The first 40 million years of planktonic foraminifera

We provide a biochronology of Jurassic planktonic foramininfera, using first order linkage to ammonite and nannofossil stratigraphy and geochronology. This enigmatic and understudied group of microfossils occurred from middle Toarcian through Tithonian time, from ~180 to ~143 Ma; its origin is unkno...

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Published in:Geosciences
Main Authors: Gradstein, Felix M, Waskowska, Anna, Glinskikh, Larisa
Format: Article in Journal/Newspaper
Language:English
Published: 2022
Subjects:
Online Access:http://hdl.handle.net/10852/93106
http://urn.nb.no/URN:NBN:no-95661
https://doi.org/10.3390/geosciences11020085
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spelling ftoslouniv:oai:www.duo.uio.no:10852/93106 2023-05-15T18:00:32+02:00 The first 40 million years of planktonic foraminifera Gradstein, Felix M Waskowska, Anna Glinskikh, Larisa 2022-02-17T19:25:33Z http://hdl.handle.net/10852/93106 http://urn.nb.no/URN:NBN:no-95661 https://doi.org/10.3390/geosciences11020085 EN eng http://urn.nb.no/URN:NBN:no-95661 Gradstein, Felix M Waskowska, Anna Glinskikh, Larisa . The first 40 million years of planktonic foraminifera. Geosciences. 2021, 11(2), 1-25 http://hdl.handle.net/10852/93106 2003075 info:ofi/fmt:kev:mtx:ctx&ctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Geosciences&rft.volume=11&rft.spage=1&rft.date=2021 Geosciences 11 2 https://doi.org/10.3390/geosciences11020085 URN:NBN:no-95661 Fulltext https://www.duo.uio.no/bitstream/handle/10852/93106/1/The%2BFirst%2B40%2BMillion.pdf Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/ CC-BY 2076-3263 Journal article Tidsskriftartikkel Peer reviewed PublishedVersion 2022 ftoslouniv https://doi.org/10.3390/geosciences11020085 2022-04-06T22:33:48Z We provide a biochronology of Jurassic planktonic foramininfera, using first order linkage to ammonite and nannofossil stratigraphy and geochronology. This enigmatic and understudied group of microfossils occurred from middle Toarcian through Tithonian time, from ~180 to ~143 Ma; its origin is unknown. There are three genera: Globuligerina, Conoglobigerina and Petaloglobigerina. The genus Globuligerina, with a smooth to pustulose test surface texture appeared in Toarcian (late Early Jurassic) and Conoglobigerina, with a rough reticulate test surface texture in Oxfordian (early Late Jurassic) time. The genus Petaloglobigerina, having a petaloid last whorl with one or more claviform and twisted chambers evolved in early Kimmeridgian time from Globuligerina balakhmatovae. Biochronologic events for Jurassic planktonic foraminifera are most like First Common Appearance or Last Common Appearance events. The very first or very last appearance levels of taxa are not easily sampled and detected. We recognize stratigraphic events from eleven species across four postulated evolutionary lineages, calibrated to Geologic Time Scale 2020. A faunal change, which is not well documented led to the survival of only one taxon, most likely Gobuligerina oxfordiana in the Tithonian. Article in Journal/Newspaper Planktonic foraminifera Universitet i Oslo: Digitale utgivelser ved UiO (DUO) Geosciences 11 2 85
institution Open Polar
collection Universitet i Oslo: Digitale utgivelser ved UiO (DUO)
op_collection_id ftoslouniv
language English
description We provide a biochronology of Jurassic planktonic foramininfera, using first order linkage to ammonite and nannofossil stratigraphy and geochronology. This enigmatic and understudied group of microfossils occurred from middle Toarcian through Tithonian time, from ~180 to ~143 Ma; its origin is unknown. There are three genera: Globuligerina, Conoglobigerina and Petaloglobigerina. The genus Globuligerina, with a smooth to pustulose test surface texture appeared in Toarcian (late Early Jurassic) and Conoglobigerina, with a rough reticulate test surface texture in Oxfordian (early Late Jurassic) time. The genus Petaloglobigerina, having a petaloid last whorl with one or more claviform and twisted chambers evolved in early Kimmeridgian time from Globuligerina balakhmatovae. Biochronologic events for Jurassic planktonic foraminifera are most like First Common Appearance or Last Common Appearance events. The very first or very last appearance levels of taxa are not easily sampled and detected. We recognize stratigraphic events from eleven species across four postulated evolutionary lineages, calibrated to Geologic Time Scale 2020. A faunal change, which is not well documented led to the survival of only one taxon, most likely Gobuligerina oxfordiana in the Tithonian.
format Article in Journal/Newspaper
author Gradstein, Felix M
Waskowska, Anna
Glinskikh, Larisa
spellingShingle Gradstein, Felix M
Waskowska, Anna
Glinskikh, Larisa
The first 40 million years of planktonic foraminifera
author_facet Gradstein, Felix M
Waskowska, Anna
Glinskikh, Larisa
author_sort Gradstein, Felix M
title The first 40 million years of planktonic foraminifera
title_short The first 40 million years of planktonic foraminifera
title_full The first 40 million years of planktonic foraminifera
title_fullStr The first 40 million years of planktonic foraminifera
title_full_unstemmed The first 40 million years of planktonic foraminifera
title_sort first 40 million years of planktonic foraminifera
publishDate 2022
url http://hdl.handle.net/10852/93106
http://urn.nb.no/URN:NBN:no-95661
https://doi.org/10.3390/geosciences11020085
genre Planktonic foraminifera
genre_facet Planktonic foraminifera
op_source 2076-3263
op_relation http://urn.nb.no/URN:NBN:no-95661
Gradstein, Felix M Waskowska, Anna Glinskikh, Larisa . The first 40 million years of planktonic foraminifera. Geosciences. 2021, 11(2), 1-25
http://hdl.handle.net/10852/93106
2003075
info:ofi/fmt:kev:mtx:ctx&ctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Geosciences&rft.volume=11&rft.spage=1&rft.date=2021
Geosciences
11
2
https://doi.org/10.3390/geosciences11020085
URN:NBN:no-95661
Fulltext https://www.duo.uio.no/bitstream/handle/10852/93106/1/The%2BFirst%2B40%2BMillion.pdf
op_rights Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/
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op_doi https://doi.org/10.3390/geosciences11020085
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