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Early Paleogene evolution of terrestrial climate in the SW Pacific, Southern New Zealand

Early Paleogene evolution of terrestrial climate in the SW Pacific, Southern New Zealand
Early Paleogene evolution of terrestrial climate in the SW Pacific, Southern New Zealand
We present a long‐term record of terrestrial climate change for the Early Paleogene of the Southern Hemisphere that complements previously reported marine temperature records. Using the MBT′‐CBT proxy, based on the distribution of soil bacterial glycerol dialkyl glycerol tetraether lipids, we reconstructed mean annual air temperature (MAT) from the Middle Paleocene to Middle Eocene (62–42 Ma) for southern New Zealand. This record is consistent with temperature estimates derived from leaf fossils and palynology, as well as previously published MBT′‐CBT records, which provides confidence in absolute temperature estimates. Our record indicates that through this interval, temperatures were typically 5°C warmer than those of today at such latitudes, with more pronounced warming during the Early Eocene Climate Optimum (EECO; ∼50 Ma) when MAT was ∼20°C. Moreover, the EECO MATs are similar to those determined for Antarctica, with a weak high‐latitude terrestrial temperature gradient (∼5°C) developing by the Middle Eocene. We also document a short‐lived cooling episode in the early Late Paleocene when MAT was comparable to present. This record corroborates the trends documented by sea surface temperature (SST) proxies, although absolute SSTs are up to 6°C warmer than MATs. Although the high‐calibration error of the MBT′‐CBT proxy dictates caution, the good match between our MAT results and modeled temperatures supports the suggestion that SST records suffer from a warm (summer?) bias, particularly during times of peak warming.
1525-2027
5413-5429
Pancost, Richard D.
5914e19e-7777-4304-9fd8-86e2e9cfe8a1
Taylor, Kyle W.R.
ae845801-374a-405f-a15d-4d29e1014f68
Inglis, Gordon N.
1651196d-916c-43cb-b5a0-9b3ecaf5d664
Kennedy, Elizabeth M.
77346796-f312-4310-afd1-8192dc45a089
Handley, Luke
e2d80819-9caa-40b5-963c-eb9b827133ad
Hollis, Christopher J.
203511ab-eec4-41c5-b718-622189de5dfc
Crouch, Erica M.
8d93a076-3dd9-4435-896d-c5c4ebc01b01
Pross, Jörg
7c848424-852f-467b-90f0-19d4f8d4ae01
Huber, Matthew
cac8c146-e2e3-4758-9fe9-46aa85e35ad2
Schouten, Stefan
0d0291ca-b8dc-48a2-b61c-798c650ec1fd
Pancost, Richard D.
5914e19e-7777-4304-9fd8-86e2e9cfe8a1
Taylor, Kyle W.R.
ae845801-374a-405f-a15d-4d29e1014f68
Inglis, Gordon N.
1651196d-916c-43cb-b5a0-9b3ecaf5d664
Kennedy, Elizabeth M.
77346796-f312-4310-afd1-8192dc45a089
Handley, Luke
e2d80819-9caa-40b5-963c-eb9b827133ad
Hollis, Christopher J.
203511ab-eec4-41c5-b718-622189de5dfc
Crouch, Erica M.
8d93a076-3dd9-4435-896d-c5c4ebc01b01
Pross, Jörg
7c848424-852f-467b-90f0-19d4f8d4ae01
Huber, Matthew
cac8c146-e2e3-4758-9fe9-46aa85e35ad2
Schouten, Stefan
0d0291ca-b8dc-48a2-b61c-798c650ec1fd

Pancost, Richard D., Taylor, Kyle W.R., Inglis, Gordon N., Kennedy, Elizabeth M., Handley, Luke, Hollis, Christopher J., Crouch, Erica M., Pross, Jörg, Huber, Matthew and Schouten, Stefan (2013) Early Paleogene evolution of terrestrial climate in the SW Pacific, Southern New Zealand. Geochemistry, Geophysics, Geosystems, 14 (12), 5413-5429. (doi:10.1002/2013GC004935).

Record type: Article

Abstract

We present a long‐term record of terrestrial climate change for the Early Paleogene of the Southern Hemisphere that complements previously reported marine temperature records. Using the MBT′‐CBT proxy, based on the distribution of soil bacterial glycerol dialkyl glycerol tetraether lipids, we reconstructed mean annual air temperature (MAT) from the Middle Paleocene to Middle Eocene (62–42 Ma) for southern New Zealand. This record is consistent with temperature estimates derived from leaf fossils and palynology, as well as previously published MBT′‐CBT records, which provides confidence in absolute temperature estimates. Our record indicates that through this interval, temperatures were typically 5°C warmer than those of today at such latitudes, with more pronounced warming during the Early Eocene Climate Optimum (EECO; ∼50 Ma) when MAT was ∼20°C. Moreover, the EECO MATs are similar to those determined for Antarctica, with a weak high‐latitude terrestrial temperature gradient (∼5°C) developing by the Middle Eocene. We also document a short‐lived cooling episode in the early Late Paleocene when MAT was comparable to present. This record corroborates the trends documented by sea surface temperature (SST) proxies, although absolute SSTs are up to 6°C warmer than MATs. Although the high‐calibration error of the MBT′‐CBT proxy dictates caution, the good match between our MAT results and modeled temperatures supports the suggestion that SST records suffer from a warm (summer?) bias, particularly during times of peak warming.

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More information

Accepted/In Press date: 18 November 2013
e-pub ahead of print date: 25 November 2013
Published date: December 2013

Identifiers

Local EPrints ID: 437539
URI: http://eprints.soton.ac.uk/id/eprint/437539
ISSN: 1525-2027
PURE UUID: c770520e-5e19-4f2e-b6d0-a30b814a672f
ORCID for Gordon N. Inglis: ORCID iD orcid.org/0000-0002-0032-4668

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Date deposited: 04 Feb 2020 17:30
Last modified: 17 Mar 2024 04:00

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Contributors

Author: Richard D. Pancost
Author: Kyle W.R. Taylor
Author: Elizabeth M. Kennedy
Author: Luke Handley
Author: Christopher J. Hollis
Author: Erica M. Crouch
Author: Jörg Pross
Author: Matthew Huber
Author: Stefan Schouten

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