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111 lines
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<document id="1A069ADA08A37A7C08CC9B97D0EE0024" ID-CLB-Dataset="305524" ID-DOI="10.5852/cr-palevol2024v23a22" ID-GBIF-Dataset="fefdf6a6-89e6-4b61-8d87-ff08580d85f9" ID-ISSN="1777-571X" ID-Zenodo-Dep="14224959" ID-ZooBank="urn:lsid:zoobank.org:pub:FAE07554-6F51-46B5-A81D-EA7D9091E776" IM.bibliography_approvedBy="valdenar" IM.illustrations_approvedBy="felipe" IM.materialsCitations_approvedBy="felipe" IM.metadata_approvedBy="felipe" IM.taxonomicNames_approvedBy="valdenar" IM.treatments_approvedBy="valdenar" checkinTime="1732638299342" checkinUser="felipe" docAuthor="Uchman, Alfred & Wetzel, Andreas" docDate="2024" docId="03DB87D8FFECFF92AC86FC380735C030" docLanguage="en" docName="CRPalevol.23.22.325-338.pdf" docOrigin="Comptes Rendus Palevol 23 (22)" docSource="http://dx.doi.org/10.5852/cr-palevol2024v23a22" docStyle="DocumentStyle:DACF86F01658A8850E13A63D98C287FD.1:CRPalevol.2020-.journal_article" docStyleId="DACF86F01658A8850E13A63D98C287FD" docStyleName="CRPalevol.2020-.journal_article" docStyleVersion="1" docTitle="Cladichnus D'Alessandro & Bromley 1987" docType="treatment" docVersion="3" lastPageNumber="330" masterDocId="FFE2FFA0FFEBFF95AC1CFF8D064AC71C" masterDocTitle="Sequestrichnia - an ethological category of marine trace fossils recording the collection and stowage of nutritional material within burrows" masterLastPageNumber="338" masterPageNumber="325" pageNumber="330" updateTime="1732743699526" updateUser="ExternalLinkService" zenodo-license-document="CC-BY-4.0">
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<mods:title id="46E79538A0DA8F5FD61922D8821EFA1E">Sequestrichnia - an ethological category of marine trace fossils recording the collection and stowage of nutritional material within burrows</mods:title>
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<mods:name id="9A8D0C559F3DDDB83FD6EC355CC4655B" type="personal">
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<mods:namePart id="CD3A7ED3D5F9E44ACFD874A62F1FC083">Uchman, Alfred</mods:namePart>
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<mods:affiliation id="5C28205F97B785386BAAAC52782883D1">Jagiellonian University, Faculty of Geography and Geology, Institute of Geological Sciences, Gronostajowa 3 a, PL- 30 - 387 Kraków (Poland) alfred. uchman @ uj. edu. pl (corresponding author)</mods:affiliation>
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<mods:nameIdentifier id="71232684E4146967B0002E782CCD76F6" type="email">alfred.uchman@uj.edu.pl</mods:nameIdentifier>
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<mods:namePart id="B66DD388922FAF1E29545DA6DCDD46AF">Wetzel, Andreas</mods:namePart>
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<mods:affiliation id="5FA738F19AAF0B939B0394A06AA43E37">Department of Environmental Sciences - Geology, Universität Basel, Bernoullistrasse 32, CH- 4056 Basel (Switzerland) andreas. wetzel @ unibas. ch</mods:affiliation>
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<mods:nameIdentifier id="BB0306BBC7B829167E2704E9809C3A92" type="email">andreas.wetzel@unibas.ch</mods:nameIdentifier>
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<mods:title id="D6B789A2FF0FE2FAD06675A744324220">Comptes Rendus Palevol</mods:title>
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<mods:date id="F477C86475B324FD2BC646C375236B3C">2024</mods:date>
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<mods:number id="9C085C98A3C904ECF3E70EEBC3AA3D04">2024-08-30</mods:number>
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<mods:number id="2970978B474666BB0A89BF19026D3965">23</mods:number>
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<mods:url id="3A716B1CA8DA0C749A4C2C7642031DAB">http://dx.doi.org/10.5852/cr-palevol2024v23a22</mods:url>
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<mods:identifier id="BDEA504A4DEFFAB42999468D8223B8AB" type="DOI">10.5852/cr-palevol2024v23a22</mods:identifier>
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<treatment id="03DB87D8FFECFF92AC86FC380735C030" ID-DOI="http://doi.org/10.5281/zenodo.14232263" ID-GBIF-Taxon="247601435" ID-Zenodo-Dep="14232263" LSID="urn:lsid:plazi:treatment:03DB87D8FFECFF92AC86FC380735C030" httpUri="http://treatment.plazi.org/id/03DB87D8FFECFF92AC86FC380735C030" lastPageNumber="330" pageId="7" pageNumber="330">
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<subSubSection id="C3686545FFECFF92AC86FC3804BBC4D3" box="[154,753,949,975]" pageId="7" pageNumber="330" type="nomenclature">
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<paragraph id="8BCD36CEFFECFF92AC86FC3804BBC4D3" blockId="7.[154,753,949,975]" box="[154,753,949,975]" pageId="7" pageNumber="330">
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<heading id="D08581A2FFECFF92AC86FC3804BBC4D3" box="[154,753,949,975]" centered="true" fontSize="10" level="2" pageId="7" pageNumber="330" reason="2">
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Ichnogenus
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<taxonomicName id="4C724D4DFFECFF92AD02FC3804BBC4D3" authority="D'Alessandro & Bromley, 1987" authorityName="D'Alessandro & Bromley" authorityYear="1987" box="[286,753,949,975]" genus="Cladichnus" higherTaxonomySource="GBIF" kingdom="Animalia" pageId="7" pageNumber="330" rank="genus">
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<emphasis id="B906EADCFFECFF92AD02FC3807D8C4D3" box="[286,402,949,975]" italics="true" pageId="7" pageNumber="330">Cladichnus</emphasis>
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<bibRefCitation id="EFE34B3FFFECFF92AD85FC3804BBC4D3" author="D'ALESSANDRO A. & BROMLEY R. G." box="[409,753,949,975]" pageId="7" pageNumber="330" pagination="743 - 763" refId="ref8827" refString="D'ALESSANDRO A. & BROMLEY R. G. 1987. - Meniscate trace fossils and the Muensteria-Taenidium problem. Palaeontology 30: 743 - 763. https: // www. biodiversitylibrary. org / page / 49682493" type="journal article" year="1987">D’Alessandro & Bromley, 1987</bibRefCitation>
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</taxonomicName>
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</heading>
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</paragraph>
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</subSubSection>
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<subSubSection id="C3686545FFECFF92AC98FC780735C030" pageId="7" pageNumber="330" type="description">
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<paragraph id="8BCD36CEFFECFF92AC98FC78054FC212" blockId="7.[130,777,1013,1837]" pageId="7" pageNumber="330">
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The
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<taxonomicName id="4C724D4DFFECFF92ACA8FC780762C313" authorityName="D'Alessandro & Bromley" authorityYear="1987" box="[180,296,1013,1039]" genus="Cladichnus" higherTaxonomySource="GBIF" kingdom="Animalia" pageId="7" pageNumber="330" rank="genus">
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<emphasis id="B906EADCFFECFF92ACA8FC780762C313" box="[180,296,1013,1039]" italics="true" pageId="7" pageNumber="330">Cladichnus</emphasis>
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</taxonomicName>
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burrow (Cretaceous-Eocene) consists of primary successively branched and radiating tubes, which contain a meniscate fill. These traces are preferentially constructed in anoxic sediments. New branches are produced roughly at the same level as previous ones, implying that appropriate conditions for stowing were encountered by the producer. In contrast, new branches constructed below or above may target stronger or weaker reducing conditions or represent a response to the downward or upward migration of the redox boundary.
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</paragraph>
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<paragraph id="8BCD36CEFFECFF92AC87FA9904DCC132" blockId="7.[130,777,1013,1837]" pageId="7" pageNumber="330">
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Collection and transfer of surface material is recorded by the tubes’ fill that was analyzed in detail for the ichnospecies
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<taxonomicName id="4C724D4DFFECFF92AC98FAD904C8C272" authority="Wetzel & Uchman, 2013" authorityName="Wetzel & Uchman" authorityYear="2013" box="[132,642,1364,1390]" genus="Cladichnus" higherTaxonomySource="GBIF" kingdom="Animalia" pageId="7" pageNumber="330" rank="species" species="parallelum">
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<emphasis id="B906EADCFFECFF92AC98FAD90727C272" box="[132,365,1364,1390]" italics="true" pageId="7" pageNumber="330">Cladichnus parallelum</emphasis>
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<bibRefCitation id="EFE34B3FFFECFF92AD6FFAD904C8C272" author="WETZEL A. & UCHMAN A." box="[371,642,1364,1390]" pageId="7" pageNumber="330" pagination="120 - 128" refId="ref14579" refString="WETZEL A. & UCHMAN A. 2013. - Cladichnus parallelum isp. nov. - a mid- to deep-tier feeding burrow system. Ichnos 20 (3): 120 - 128. https: // doi. org / 10.1080 / 10420940.2013.816301" type="journal article" year="2013">Wetzel & Uchman, 2013</bibRefCitation>
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</taxonomicName>
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, which contains 0.8%
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<subScript id="17F6348BFFECFF92AD1FFAF90765C28D" attach="left" box="[259,303,1396,1425]" fontSize="7" pageId="7" pageNumber="330">Corg</subScript>
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and 0.3% CaCO
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compared to 0.3%
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<subScript id="17F6348BFFECFF92AEC7FAF9054DC28D" attach="left" box="[731,775,1396,1425]" fontSize="7" pageId="7" pageNumber="330">Corg</subScript>
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and 64% CaCO
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<subScript id="17F6348BFFECFF92AD22FA2D0702C2AD" attach="left" box="[318,328,1440,1457]" fontSize="7" pageId="7" pageNumber="330">3</subScript>
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in
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</quantity>
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the host sediment Cretaceous in age (
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<bibRefCitation id="EFE34B3FFFECFF92AC92FA3E07D1C2D2" author="WETZEL A. & UCHMAN A." box="[142,411,1459,1486]" pageId="7" pageNumber="330" pagination="120 - 128" refId="ref14579" refString="WETZEL A. & UCHMAN A. 2013. - Cladichnus parallelum isp. nov. - a mid- to deep-tier feeding burrow system. Ichnos 20 (3): 120 - 128. https: // doi. org / 10.1080 / 10420940.2013.816301" type="journal article" year="2013">Wetzel & Uchman 2013</bibRefCitation>
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). The fill of the branches is interpreted to indicate priming that provided microbes (or their metabolic products) as an additional subsurface food source (cf.
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<bibRefCitation id="EFE34B3FFFECFF92ACB2F9990726C131" author="MAYER L. M. & JUMARS P. A. & BOCK M. J. & VETTER Y. A. & SCHMIDT J. L." box="[174,364,1555,1582]" pageId="7" pageNumber="330" pagination="335 - 347" refId="ref11333" refString="MAYER L. M., JUMARS P. A., BOCK M. J., VETTER Y. A. & SCHMIDT J. L. 2001. - Two roads to sparagmos: extracellular digestion of sedimentary food by bacterial inoculation versus deposit-feeding, in ALLER J. Y., WOODIN S. A. & ALLER R. C. (eds), Organism - Sediment Interactions. University of South Carolina Press, Columbia (S. C.): 335 - 347." type="book chapter" year="2001">
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Mayer
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<emphasis id="B906EADCFFECFF92ACE6F9990764C131" box="[250,302,1555,1581]" italics="true" pageId="7" pageNumber="330">et al.</emphasis>
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2001
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</bibRefCitation>
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;
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<bibRefCitation id="EFE34B3FFFECFF92AD66F99904CDC131" author="VAN NUGTEREN P. & MOODLEY L. & BRUMMER G. - J. & HEIP C. H. R. & HERMAN P. M. J. & MIDDELBURG J. J." box="[378,647,1555,1582]" pageId="7" pageNumber="330" pagination="2277 - 2287" refId="ref13968" refString="VAN NUGTEREN P., MOODLEY L., BRUMMER G. - J., HEIP C. H. R., HERMAN P. M. J. & MIDDELBURG J. J. 2009. - Seafloor ecosystem functioning: the importance of organic matter priming. Marine Biology 156: 2277 - 2287. https: // doi. org / 10.1007 / s 00227 - 009 - 1255 - 5" type="journal article" year="2009">
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van Nugteren
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<emphasis id="B906EADCFFECFF92AE08F9990402C131" box="[532,584,1555,1581]" italics="true" pageId="7" pageNumber="330">et al.</emphasis>
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2009
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</bibRefCitation>
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).
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</paragraph>
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<paragraph id="8BCD36CEFFECFF92AC87F9B90735C030" blockId="7.[130,777,1013,1837]" pageId="7" pageNumber="330">Most likely, the trace producer ingested a considerable proportion of the filling material before emplacing the final, now meniscate fill. The arrangement of the branches has further implications. Branches at a level above the previous ones could allow utilization of upstreaming pore water, probably carrying nutritious compounds. Alternatively, a shift of the redox boundary may have caused the construction of new levels of open burrows.</paragraph>
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</subSubSection>
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</treatment>
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</document> |