Exceptionally preserved lacustrine ostracods from the Middle Miocene of Antarctica: implications for high latitude palaeoenvironment at 77° south
A newly discovered Konservat-Lagerstätte from the Middle Miocene of the western Olympus Range, Dry Valleys, Antarctica, yields cypridoidean ostracods complete with preserved body and appendages. This is the first record of 3-dimensionally fossilized animal soft tissues from the continent. The ostrac...
Published in: | Proceedings of the Royal Society B: Biological Sciences |
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Online Access: | http://rspb.royalsocietypublishing.org/content/275/1650/2449 http://hdl.handle.net/2381/8081 https://doi.org/10.1098/rspb.2008.0396 |
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ftleicester:oai:lra.le.ac.uk:2381/8081 2023-05-15T13:50:23+02:00 Exceptionally preserved lacustrine ostracods from the Middle Miocene of Antarctica: implications for high latitude palaeoenvironment at 77° south Williams, Mark Siveter, David J. Ashworth, Allan C. Wilby, Philip R. Horne, David J. Lewis, Adam R. Marchant, David R. 2010-06-21T13:48:37Z http://rspb.royalsocietypublishing.org/content/275/1650/2449 http://hdl.handle.net/2381/8081 https://doi.org/10.1098/rspb.2008.0396 en eng The Royal Society Proceedings of the Royal Society B: Biological Sciences, 2008, 275 (1650), pp. 2449–2454 0962-8452 1471-2954 http://rspb.royalsocietypublishing.org/content/275/1650/2449 http://hdl.handle.net/2381/8081 doi:10.1098/rspb.2008.0396 This is the author’s final draft of the paper published as Proceedings of the Royal Society B: Biological Sciences, 2008, 275 (1650), pp. 2449–2454. The final published version is available at http://rspb.royalsocietypublishing.org/content/275/1650/2449, Doi:10.1098/rspb.2008.0396. ostracods Konservat Lagerstätte Dry Valleys Miocene palaeoclimate palaeolake pyritization soft-tissues Article 2010 ftleicester https://doi.org/10.1098/rspb.2008.0396 2019-03-22T20:13:16Z A newly discovered Konservat-Lagerstätte from the Middle Miocene of the western Olympus Range, Dry Valleys, Antarctica, yields cypridoidean ostracods complete with preserved body and appendages. This is the first record of 3-dimensionally fossilized animal soft tissues from the continent. The ostracods are preserved in goethite, secondary after pyrite, representing a novel mode of exceptional preservation. They signal a high latitude (>77°S) lake setting (Palaeolake Boreas) viable for benthic animal colonisation prior to 14 Ma. Their presence supports the notion of warmer, tundra-like environmental conditions persisting in the Dry Valleys until the Middle Miocene. Article in Journal/Newspaper Antarc* Antarctica Tundra University of Leicester: Leicester Research Archive (LRA) Boreas ENVELOPE(-3.933,-3.933,-71.300,-71.300) Olympus ENVELOPE(156.767,156.767,-80.217,-80.217) Olympus Range ENVELOPE(162.000,162.000,-77.467,-77.467) Proceedings of the Royal Society B: Biological Sciences 275 1650 2449 2454 |
institution |
Open Polar |
collection |
University of Leicester: Leicester Research Archive (LRA) |
op_collection_id |
ftleicester |
language |
English |
topic |
ostracods Konservat Lagerstätte Dry Valleys Miocene palaeoclimate palaeolake pyritization soft-tissues |
spellingShingle |
ostracods Konservat Lagerstätte Dry Valleys Miocene palaeoclimate palaeolake pyritization soft-tissues Williams, Mark Siveter, David J. Ashworth, Allan C. Wilby, Philip R. Horne, David J. Lewis, Adam R. Marchant, David R. Exceptionally preserved lacustrine ostracods from the Middle Miocene of Antarctica: implications for high latitude palaeoenvironment at 77° south |
topic_facet |
ostracods Konservat Lagerstätte Dry Valleys Miocene palaeoclimate palaeolake pyritization soft-tissues |
description |
A newly discovered Konservat-Lagerstätte from the Middle Miocene of the western Olympus Range, Dry Valleys, Antarctica, yields cypridoidean ostracods complete with preserved body and appendages. This is the first record of 3-dimensionally fossilized animal soft tissues from the continent. The ostracods are preserved in goethite, secondary after pyrite, representing a novel mode of exceptional preservation. They signal a high latitude (>77°S) lake setting (Palaeolake Boreas) viable for benthic animal colonisation prior to 14 Ma. Their presence supports the notion of warmer, tundra-like environmental conditions persisting in the Dry Valleys until the Middle Miocene. |
format |
Article in Journal/Newspaper |
author |
Williams, Mark Siveter, David J. Ashworth, Allan C. Wilby, Philip R. Horne, David J. Lewis, Adam R. Marchant, David R. |
author_facet |
Williams, Mark Siveter, David J. Ashworth, Allan C. Wilby, Philip R. Horne, David J. Lewis, Adam R. Marchant, David R. |
author_sort |
Williams, Mark |
title |
Exceptionally preserved lacustrine ostracods from the Middle Miocene of Antarctica: implications for high latitude palaeoenvironment at 77° south |
title_short |
Exceptionally preserved lacustrine ostracods from the Middle Miocene of Antarctica: implications for high latitude palaeoenvironment at 77° south |
title_full |
Exceptionally preserved lacustrine ostracods from the Middle Miocene of Antarctica: implications for high latitude palaeoenvironment at 77° south |
title_fullStr |
Exceptionally preserved lacustrine ostracods from the Middle Miocene of Antarctica: implications for high latitude palaeoenvironment at 77° south |
title_full_unstemmed |
Exceptionally preserved lacustrine ostracods from the Middle Miocene of Antarctica: implications for high latitude palaeoenvironment at 77° south |
title_sort |
exceptionally preserved lacustrine ostracods from the middle miocene of antarctica: implications for high latitude palaeoenvironment at 77° south |
publisher |
The Royal Society |
publishDate |
2010 |
url |
http://rspb.royalsocietypublishing.org/content/275/1650/2449 http://hdl.handle.net/2381/8081 https://doi.org/10.1098/rspb.2008.0396 |
long_lat |
ENVELOPE(-3.933,-3.933,-71.300,-71.300) ENVELOPE(156.767,156.767,-80.217,-80.217) ENVELOPE(162.000,162.000,-77.467,-77.467) |
geographic |
Boreas Olympus Olympus Range |
geographic_facet |
Boreas Olympus Olympus Range |
genre |
Antarc* Antarctica Tundra |
genre_facet |
Antarc* Antarctica Tundra |
op_relation |
Proceedings of the Royal Society B: Biological Sciences, 2008, 275 (1650), pp. 2449–2454 0962-8452 1471-2954 http://rspb.royalsocietypublishing.org/content/275/1650/2449 http://hdl.handle.net/2381/8081 doi:10.1098/rspb.2008.0396 |
op_rights |
This is the author’s final draft of the paper published as Proceedings of the Royal Society B: Biological Sciences, 2008, 275 (1650), pp. 2449–2454. The final published version is available at http://rspb.royalsocietypublishing.org/content/275/1650/2449, Doi:10.1098/rspb.2008.0396. |
op_doi |
https://doi.org/10.1098/rspb.2008.0396 |
container_title |
Proceedings of the Royal Society B: Biological Sciences |
container_volume |
275 |
container_issue |
1650 |
container_start_page |
2449 |
op_container_end_page |
2454 |
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1766253448924233728 |