treatments-xml/data/42/30/87/423087B2FFD6FF97FF40FE88F0AEFB88.xml
2024-06-21 12:34:44 +02:00

128 lines
16 KiB
XML

<document id="EFE620F19D678769F4BF7A4293BEF118" ID-DOI="10.35463/j.apr.2022.01.03" ID-ISSN="1842-371x" ID-Zenodo-Dep="10520845" IM.bibliography_approvedBy="juliana" IM.materialsCitations_approvedBy="juliana" IM.metadata_approvedBy="juliana" IM.taxonomicNames_approvedBy="juliana" IM.treatments_approvedBy="juliana" checkinTime="1705451459016" checkinUser="felipe" docAuthor="SCHLAGINTWEIT, FELIX" docDate="2021" docId="423087B2FFD6FF97FF40FE88F0AEFB88" docLanguage="en" docName="ActaPalaeontolRom.18.1.17-23.pdf" docOrigin="Acta Palaeontologica Romaniae 18 (1)" docSource="http://dx.doi.org/10.35463/j.apr.2022.01.03" docStyle="DocumentStyle:CA474AAD92E97C533D63E0C5C0F159F1.1:ActaPalaeontolRom.2019-.journal_article" docStyleId="CA474AAD92E97C533D63E0C5C0F159F1" docStyleName="ActaPalaeontolRom.2019-.journal_article" docStyleVersion="1" docTitle="Mesorbitolina parva" docType="treatment" docVersion="1" lastPageNumber="18" masterDocId="BE09FFCAFFD7FF96FFD7FF8AF21FFFBB" masterDocTitle="Orbitolinids And Other Larger Benthic Foraminifera From The Aptian-Albian Of Tibet: Critical Discussion Of Some Recently Published Data" masterLastPageNumber="23" masterPageNumber="17" pageNumber="18" updateTime="1712865678635" updateUser="juliana" zenodo-license-document="CC-BY-4.0">
<mods:mods id="5E2DC08F3B1CEF0275E29DFA61E7F721" xmlns:mods="http://www.loc.gov/mods/v3">
<mods:titleInfo id="6E1978ECB5DDC7C827ABA1EF1B7B823C">
<mods:title id="73679CF1E57D1A0617028511FA2D65EB">Orbitolinids And Other Larger Benthic Foraminifera From The Aptian-Albian Of Tibet: Critical Discussion Of Some Recently Published Data</mods:title>
</mods:titleInfo>
<mods:name id="67B63798A7A345481A4CF9CFB54FB78A" type="personal">
<mods:role id="E3117D8553A85D4FE541167A81CBF243">
<mods:roleTerm id="920336CDAF76D5A518A4BF3B0F61846D">Author</mods:roleTerm>
</mods:role>
<mods:namePart id="A52AB8AEB5CEF4F96D4FCC7C30486F9F">SCHLAGINTWEIT, FELIX</mods:namePart>
<mods:affiliation id="97516F5961AFCBA6CF559CFFAF67CAF3">Lerchenauerstr. 167, 80935 Munich, Germany</mods:affiliation>
<mods:nameIdentifier id="70742814BDB1B3075B2FB71358C7A540" type="email">felix.schlagintweit@gmx.de</mods:nameIdentifier>
</mods:name>
<mods:typeOfResource id="5D48444DA98FAD79B42D58995EF0FB4B">text</mods:typeOfResource>
<mods:relatedItem id="0C16BE6D2347592418AF59CE1750342D" type="host">
<mods:titleInfo id="C114718464738A02EDCC93017EE6DC76">
<mods:title id="7D86650DCFCD09B2397809BA17C526CC">Acta Palaeontologica Romaniae</mods:title>
</mods:titleInfo>
<mods:part id="E654F6797E046E00A75585EF773A0F0B">
<mods:date id="CFD09A37344C714C41A8D44D4B8FDB1F">2021</mods:date>
<mods:detail id="75EE965AB256BA1EFD3AE6B0B7D01B2C" type="pubDate">
<mods:number id="71278933909589A5940A3856A2FF38A9">2021-09-09</mods:number>
</mods:detail>
<mods:detail id="69AFC65E5B005AE6F01C576DFF981A97" type="volume">
<mods:number id="63D8952C2FB316D094DA39F01F6262EF">18</mods:number>
</mods:detail>
<mods:detail id="41BB2365EC2423970AB9100BDEDA4FE2" type="issue">
<mods:number id="BF808FCADECB3FE74E269A78D2C859A7">1</mods:number>
</mods:detail>
<mods:extent id="C0DCC7D6066DCCE4A7F3A77DA9BB3BD2" unit="page">
<mods:start id="3FA7149A2375E41522B93D8CA2833783">17</mods:start>
<mods:end id="8C9B1AC542FE588F05EC26A64FF101DF">23</mods:end>
</mods:extent>
</mods:part>
</mods:relatedItem>
<mods:location id="DCA0C22DF6868D0F5CA00407E15700A5">
<mods:url id="4E32F15C1E5BDAEB9330CDB8CEAF2CD6">http://dx.doi.org/10.35463/j.apr.2022.01.03</mods:url>
</mods:location>
<mods:classification id="ABC84A0B08511FE1A446A608165931B5">journal article</mods:classification>
<mods:identifier id="314F1B86A73FEB4822FC351B31C424A2" type="DOI">10.35463/j.apr.2022.01.03</mods:identifier>
<mods:identifier id="8412905BD359AD2BAD1954F7858F8097" type="ISSN">1842-371x</mods:identifier>
<mods:identifier id="DDB0B4E0D66B3C3BF58EB2D558EAE638" type="Zenodo-Dep">10520845</mods:identifier>
</mods:mods>
<treatment id="423087B2FFD6FF97FF40FE88F0AEFB88" LSID="urn:lsid:plazi:treatment:423087B2FFD6FF97FF40FE88F0AEFB88" httpUri="http://treatment.plazi.org/id/423087B2FFD6FF97FF40FE88F0AEFB88" lastPageNumber="18" pageId="1" pageNumber="18">
<subSubSection id="8283652FFFD6FF97FF40FE88F0B2FEA1" box="[151,685,258,282]" pageId="1" pageNumber="18" type="nomenclature">
<paragraph id="CA2636A4FFD6FF97FF40FE88F0B2FEA1" blockId="1.[151,685,258,314]" box="[151,685,258,282]" pageId="1" pageNumber="18">
<emphasis id="F8EDEAB6FFD6FF97FF40FE88F0B2FEA1" bold="true" box="[151,685,258,282]" pageId="1" pageNumber="18">
Record of
<taxonomicName id="0D994D27FFD6FF97FED9FE88F0B2FEA1" ID-CoL="82Y2M" authority="(Douglass, 1960)" baseAuthorityName="Douglass" baseAuthorityYear="1960" box="[270,685,258,282]" class="Globothalamea" family="Orbitolinidae" genus="Mesorbitolina" kingdom="Chromista" order="Loftusiida" pageId="1" pageNumber="18" phylum="Foraminifera" rank="species" species="parva">
<emphasis id="F8EDEAB6FFD6FF97FED9FE88F3F3FEA1" bold="true" box="[270,492,258,282]" italics="true" pageId="1" pageNumber="18">Mesorbitolina parva</emphasis>
(
<bibRefCitation id="AE084B55FFD6FF97FE2CFE88F0B8FEA1" author="Douglass, R. C." box="[507,679,258,282]" pageId="1" pageNumber="18" pagination="1 - 52" refId="ref3997" refString="Douglass, R. C., 1960. The foraminiferal genus Orbitolina in North America. Geological Survey Professional Papers, 333: 1 - 52." type="journal article" year="1960">Douglass, 1960</bibRefCitation>
)
</taxonomicName>
</emphasis>
</paragraph>
</subSubSection>
<subSubSection id="8283652FFFD6FF97FF40FEA8F2E4FE81" box="[151,251,290,314]" pageId="1" pageNumber="18" type="description">
<paragraph id="CA2636A4FFD6FF97FF40FEA8F2E4FE81" blockId="1.[151,685,258,314]" box="[151,251,290,314]" pageId="1" pageNumber="18">
(
<figureCitation id="52A22A21FFD6FF97FF48FEA8F2EEFE81" box="[159,241,290,314]" captionStart="Fig" captionStartId="2.[225,260,455,476]" captionTargetBox="[225,1363,155,419]" captionTargetId="figure-1358@2.[225,1363,155,419]" captionTargetPageId="2" captionText="Fig. 1. A, Mesorbitolina parva (Douglass) fide BouDagher-Fadel et al. (2017, excerpt of fig. 8), Lower Cretaceous of Tibet. B-E, Praeorbitolina cormyi Schroeder, axial sections perpendicular to the median plane (B-C: excerpt of Bosselini et al., 1999, fig. 5a and 5g, early Aptian of Ethiopia; D-E: early Aptian of Iran). Figures without scale." figureDoi="http://doi.org/10.5281/zenodo.10520847" httpUri="https://zenodo.org/record/10520847/files/figure.png" pageId="1" pageNumber="18">Fig. 1A</figureCitation>
)
</paragraph>
</subSubSection>
<subSubSection id="8283652FFFD6FF97FF40FEEEF00AFE26" pageId="1" pageNumber="18" type="reference_group">
<paragraph id="CA2636A4FFD6FF97FF40FEEEF00AFE26" blockId="1.[151,771,356,413]" pageId="1" pageNumber="18">
Referred illustrations:
<taxonomicName id="0D994D27FFD6FF97FE5EFEEEF079FEC7" baseAuthorityName="Douglass" baseAuthorityYear="1960" box="[393,614,356,380]" class="Globothalamea" family="Orbitolinidae" genus="Mesorbitolina" kingdom="Chromista" order="Loftusiida" pageId="1" pageNumber="18" phylum="Foraminifera" rank="species" species="parva">
<emphasis id="F8EDEAB6FFD6FF97FE5EFEEEF079FEC7" box="[393,614,356,380]" italics="true" pageId="1" pageNumber="18">Mesorbitolina parva</emphasis>
</taxonomicName>
, part of figure
<quantity id="0D619B41FFD6FF97FF40FE0FF2DFFE26" box="[151,192,389,413]" metricMagnitude="-1" metricUnit="m" metricValue="2.032" pageId="1" pageNumber="18" unit="in" value="8.0">8 in</quantity>
<bibRefCitation id="AE084B55FFD6FF97FF10FE0FF00EFE26" author="BouDagher-Fadel, M. &amp; Hu, X. &amp; Price, G. D. &amp; Sun, G. &amp; Wang, J. - G. &amp; An, W." box="[199,529,389,413]" pageId="1" pageNumber="18" pagination="188 - 207" refId="ref3463" refString="BouDagher-Fadel, M., Hu, X., Price, G. D., Sun, G., Wang, J. - G. &amp; An, W., 2017. Foraminiferal biostratigraphy and palaeoenvironmental analysis of the mid-Cretaceous limestones in the southern Tibetian Plateau. Journal for Foraminiferal Research, 47 (2): 188 - 207." type="journal article" year="2017">BouDagher-Fadel et al. (2017)</bibRefCitation>
.
</paragraph>
</subSubSection>
<subSubSection id="8283652FFFD6FF97FF40FE42F0AEFB88" pageId="1" pageNumber="18" type="discussion">
<paragraph id="CA2636A4FFD6FF97FF40FE42F0AEFB88" blockId="1.[151,772,456,1076]" pageId="1" pageNumber="18">
<taxonomicName id="0D994D27FFD6FF97FF40FE42F02DFE5B" authority="(Douglass, 1960)" baseAuthorityName="Douglass" baseAuthorityYear="1960" box="[151,562,456,480]" class="Globothalamea" family="Orbitolinidae" genus="Mesorbitolina" kingdom="Chromista" order="Loftusiida" pageId="1" pageNumber="18" phylum="Foraminifera" rank="species" species="parva">
<emphasis id="F8EDEAB6FFD6FF97FF40FE42F36CFE5B" box="[151,371,456,480]" italics="true" pageId="1" pageNumber="18">Mesorbitolina parva</emphasis>
(
<bibRefCitation id="AE084B55FFD6FF97FE55FE42F034FE5B" author="Douglass, R. C." box="[386,555,456,480]" pageId="1" pageNumber="18" pagination="1 - 52" refId="ref3997" refString="Douglass, R. C., 1960. The foraminiferal genus Orbitolina in North America. Geological Survey Professional Papers, 333: 1 - 52." type="journal article" year="1960">Douglass, 1960</bibRefCitation>
)
</taxonomicName>
has been described as
<taxonomicName id="0D994D27FFD6FF97FF68FE63F09EFDBA" authorityName="Zhang" authorityYear="1986" box="[191,641,489,513]" class="Globothalamea" family="Orbitolinidae" genus="Orbitolina" kingdom="Chromista" order="Loftusiida" pageId="1" pageNumber="18" phylum="Foraminifera" rank="species" species="absidata" subGenus="Columnorbitolina">
<emphasis id="F8EDEAB6FFD6FF97FF68FE63F330FDBA" box="[191,303,489,513]" italics="true" pageId="1" pageNumber="18">Orbitolina</emphasis>
(
<emphasis id="F8EDEAB6FFD6FF97FE9CFE63F015FDBA" box="[331,522,489,513]" italics="true" pageId="1" pageNumber="18">Columnorbitolina</emphasis>
)
<emphasis id="F8EDEAB6FFD6FF97FDF2FE63F09EFDBA" box="[549,641,489,513]" italics="true" pageId="1" pageNumber="18">absidata</emphasis>
</taxonomicName>
by
<bibRefCitation id="AE084B55FFD6FF97FD68FE63F2C1FD99" author="Zhang, B. G." pageId="1" pageNumber="18" pagination="101 - 122" refId="ref5629" refString="Zhang, B. G., 1986. Early Cretaceous Orbitolinids from Xainza and Baingoin, Xizang. Bulletin of Nanjing Institute of Geology and Palaeontology, Academia Sinica, 10: 101 - 122 (in Chinese with English abstract)." type="journal article" year="1986">Zhang (1986)</bibRefCitation>
from the Langshan Formation of the Lhasa Block. Here we make reference to a tiny image of “
<taxonomicName id="0D994D27FFD6FF97FD5AFDA1F318FDDF" baseAuthorityName="Douglass" baseAuthorityYear="1960" class="Globothalamea" family="Orbitolinidae" genus="Mesorbitolina" kingdom="Chromista" order="Loftusiida" pageId="1" pageNumber="18" phylum="Foraminifera" rank="species" species="parva">
<emphasis id="F8EDEAB6FFD6FF97FD5AFDA1F318FDDF" italics="true" pageId="1" pageNumber="18">Mesorbitolina parva</emphasis>
</taxonomicName>
” included in Fig. 8 of
<bibRefCitation id="AE084B55FFD6FF97FDD1FDC6F2C0FD3E" author="BouDagher-Fadel, M. &amp; Hu, X. &amp; Price, G. D. &amp; Sun, G. &amp; Wang, J. - G. &amp; An, W." pageId="1" pageNumber="18" pagination="188 - 207" refId="ref3463" refString="BouDagher-Fadel, M., Hu, X., Price, G. D., Sun, G., Wang, J. - G. &amp; An, W., 2017. Foraminiferal biostratigraphy and palaeoenvironmental analysis of the mid-Cretaceous limestones in the southern Tibetian Plateau. Journal for Foraminiferal Research, 47 (2): 188 - 207." type="journal article" year="2017">BouDagher-Fadel et al. (2017)</bibRefCitation>
therein showing the stratigraphic ranges and assumed phylogenetic relationships (
<figureCitation id="52A22A21FFD6FF97FDCDFD04F06AFD1D" box="[538,629,654,678]" captionStart="Fig" captionStartId="2.[225,260,455,476]" captionTargetBox="[225,1363,155,419]" captionTargetId="figure-1358@2.[225,1363,155,419]" captionTargetPageId="2" captionText="Fig. 1. A, Mesorbitolina parva (Douglass) fide BouDagher-Fadel et al. (2017, excerpt of fig. 8), Lower Cretaceous of Tibet. B-E, Praeorbitolina cormyi Schroeder, axial sections perpendicular to the median plane (B-C: excerpt of Bosselini et al., 1999, fig. 5a and 5g, early Aptian of Ethiopia; D-E: early Aptian of Iran). Figures without scale." figureDoi="http://doi.org/10.5281/zenodo.10520847" httpUri="https://zenodo.org/record/10520847/files/figure.png" pageId="1" pageNumber="18">Fig. 1A</figureCitation>
). The specimen is here interpreted as an axial section of
<taxonomicName id="0D994D27FFD6FF97FD52FD25F30BFD52" authorityName="Schroeder" authorityYear="1964" class="Globothalamea" family="Orbitolinidae" genus="Praeorbitolina" kingdom="Chromista" order="Loftusiida" pageId="1" pageNumber="18" phylum="Foraminifera" rank="species" species="cormyi">
<emphasis id="F8EDEAB6FFD6FF97FD52FD25F30BFD52" italics="true" pageId="1" pageNumber="18">Praeorbitolina cormyi</emphasis>
</taxonomicName>
perpendicular to the median plane comparable to those illustrated by
<bibRefCitation id="AE084B55FFD6FF97FE6AFD78F0B2FCB1" author="Bosselini, A. &amp; Russo, A. &amp; Schroeder, R." box="[445,685,754,778]" pageId="1" pageNumber="18" pagination="783 - 791" refId="ref3529" refString="Bosselini, A., Russo, A. &amp; Schroeder, R., 1999. Stratigraphic evidence for an Early Aptian sea-level fluctuation: the Graua Limestone of south-eastern Ethiopia. Cretaceous Research, 20: 783 - 791." type="journal article" year="1999">Bosselini et al. (1999</bibRefCitation>
, fig. 5a and
<quantity id="0D619B41FFD6FF97FF12FC99F2FFFC90" box="[197,224,787,811]" metricMagnitude="-3" metricUnit="kg" metricValue="5.0" pageId="1" pageNumber="18" unit="g" value="5.0">5g</quantity>
) from the early Aptian of
<collectingCountry id="B28E7634FFD6FF97FE28FC99F046FC90" box="[511,601,787,811]" name="Ethiopia" pageId="1" pageNumber="18">Ethiopia</collectingCountry>
(
<figureCitation id="52A22A21FFD6FF97FDBEFC99F0BBFC90" box="[617,676,787,811]" captionStart="Fig" captionStartId="2.[225,260,455,476]" captionTargetBox="[225,1363,155,419]" captionTargetId="figure-1358@2.[225,1363,155,419]" captionTargetPageId="2" captionText="Fig. 1. A, Mesorbitolina parva (Douglass) fide BouDagher-Fadel et al. (2017, excerpt of fig. 8), Lower Cretaceous of Tibet. B-E, Praeorbitolina cormyi Schroeder, axial sections perpendicular to the median plane (B-C: excerpt of Bosselini et al., 1999, fig. 5a and 5g, early Aptian of Ethiopia; D-E: early Aptian of Iran). Figures without scale." figureDoi="http://doi.org/10.5281/zenodo.10520847" httpUri="https://zenodo.org/record/10520847/files/figure.png" pageId="1" pageNumber="18">Fig. 1</figureCitation>
B-C), or own material from
<collectingCountry id="B28E7634FFD6FF97FEBFFCBFF38CFCF7" box="[360,403,821,844]" name="Iran" pageId="1" pageNumber="18">Iran</collectingCountry>
(
<figureCitation id="52A22A21FFD6FF97FE74FCBEF3C0FCF7" box="[419,479,820,844]" captionStart="Fig" captionStartId="2.[225,260,455,476]" captionTargetBox="[225,1363,155,419]" captionTargetId="figure-1358@2.[225,1363,155,419]" captionTargetPageId="2" captionText="Fig. 1. A, Mesorbitolina parva (Douglass) fide BouDagher-Fadel et al. (2017, excerpt of fig. 8), Lower Cretaceous of Tibet. B-E, Praeorbitolina cormyi Schroeder, axial sections perpendicular to the median plane (B-C: excerpt of Bosselini et al., 1999, fig. 5a and 5g, early Aptian of Ethiopia; D-E: early Aptian of Iran). Figures without scale." figureDoi="http://doi.org/10.5281/zenodo.10520847" httpUri="https://zenodo.org/record/10520847/files/figure.png" pageId="1" pageNumber="18">Fig. 1</figureCitation>
D-E). It shows a subdivided subembryonic zone overlain by protoconch and deuterconch; a supraembryonic zone is seemingly lacking. The regular presence of short partitions at the top of the deuteroconch (not well discernible) would indicate
<taxonomicName id="0D994D27FFD6FF97FD10FC33F02CFC4A" authority="Schlagintweit et al." authorityName="Schlagintweit" class="Globothalamea" family="Orbitolinidae" genus="Praeorbitolina" kingdom="Chromista" order="Loftusiida" pageId="1" pageNumber="18" phylum="Foraminifera" rank="species" species="claveli">
<emphasis id="F8EDEAB6FFD6FF97FD10FC33F34CFC4A" italics="true" pageId="1" pageNumber="18">Praeorbitolina claveli</emphasis>
Schlagintweit et al.
</taxonomicName>
This example and the following ones give evidence that the established ranges partly include incorrect determinations too.
</paragraph>
</subSubSection>
</treatment>
</document>