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Late Cretaceous Temperature Evolution of the Southern High Latitudes: A TEX 86 Perspective
Author(s) -
O'Connor Lauren K.,
Robinson Stuart A.,
Naafs B. David A.,
Jenkyns Hugh C.,
Henson Sam,
Clarke Madeleine,
Pancost Richard D.
Publication year - 2019
Publication title -
paleoceanography and paleoclimatology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.927
H-Index - 127
eISSN - 2572-4525
pISSN - 2572-4517
DOI - 10.1029/2018pa003546
Subject(s) - cretaceous , geology , latitude , plateau (mathematics) , sea surface temperature , context (archaeology) , cenomanian , anomaly (physics) , climatology , paleoclimatology , oceanography , paleontology , climate change , mathematical analysis , physics , mathematics , geodesy , condensed matter physics
The Late Cretaceous was a greenhouse world, characterized by elevated temperatures and high atmospheric p CO 2 . Even in the context of an extreme greenhouse climate, existing planktic foraminiferal δ 18 O data from the Falkland Plateau (paleolatitude of ~55°S) suggest anomalous warmth, with sea‐surface temperatures (SSTs) >30 °C for much of the Late Cretaceous, followed by sudden cooling in the Campanian. Over the last two decades, there has been discussion as to whether these high δ 18 O‐based SSTs reflect a genuine temperature signal and, if so, whether there was a local temperature anomaly in the South Atlantic or whether the data are representative of zonal paleotemperatures at 55°S. To provide new insights into the degree of ocean warming in the southern high latitudes during the Late Cretaceous (Cenomanian to Campanian), new SST records from the Falkland and Kerguelen Plateaus are presented here using the organic geochemical paleothermometer TetraEther indeX of 86 carbon atoms (TEX 86 ). Overall, the TEX 86 data support the δ 18 O data, indicating extreme and widespread warmth in the middle to high southern latitudes in the Late Cretaceous, with SSTs from 27 to 37 °C. Crucially, the TEX 86 data show slow, steady cooling from the Turonian to the Campanian and suggest that temperature gradients during the Campanian did not become as steep as suggested by some planktic foraminiferal data.