudinal wrinkles on its surface, but whether these are original is uncertain. In thin section, tube walls are thick and concentrically multi-layered (
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<figureCitation id="13522CD89037FFB03FAAFEBC4C53FE2A" box="[486,605,285,308]" captionStart="Figure 5" captionStartId="10.[159,227,1419,1440]" captionTargetBox="[174,1451,184,1385]" captionTargetId="figure-186@10.[173,1453,183,1387]" captionTargetPageId="10" captionText="Figure 5. ‘Murdock Creek tubes’, WA-MC LACMIP loc. 6295, Early Oligocene, Washington State, USA. A, a single tube in hand specimen possibly bearing longitudinal wrinkles. B, detail of tube wall in transverse section with thick, multi-layered and delaminated tube wall. C, transverse section of tube which appears to have originally been flexible. D, detail of tube wall where a preserved tear occurs, revealing fibre endings (grey arrow). Scale bars: A = 5 mm; B = 150 µm; C = 100 µm; D = 50 µm." figureDoi="http://doi.org/10.5281/zenodo.10883391" httpUri="https://zenodo.org/record/10883391/files/figure.png" pageId="11" pageNumber="297">Fig. 5B–D</figureCitation>
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), and occasionally delaminated (
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<figureCitation id="13522CD89037FFB03F2BFE9C4FB3FE4A" box="[359,445,317,340]" captionStart="Figure 5" captionStartId="10.[159,227,1419,1440]" captionTargetBox="[174,1451,184,1385]" captionTargetId="figure-186@10.[173,1453,183,1387]" captionTargetPageId="10" captionText="Figure 5. ‘Murdock Creek tubes’, WA-MC LACMIP loc. 6295, Early Oligocene, Washington State, USA. A, a single tube in hand specimen possibly bearing longitudinal wrinkles. B, detail of tube wall in transverse section with thick, multi-layered and delaminated tube wall. C, transverse section of tube which appears to have originally been flexible. D, detail of tube wall where a preserved tear occurs, revealing fibre endings (grey arrow). Scale bars: A = 5 mm; B = 150 µm; C = 100 µm; D = 50 µm." figureDoi="http://doi.org/10.5281/zenodo.10883391" httpUri="https://zenodo.org/record/10883391/files/figure.png" pageId="11" pageNumber="297">Fig. 5B</figureCitation>
|
||
). Some of the tubes appear to have originally been flexible (
|
||
<figureCitation id="13522CD89037FFB03FBDFEFC4C48FE6A" box="[497,582,349,372]" captionStart="Figure 5" captionStartId="10.[159,227,1419,1440]" captionTargetBox="[174,1451,184,1385]" captionTargetId="figure-186@10.[173,1453,183,1387]" captionTargetPageId="10" captionText="Figure 5. ‘Murdock Creek tubes’, WA-MC LACMIP loc. 6295, Early Oligocene, Washington State, USA. A, a single tube in hand specimen possibly bearing longitudinal wrinkles. B, detail of tube wall in transverse section with thick, multi-layered and delaminated tube wall. C, transverse section of tube which appears to have originally been flexible. D, detail of tube wall where a preserved tear occurs, revealing fibre endings (grey arrow). Scale bars: A = 5 mm; B = 150 µm; C = 100 µm; D = 50 µm." figureDoi="http://doi.org/10.5281/zenodo.10883391" httpUri="https://zenodo.org/record/10883391/files/figure.png" pageId="11" pageNumber="297">Fig. 5C</figureCitation>
|
||
) and to have had fibrous walls due to visible preserved wall tears in thin section (
|
||
<figureCitation id="13522CD89037FFB03EB6FE3C4F40FEAA" box="[250,334,413,436]" captionStart="Figure 5" captionStartId="10.[159,227,1419,1440]" captionTargetBox="[174,1451,184,1385]" captionTargetId="figure-186@10.[173,1453,183,1387]" captionTargetPageId="10" captionText="Figure 5. ‘Murdock Creek tubes’, WA-MC LACMIP loc. 6295, Early Oligocene, Washington State, USA. A, a single tube in hand specimen possibly bearing longitudinal wrinkles. B, detail of tube wall in transverse section with thick, multi-layered and delaminated tube wall. C, transverse section of tube which appears to have originally been flexible. D, detail of tube wall where a preserved tear occurs, revealing fibre endings (grey arrow). Scale bars: A = 5 mm; B = 150 µm; C = 100 µm; D = 50 µm." figureDoi="http://doi.org/10.5281/zenodo.10883391" httpUri="https://zenodo.org/record/10883391/files/figure.png" pageId="11" pageNumber="297">Fig. 5D</figureCitation>
|
||
).
|
||
</paragraph>
|
||
</subSubSection>
|
||
<subSubSection id="C37363D69037FFB03ED3FE724F12FC77" pageId="11" pageNumber="297" type="discussion">
|
||
<paragraph id="8BD6305D9037FFB03ED3FE724F12FC77" blockId="11.[159,781,467,873]" pageId="11" pageNumber="297">
|
||
<emphasis id="B91DEC4F9037FFB03ED3FE724F00FEF4" bold="true" box="[159,270,467,490]" pageId="11" pageNumber="297">Remarks.</emphasis>
|
||
These tubes appear to have been organic originally due to preserved tube wall tears that reveal a fibrous nature. The size of the tubes, their thick, multi-layered walls and the spiralling that they exhibit suggest that the tubes may have been made by vestimentiferans, as the combination of these features are not commonly encountered in other organic tube-building annelids that occur at vents and seeps. Due to a limited amount of material available for study, and as these tubes were only resolved among those of siboglinids when homoplastic characters are downweighted less within cladistic analyses (
|
||
<figureCitation id="13522CD89037FFB03EE4FC934F04FC57" box="[168,266,818,841]" captionStart="Figure 23" captionStartId="34.[159,227,1279,1300]" captionTargetBox="[173,1453,183,1247]" captionTargetId="figure-219@34.[173,1453,183,1247]" captionTargetPageId="34" captionText="Figure 23. Strict consensus cladograms constructed using a total of 64 modern and fossil annelid taxa and 48 mostly morphological tube characters. Analyses were performed using implied character weighting, with the concavity constant set as default (k = 3; A), and also set to downweight homoplastic characters less (k = 4; B). Numbers on nodes represent groups present/contradicted support values. Modern taxa are coloured according to taxonomic groups; fossil taxa are in grey. A, consensus of 271 most parsimonious trees (best score = 15.387, consistency index = 0.195, retention index = 0.264); B, consensus of 60 most parsimonious trees (best score = 13.568, consistency index = 0.232, retention index = 0.569). Symbols/colours indicate taxonomic affinities." figureDoi="http://doi.org/10.5281/zenodo.10883427" httpUri="https://zenodo.org/record/10883427/files/figure.png" pageId="11" pageNumber="297">Fig. 23B</figureCitation>
|
||
), the tubes are only tentatively assigned to the siboglinids.
|
||
</paragraph>
|
||
</subSubSection>
|
||
</treatment>
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||
</document> |