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Mid-latitude continental temperatures through the early Eocene in western Europe

Mid-latitude continental temperatures through the early Eocene in western Europe
Mid-latitude continental temperatures through the early Eocene in western Europe
Branched glycerol dialkyl glycerol tetraethers (brGDGTs) are increasingly used to reconstruct mean annual air temperature (MAAT) during the early Paleogene. However, the application of this proxy in coal deposits is limited and brGDGTs have only been detected in immature coals (i.e. lignites). Using samples recovered from Schöningen, Germany (∼48°N palaeolatitude), we provide the first detailed study into the occurrence and distribution of brGDGTs through a sequence of early Eocene lignites and associated interbeds. BrGDGTs are abundant and present in every sample. In comparison to modern studies, changes in vegetation type do not appear to significantly impact brGDGT distributions; however, there are subtle differences between lignites – representing peat-forming environments – and siliciclastic nearshore marine interbed depositional environments. Using the most recent brGDGT temperature calibration (MATmr) developed for soils, we generate the first continental temperature record from central-western continental Europe through the early Eocene. Lignite-derived MAAT estimates range from 23 to 26 °C while those derived from the nearshore marine interbeds exceed 20 °C. These estimates are consistent with other mid-latitude environments and model simulations, indicating enhanced mid-latitude, early Eocene warmth. In the basal part of the section studied, warming is recorded in both the lignites (∼2 °C) and nearshore marine interbeds (∼2–3 °C). This culminates in a long-term temperature maximum, likely including the Early Eocene Climatic Optimum (EECO). Although this long-term warming trend is relatively well established in the marine realm, it has rarely been shown in terrestrial settings. Using a suite of model simulations we show that the magnitude of warming at Schöningen is broadly consistent with a doubling of CO2, in agreement with late Paleocene and early Eocene pCO2 estimates.
0012-821X
86-96
Inglis, Gordon N.
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Collinson, Margaret E.
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Riegel, Walter
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Wilde, Volker
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Farnsworth, Alexander
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Lunt, Daniel J.
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Valdes, Paul
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Robson, Brittany E.
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Scott, Andrew C.
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Lenz, Olaf K.
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Naafs, B. David A.
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Pancost, Richard D.
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Inglis, Gordon N.
1651196d-916c-43cb-b5a0-9b3ecaf5d664
Collinson, Margaret E.
4558b0e7-a6c1-4b1c-a6e8-36e3e9f3c320
Riegel, Walter
83bcdc4a-42f5-4f98-9121-081ad267dbbd
Wilde, Volker
efe0ffd3-3347-410d-9f0f-2d5fc5deb996
Farnsworth, Alexander
42c07817-9776-49d0-af90-e562d8b85482
Lunt, Daniel J.
931ecfb5-1f50-412c-8f01-a46d69b1f82f
Valdes, Paul
1d96598c-56b8-4582-bc4a-e5618309641b
Robson, Brittany E.
56e5e38f-6c81-435a-b0f1-35f8535b05c5
Scott, Andrew C.
5045cc49-54a0-4bd9-b2ce-d29ec7a10a5a
Lenz, Olaf K.
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Naafs, B. David A.
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Pancost, Richard D.
5914e19e-7777-4304-9fd8-86e2e9cfe8a1

Inglis, Gordon N., Collinson, Margaret E., Riegel, Walter, Wilde, Volker, Farnsworth, Alexander, Lunt, Daniel J., Valdes, Paul, Robson, Brittany E., Scott, Andrew C., Lenz, Olaf K., Naafs, B. David A. and Pancost, Richard D. (2017) Mid-latitude continental temperatures through the early Eocene in western Europe. Earth and Planetary Science Letters, 460, 86-96. (doi:10.1016/j.epsl.2016.12.009).

Record type: Article

Abstract

Branched glycerol dialkyl glycerol tetraethers (brGDGTs) are increasingly used to reconstruct mean annual air temperature (MAAT) during the early Paleogene. However, the application of this proxy in coal deposits is limited and brGDGTs have only been detected in immature coals (i.e. lignites). Using samples recovered from Schöningen, Germany (∼48°N palaeolatitude), we provide the first detailed study into the occurrence and distribution of brGDGTs through a sequence of early Eocene lignites and associated interbeds. BrGDGTs are abundant and present in every sample. In comparison to modern studies, changes in vegetation type do not appear to significantly impact brGDGT distributions; however, there are subtle differences between lignites – representing peat-forming environments – and siliciclastic nearshore marine interbed depositional environments. Using the most recent brGDGT temperature calibration (MATmr) developed for soils, we generate the first continental temperature record from central-western continental Europe through the early Eocene. Lignite-derived MAAT estimates range from 23 to 26 °C while those derived from the nearshore marine interbeds exceed 20 °C. These estimates are consistent with other mid-latitude environments and model simulations, indicating enhanced mid-latitude, early Eocene warmth. In the basal part of the section studied, warming is recorded in both the lignites (∼2 °C) and nearshore marine interbeds (∼2–3 °C). This culminates in a long-term temperature maximum, likely including the Early Eocene Climatic Optimum (EECO). Although this long-term warming trend is relatively well established in the marine realm, it has rarely been shown in terrestrial settings. Using a suite of model simulations we show that the magnitude of warming at Schöningen is broadly consistent with a doubling of CO2, in agreement with late Paleocene and early Eocene pCO2 estimates.

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Accepted/In Press date: 7 December 2016
e-pub ahead of print date: 22 December 2016
Published date: 15 February 2017

Identifiers

Local EPrints ID: 437532
URI: http://eprints.soton.ac.uk/id/eprint/437532
ISSN: 0012-821X
PURE UUID: a2c7de87-2d2f-4e40-b9f6-2e24e24e5493
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: Margaret E. Collinson
Author: Walter Riegel
Author: Volker Wilde
Author: Alexander Farnsworth
Author: Daniel J. Lunt
Author: Paul Valdes
Author: Brittany E. Robson
Author: Andrew C. Scott
Author: Olaf K. Lenz
Author: B. David A. Naafs
Author: Richard D. Pancost

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