Late Cretaceous palaeoenvironments and biotas: an Antarctic perspective
The Cretaceous period is often regarded as one of "greenhouse" warmth, with perhaps its acme occurring in the late Albian stage (100 Ma ago). However, it is now apparent that, even at this time, there were significant meridional temperature gradients and distinct temperate biotas in the hi...
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Cambridge University Press
1992
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ftnerc:oai:nora.nerc.ac.uk:518384 2023-05-15T13:49:34+02:00 Late Cretaceous palaeoenvironments and biotas: an Antarctic perspective Crame, J.A. 1992-12 http://nora.nerc.ac.uk/id/eprint/518384/ https://doi.org/10.1017/S0954102092000555 unknown Cambridge University Press Crame, J.A. orcid:0000-0002-5027-9965 . 1992 Late Cretaceous palaeoenvironments and biotas: an Antarctic perspective. Antarctic Science, 4 (04). 371-382. https://doi.org/10.1017/S0954102092000555 <https://doi.org/10.1017/S0954102092000555> Publication - Article PeerReviewed 1992 ftnerc https://doi.org/10.1017/S0954102092000555 2023-02-04T19:45:38Z The Cretaceous period is often regarded as one of "greenhouse" warmth, with perhaps its acme occurring in the late Albian stage (100 Ma ago). However, it is now apparent that, even at this time, there were significant meridional temperature gradients and distinct temperate biotas in the highest latitude regions. This is particularly so in the Southern Hemisphere, where an extensive Albian fossil record from Antarctica, Australia and New Zealand has revealed the presence of austral floras and faunas. With the recent improvements in stratigraphical correlations, it has become possible to trace the later Cretaceous palaeoenvironmental record in the Antarctic Peninsula region. Unfortunately, resolution of the early Late Cretaceous (Cenomanian–Coniacian stages) is still imprecise; there are some indications of strongly differentiated palynological assemblages, but studies of both macrofaunas and palaeotemperature estimates are incomplete. By the Santonian–Campanian, high-latitude biotas are well developed in the James Ross Island region and their enhancement through the final stages of the Cretaceous can be linked to a phase of global cooling. The persistence of low diversity temperate communities in high latitude regions may be of considerable ecological and evolutionary significance. For example, there is evidence to suggest that these communities may have been more resistant to mass extinction events; they may also have been important source regions for replacement taxa that arose after such events. Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Antarctic Science Antarctica James Ross Island Ross Island Natural Environment Research Council: NERC Open Research Archive Antarctic The Antarctic Antarctic Peninsula Austral Ross Island New Zealand Antarctic Science 4 4 371 382 |
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Natural Environment Research Council: NERC Open Research Archive |
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The Cretaceous period is often regarded as one of "greenhouse" warmth, with perhaps its acme occurring in the late Albian stage (100 Ma ago). However, it is now apparent that, even at this time, there were significant meridional temperature gradients and distinct temperate biotas in the highest latitude regions. This is particularly so in the Southern Hemisphere, where an extensive Albian fossil record from Antarctica, Australia and New Zealand has revealed the presence of austral floras and faunas. With the recent improvements in stratigraphical correlations, it has become possible to trace the later Cretaceous palaeoenvironmental record in the Antarctic Peninsula region. Unfortunately, resolution of the early Late Cretaceous (Cenomanian–Coniacian stages) is still imprecise; there are some indications of strongly differentiated palynological assemblages, but studies of both macrofaunas and palaeotemperature estimates are incomplete. By the Santonian–Campanian, high-latitude biotas are well developed in the James Ross Island region and their enhancement through the final stages of the Cretaceous can be linked to a phase of global cooling. The persistence of low diversity temperate communities in high latitude regions may be of considerable ecological and evolutionary significance. For example, there is evidence to suggest that these communities may have been more resistant to mass extinction events; they may also have been important source regions for replacement taxa that arose after such events. |
format |
Article in Journal/Newspaper |
author |
Crame, J.A. |
spellingShingle |
Crame, J.A. Late Cretaceous palaeoenvironments and biotas: an Antarctic perspective |
author_facet |
Crame, J.A. |
author_sort |
Crame, J.A. |
title |
Late Cretaceous palaeoenvironments and biotas: an Antarctic perspective |
title_short |
Late Cretaceous palaeoenvironments and biotas: an Antarctic perspective |
title_full |
Late Cretaceous palaeoenvironments and biotas: an Antarctic perspective |
title_fullStr |
Late Cretaceous palaeoenvironments and biotas: an Antarctic perspective |
title_full_unstemmed |
Late Cretaceous palaeoenvironments and biotas: an Antarctic perspective |
title_sort |
late cretaceous palaeoenvironments and biotas: an antarctic perspective |
publisher |
Cambridge University Press |
publishDate |
1992 |
url |
http://nora.nerc.ac.uk/id/eprint/518384/ https://doi.org/10.1017/S0954102092000555 |
geographic |
Antarctic The Antarctic Antarctic Peninsula Austral Ross Island New Zealand |
geographic_facet |
Antarctic The Antarctic Antarctic Peninsula Austral Ross Island New Zealand |
genre |
Antarc* Antarctic Antarctic Peninsula Antarctic Science Antarctica James Ross Island Ross Island |
genre_facet |
Antarc* Antarctic Antarctic Peninsula Antarctic Science Antarctica James Ross Island Ross Island |
op_relation |
Crame, J.A. orcid:0000-0002-5027-9965 . 1992 Late Cretaceous palaeoenvironments and biotas: an Antarctic perspective. Antarctic Science, 4 (04). 371-382. https://doi.org/10.1017/S0954102092000555 <https://doi.org/10.1017/S0954102092000555> |
op_doi |
https://doi.org/10.1017/S0954102092000555 |
container_title |
Antarctic Science |
container_volume |
4 |
container_issue |
4 |
container_start_page |
371 |
op_container_end_page |
382 |
_version_ |
1766251716262494208 |