No state change in pelagic fish production and biodiversity during the Eocene-Oligocene Transition
The Eocene-Oligocene (E/O) boundary ~33.9 million years ago, has been described as a state change in the Earth system marked by the permanent glaciation of Antarctica and a proposed increase in oceanic productivity. Here we quantified the response of fish production and biodiversity to this event us...
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ftzenodo:oai:zenodo.org:4992386 2024-09-15T17:45:25+00:00 No state change in pelagic fish production and biodiversity during the Eocene-Oligocene Transition Sibert, Elizabeth Zill, Michelle Frigyik, Ella Norris, Richard 2020-03-02 https://doi.org/10.5061/dryad.nk98sf7q5 unknown Zenodo https://doi.org/10.1038/s41561-020-0540-2 https://zenodo.org/communities/dryad https://doi.org/10.5061/dryad.nk98sf7q5 oai:zenodo.org:4992386 info:eu-repo/semantics/openAccess Creative Commons Zero v1.0 Universal https://creativecommons.org/publicdomain/zero/1.0/legalcode Eocene-Oligocene fossils microfossils Ichthyoliths pelagic fish info:eu-repo/semantics/other 2020 ftzenodo https://doi.org/10.5061/dryad.nk98sf7q510.1038/s41561-020-0540-2 2024-07-26T03:19:14Z The Eocene-Oligocene (E/O) boundary ~33.9 million years ago, has been described as a state change in the Earth system marked by the permanent glaciation of Antarctica and a proposed increase in oceanic productivity. Here we quantified the response of fish production and biodiversity to this event using microfossil fish teeth (ichthyoliths) in seven deep-sea sediment cores from around the world. Ichthyolith accumulation rate (a proxy for fish biomass production) shows no synchronous trends across the E/O. Ichthyolith accumulation in the Southern Ocean and Pacific Gyre sites is an order of magnitude lower than the equatorial and Atlantic sites, demonstrating that the Southern Ocean was not a highly productive ecosystem for fish before or after the E/O. Further, tooth morphotype diversity and assemblage composition remained stable across the interval, indicating little change in the biodiversity or ecological role of open ocean fish. While the E/O boundary was a major global climate change event, its impact on pelagic fish was relatively muted. Our results support recent findings of whale and krill diversification which suggest that the pelagic ecosystem restructuring commonly attributed to the E/O transition likely occurred much later, in the late Oligocene or Miocene. README for Data Archive for: Pelagic fish production and diversity unchanging across the Eocene-Oligocene Glaciation Elizabeth C Sibert, Michelle E Zill, Ella T. Frigyik, and Richard D Norris Contact: Elizabeth Sibert (esibert@fas.harvard.edu) *Email address will be updated at a future time This dataset consists of images of each unique ocean drilling sample considered in this study. There are two sites included in this study: DSDP Site 596 and ODP Site 689. They were imaged at different times and on different instruments, however the data are functionally equivilant. File Name information: ODP Site 689: Filenames take the form: SiteNumber_SlideNumber_SampleNumber_IODP-Core_IODP-Section_IODP-SampleDepthInterval_HoleNumber_ZoomLevel ODP-689B ANT01 ... Other/Unknown Material Antarc* Antarctica Southern Ocean Zenodo |
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Open Polar |
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topic |
Eocene-Oligocene fossils microfossils Ichthyoliths pelagic fish |
spellingShingle |
Eocene-Oligocene fossils microfossils Ichthyoliths pelagic fish Sibert, Elizabeth Zill, Michelle Frigyik, Ella Norris, Richard No state change in pelagic fish production and biodiversity during the Eocene-Oligocene Transition |
topic_facet |
Eocene-Oligocene fossils microfossils Ichthyoliths pelagic fish |
description |
The Eocene-Oligocene (E/O) boundary ~33.9 million years ago, has been described as a state change in the Earth system marked by the permanent glaciation of Antarctica and a proposed increase in oceanic productivity. Here we quantified the response of fish production and biodiversity to this event using microfossil fish teeth (ichthyoliths) in seven deep-sea sediment cores from around the world. Ichthyolith accumulation rate (a proxy for fish biomass production) shows no synchronous trends across the E/O. Ichthyolith accumulation in the Southern Ocean and Pacific Gyre sites is an order of magnitude lower than the equatorial and Atlantic sites, demonstrating that the Southern Ocean was not a highly productive ecosystem for fish before or after the E/O. Further, tooth morphotype diversity and assemblage composition remained stable across the interval, indicating little change in the biodiversity or ecological role of open ocean fish. While the E/O boundary was a major global climate change event, its impact on pelagic fish was relatively muted. Our results support recent findings of whale and krill diversification which suggest that the pelagic ecosystem restructuring commonly attributed to the E/O transition likely occurred much later, in the late Oligocene or Miocene. README for Data Archive for: Pelagic fish production and diversity unchanging across the Eocene-Oligocene Glaciation Elizabeth C Sibert, Michelle E Zill, Ella T. Frigyik, and Richard D Norris Contact: Elizabeth Sibert (esibert@fas.harvard.edu) *Email address will be updated at a future time This dataset consists of images of each unique ocean drilling sample considered in this study. There are two sites included in this study: DSDP Site 596 and ODP Site 689. They were imaged at different times and on different instruments, however the data are functionally equivilant. File Name information: ODP Site 689: Filenames take the form: SiteNumber_SlideNumber_SampleNumber_IODP-Core_IODP-Section_IODP-SampleDepthInterval_HoleNumber_ZoomLevel ODP-689B ANT01 ... |
format |
Other/Unknown Material |
author |
Sibert, Elizabeth Zill, Michelle Frigyik, Ella Norris, Richard |
author_facet |
Sibert, Elizabeth Zill, Michelle Frigyik, Ella Norris, Richard |
author_sort |
Sibert, Elizabeth |
title |
No state change in pelagic fish production and biodiversity during the Eocene-Oligocene Transition |
title_short |
No state change in pelagic fish production and biodiversity during the Eocene-Oligocene Transition |
title_full |
No state change in pelagic fish production and biodiversity during the Eocene-Oligocene Transition |
title_fullStr |
No state change in pelagic fish production and biodiversity during the Eocene-Oligocene Transition |
title_full_unstemmed |
No state change in pelagic fish production and biodiversity during the Eocene-Oligocene Transition |
title_sort |
no state change in pelagic fish production and biodiversity during the eocene-oligocene transition |
publisher |
Zenodo |
publishDate |
2020 |
url |
https://doi.org/10.5061/dryad.nk98sf7q5 |
genre |
Antarc* Antarctica Southern Ocean |
genre_facet |
Antarc* Antarctica Southern Ocean |
op_relation |
https://doi.org/10.1038/s41561-020-0540-2 https://zenodo.org/communities/dryad https://doi.org/10.5061/dryad.nk98sf7q5 oai:zenodo.org:4992386 |
op_rights |
info:eu-repo/semantics/openAccess Creative Commons Zero v1.0 Universal https://creativecommons.org/publicdomain/zero/1.0/legalcode |
op_doi |
https://doi.org/10.5061/dryad.nk98sf7q510.1038/s41561-020-0540-2 |
_version_ |
1810493233126440960 |