Evaluating glycerol dialkyl glycerol tetraether (GDGT)-based reconstructions from varved lake sediments during the Holocene
Evaluating glycerol dialkyl glycerol tetraether (GDGT)-based reconstructions from varved lake sediments during the Holocene
Advances in proxy development and proxy reconstructions within the Holocene increasingly reveal climatic complexity. Annually laminated (varved) lacustrine records provide an opportunity to assess this complexity at high temporal resolution. Organic geochemical proxies offer the potential for quantitative palaeoclimate reconstruction, however, their application to different varved lake settings remains limited. Here we explore the use of isoprenoid and branched glycerol dialkyl glycerol tetraethers (GDGTs) preserved in varved sediments as proxies for temperature. We analyse three Holocene-aged annually laminated lacustrine records spanning different climate regions and lake settings across Europe (Diss Mere, UK; Nautajärvi, Finland; Meerfelder Maar, Germany); including intervals at multi-decadal resolution within the mid-Holocene. We show that isoprenoid GDGT distributions in annually laminated sediment sequences are largely derived from methanogenic Euryarchaeota and yield unreliable lake surface temperature reconstructions. Conversely, branched GDGT reconstructions show good coherence with instrumental temperature data in mid- and high-latitude environments. Although we show that lake or catchment-specific processes, including differences in processes linked to varve sedimentation, hypoxia, sediment influx and landscape development, can influence brGDGT distributions in varved lakes, the trends and range of variability of our brGDGT derived Holocene temperature reconstructions broadly agree with regional European Holocene reconstructions. This suggests that temperature exerts a first-order control on the methylation of brGDGTs in varved lake sequences. Combined with precise varve chronologies, these biomarker records can be used to generate highly resolved climate data across the Holocene.
1809-1832
Abrook, Ash
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Inglis, Gordon
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Langdon, Pete
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Bentley, Mckenzie
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Brauer, Achim
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Bull, Ian D.
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Fallows, Daisy Ella
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Lincoln, Paul
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Ojala, Antti. E. K.
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Whelton, Helen L.
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Martin-Puertas, Celia
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10 March 2026
Abrook, Ash
fce0b528-95c4-46d2-908e-44b8ad57f161
Inglis, Gordon
1651196d-916c-43cb-b5a0-9b3ecaf5d664
Langdon, Pete
95b97671-f9fe-4884-aca6-9aa3cd1a6d7f
Bentley, Mckenzie
14fff641-679d-4ff3-bac7-4d917c899158
Brauer, Achim
955179a5-79db-47fa-b33b-a7ee62534643
Bull, Ian D.
d9ba8a95-30cf-4f66-9d38-aae046d8349f
Fallows, Daisy Ella
f1366dc3-5bcf-4e58-b09f-76204aa2c4c4
Lincoln, Paul
c751e6ae-aa6b-4d5f-a7f4-746a5936a384
Ojala, Antti. E. K.
9f8e8124-8f72-4c6a-8dd3-146f5c016309
Whelton, Helen L.
7e28b817-502a-48a2-b81d-eb2b801a029a
Martin-Puertas, Celia
6901171c-f580-407b-81b4-9d7680e93f70
Abrook, Ash, Inglis, Gordon, Langdon, Pete, Bentley, Mckenzie, Brauer, Achim, Bull, Ian D., Fallows, Daisy Ella, Lincoln, Paul, Ojala, Antti. E. K., Whelton, Helen L. and Martin-Puertas, Celia
(2026)
Evaluating glycerol dialkyl glycerol tetraether (GDGT)-based reconstructions from varved lake sediments during the Holocene.
Biogeosciences, 23 (5), .
(doi:10.5194/bg-23-1809-2026).
Abstract
Advances in proxy development and proxy reconstructions within the Holocene increasingly reveal climatic complexity. Annually laminated (varved) lacustrine records provide an opportunity to assess this complexity at high temporal resolution. Organic geochemical proxies offer the potential for quantitative palaeoclimate reconstruction, however, their application to different varved lake settings remains limited. Here we explore the use of isoprenoid and branched glycerol dialkyl glycerol tetraethers (GDGTs) preserved in varved sediments as proxies for temperature. We analyse three Holocene-aged annually laminated lacustrine records spanning different climate regions and lake settings across Europe (Diss Mere, UK; Nautajärvi, Finland; Meerfelder Maar, Germany); including intervals at multi-decadal resolution within the mid-Holocene. We show that isoprenoid GDGT distributions in annually laminated sediment sequences are largely derived from methanogenic Euryarchaeota and yield unreliable lake surface temperature reconstructions. Conversely, branched GDGT reconstructions show good coherence with instrumental temperature data in mid- and high-latitude environments. Although we show that lake or catchment-specific processes, including differences in processes linked to varve sedimentation, hypoxia, sediment influx and landscape development, can influence brGDGT distributions in varved lakes, the trends and range of variability of our brGDGT derived Holocene temperature reconstructions broadly agree with regional European Holocene reconstructions. This suggests that temperature exerts a first-order control on the methylation of brGDGTs in varved lake sequences. Combined with precise varve chronologies, these biomarker records can be used to generate highly resolved climate data across the Holocene.
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Accepted/In Press date: 23 February 2026
Published date: 10 March 2026
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Local EPrints ID: 510259
URI: http://eprints.soton.ac.uk/id/eprint/510259
ISSN: 1726-4170
PURE UUID: e87179ca-fb33-4266-9139-877d71b81c47
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Date deposited: 24 Mar 2026 17:51
Last modified: 25 Mar 2026 03:16
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Author:
Ash Abrook
Author:
Mckenzie Bentley
Author:
Achim Brauer
Author:
Ian D. Bull
Author:
Daisy Ella Fallows
Author:
Paul Lincoln
Author:
Antti. E. K. Ojala
Author:
Helen L. Whelton
Author:
Celia Martin-Puertas
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