Add updates up until 2024-12-01 08:10:43

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<taxonomicName id="4C724D4DFFECFF92AF98FBD80312C373" authority="Thalassinoides Ehrenberg, 1944" authorityName="Thalassinoides Ehrenberg" authorityYear="1944" box="[900,1368,1109,1135]" genus="Ichnogenus" pageId="7" pageNumber="330" rank="genus">
Ichnogenus
<emphasis id="B906EADCFFECFF92A814FBD802D0C373" box="[1032,1178,1109,1135]" italics="true" pageId="7" pageNumber="330">Thalassinoides</emphasis>
<bibRefCitation id="EFE34B3FFFECFF92A8BDFBD80312C373" author="EHRENBERG K." box="[1185,1368,1109,1135]" pageId="7" pageNumber="330" pagination="345 - 359" refId="ref8926" refString="EHRENBERG K. 1944. - Erganzende Bemerkungen zu den seinerzeit aus dem Miozan von Burgschleinitz beschriebenen Gangkernen und Bauten dekapoder Krebse. Palaontologische Zeitschrift 23: 345 - 359. https: // doi. org / 10.1007 / BF 03160443" type="journal article" year="1944">Ehrenberg, 1944</bibRefCitation>
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(
<figureCitation id="13492A4BFFECFF92A852FBF902C7C393" box="[1102,1165,1140,1167]" captionStart="FIG" captionStartId="8.[813,824,1505,1522]" captionTargetBox="[813,1455,215,1457]" captionTargetId="figure-695@8.[811,1364,787,1362]" captionTargetPageId="8" captionText="FIG. 3. — Thalassinoides Ehrenberg, 1944 filled with planktonic foraminifera tests (downward displacement marked by a yellow arrow) in a sub-CCD setting indicating rapid sequestration after deposition on the sea floor; inset showing local truncation (red lines) of laminae (yellow lines), indicating subsequent,probably multiple reworking by the producer.(RV Sonne cruise 114, core 27-1, 0-21 cm sediment depth;15°45.00N,115°45.00E, central South China Sea, 4220 m water depth; for details see Wetzel &amp; Unverricht 2013). Scale bar: 1 cm." pageId="7" pageNumber="330">Fig. 3</figureCitation>
)
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<paragraph id="8BCD36CEFFECFF92AF31FB39027CC1D1" blockId="7.[810,1458,1204,1741]" pageId="7" pageNumber="330">
Crustaceans living in the modern deep South
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Sea produce
<emphasis id="B906EADCFFECFF92AF36FB59058FC3F2" box="[810,965,1236,1262]" italics="true" pageId="7" pageNumber="330">Thalassinoides-</emphasis>
like burrows that document a sequestrichnial behaviour. Two kinds of burrows were encountered, which contained abundant foraminiferal tests stowed in greenish anoxic sediment. One burrow
<typeStatus id="54C9886CFFECFF92A833FAB90214C252" box="[1071,1118,1332,1358]" pageId="7" pageNumber="330">type</typeStatus>
contains benthic agglutinated foraminifera tests, which consist mainly of Pinatubo-1991 ash but were stowed below the ash in anoxic sediment (
<bibRefCitation id="EFE34B3FFFECFF92A940FAF905BDC2B2" author="KAMINSKI M. A. &amp; WETZEL A." pageId="7" pageNumber="330" pagination="277 - 283" refId="ref10153" refString="KAMINSKI M. A. &amp; WETZEL A. 2004. - A tubular protozoan predator: A burrow selectively filled with tubular agglutinated protozoans (Xenophyophorea, Foraminifera) in the abyssal South China Sea, in BUBIK M. &amp; KAMINSKI M. A. (eds), Proceedings of the Sixth International Workshop on Agglutinated Foraminifera. Grzybowski Foundation Special Publication, London: 277 - 283." type="proceedings paper" year="2004">Kaminski &amp; Wetzel 2004</bibRefCitation>
). The other kind of
<emphasis id="B906EADCFFECFF92A8CEFA1E032EC2B1" box="[1234,1380,1427,1453]" italics="true" pageId="7" pageNumber="330">Thalassinoides</emphasis>
occurs in water depths below the CCD; it exhibits a laminated fill consisting of calcareous planktonic foraminiferal tests that are stowed and preserved in the burrow, whereas they are already dissolved in the overlying hemipelagic sediment from which they originate (
<bibRefCitation id="EFE34B3FFFECFF92AFC8F9BE02B0C151" author="WETZEL A. &amp; UNVERRICHT D." box="[980,1274,1587,1613]" pageId="7" pageNumber="330" pagination="91 - 100" refId="ref14686" refString="WETZEL A. &amp; UNVERRICHT D. 2013. - A muddy megaturbidite in the deep central South China Sea deposited ~ 350 yrs BP. Marine Geology 346: 91 - 100. https: // doi. org / 10.1016 / j. margeo. 2013.08.010" type="journal article" year="2013">Wetzel &amp; Unverricht 2013</bibRefCitation>
). The calcareous foraminiferal tests must have been stowed shortly after their deposition; otherwise they would show dissolution features. Partly truncated laminae in the burrow imply later reworking by the producer (
<figureCitation id="13492A4BFFECFF92AFF4F93F026CC1D1" box="[1000,1062,1714,1741]" captionStart="FIG" captionStartId="8.[813,824,1505,1522]" captionTargetBox="[813,1455,215,1457]" captionTargetId="figure-695@8.[811,1364,787,1362]" captionTargetPageId="8" captionText="FIG. 3. — Thalassinoides Ehrenberg, 1944 filled with planktonic foraminifera tests (downward displacement marked by a yellow arrow) in a sub-CCD setting indicating rapid sequestration after deposition on the sea floor; inset showing local truncation (red lines) of laminae (yellow lines), indicating subsequent,probably multiple reworking by the producer.(RV Sonne cruise 114, core 27-1, 0-21 cm sediment depth;15°45.00N,115°45.00E, central South China Sea, 4220 m water depth; for details see Wetzel &amp; Unverricht 2013). Scale bar: 1 cm." pageId="7" pageNumber="330">Fig. 3</figureCitation>
).
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