treatments-xml/data/03/C9/6F/03C96F50FFD7FFBC75DFE0C9FD73C56B.xml
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<mods:title id="8FF73A5FA884B788ED115FE21C815F2F">Late Neogene Lophophaenidae (Nassellaria, Radiolaria) from the eastern equatorial Pacific</mods:title>
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<taxonomicName id="4C60A5C5FFD7FFBC75DFE0C9FEB9C7A4" box="[151,382,1214,1240]" class="Polycystina" family="Plagiacanthidae" genus="Lophophaena" kingdom="Chromista" order="Nassellaria" pageId="68" pageNumber="69" phylum="Radiozoa" rank="species" species="undefined-b">
<emphasis id="B9140254FFD7FFBC75DFE0C9FEFFC7A4" box="[151,312,1214,1240]" italics="true" pageId="68" pageNumber="69">Lophophaena</emphasis>
<emphasis id="B9140254FFD7FFBC7408E0C9FEB9C7A4" bold="true" box="[320,382,1214,1240]" pageId="68" pageNumber="69">sp. B</emphasis>
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Plate 36,
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.
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unknown plagonid group C sp 21,
<bibRefCitation id="EFF1A3B7FFD7FFBC74BEE15BFD13C638" author="Trubovitz, S. &amp; Lazarus, D. &amp; Renaudie, J. &amp; Noble, P. J." box="[502,724,1324,1348]" pageId="68" pageNumber="69" pagination="1 - 10" refId="ref96304" refString="Trubovitz, S., Lazarus, D., Renaudie, J. &amp; Noble, P. J. (2020) Marine plankton show threshold extinction response to Neogene climate change. Nature Communications, 11 (5069), 1 - 10. https: // doi. org / 10.1038 / s 41467 - 020 - 18879 - 7" type="journal article" year="2020">
Trubovitz
<emphasis id="B9140254FFD7FFBC7717E15AFD5FC638" box="[607,664,1324,1348]" italics="true" pageId="68" pageNumber="69">et al.,</emphasis>
2020
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, supplementary data 7.
</paragraph>
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<emphasis id="B9140254FFD7FFBC75DFE11AFECCC6FB" bold="true" box="[151,267,1389,1415]" pageId="68" pageNumber="69">Remarks.</emphasis>
This species is distinct for its flat-topped cephalis, with irregular pore shapes and sizes. However, with only
<specimenCount id="9D6615CFFFD7FFBC7598E1E6FEB1C6D7" box="[208,374,1425,1451]" pageId="68" pageNumber="69" type="generic">two specimens</specimenCount>
observed, we cannot formally describe it here.
</paragraph>
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<emphasis id="B9140254FFD7FFBC758FE1C2FE68C6B3" bold="true" box="[199,431,1461,1487]" pageId="68" pageNumber="69">Material examined.</emphasis>
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from Late Miocene samples 321-1337D-23H-
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and 321-1337A-12H-5,
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.
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<emphasis id="B9140254FFD7FFBC758FE18AFEDDC56B" bold="true" box="[199,282,1533,1559]" pageId="68" pageNumber="69">Range.</emphasis>
Late Miocene, in the
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(
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).
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