A global compilation of diatom silica oxygen isotope records from lake sediment

Oxygen isotopes in biogenic silica (δ18O BSi) from lake sediments allow for quantitative reconstruction of past hydroclimate and proxy–model comparison in terrestrial environments. The signals of individual records have been attributed to different factors, such as air temperature (T air ), atmosphe...

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Hauptverfasser: Meister, Philip, Alexandre, Anne, Bailey, Hannah, Barker, Philip, Biskaborn, Boris K, Broadman, Ellie, Cartier, Rosine, Chapligin, Bernhard, Couapel, Martine JJ, Dean, Jonathan R, Diekmann, Bernhard, Harding, Poppy, Henderson, Andrew, Hernandez, Armand, Herzschuh, Ulrike, Kostrova, Svetlana S, Lacey, Jack H, Leng, Melanie J, Lücke, Andreas, Mackay, Anson W, Magyari, Eniko Katalin, Narancic, Biljana, Porchier, Cécile, Rosqvist, Gunhild C, Shemesh, Aldo, Sonzogni, Corinne, Swann, George E A, Sylvestre, Florence, Meyer, Hanno
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creator Meister, Philip
Alexandre, Anne
Bailey, Hannah
Barker, Philip
Biskaborn, Boris K
Broadman, Ellie
Cartier, Rosine
Chapligin, Bernhard
Couapel, Martine JJ
Dean, Jonathan R
Diekmann, Bernhard
Harding, Poppy
Henderson, Andrew
Hernandez, Armand
Herzschuh, Ulrike
Kostrova, Svetlana S
Lacey, Jack H
Leng, Melanie J
Lücke, Andreas
Mackay, Anson W
Magyari, Eniko Katalin
Narancic, Biljana
Porchier, Cécile
Rosqvist, Gunhild C
Shemesh, Aldo
Sonzogni, Corinne
Swann, George E A
Sylvestre, Florence
Meyer, Hanno
description Oxygen isotopes in biogenic silica (δ18O BSi) from lake sediments allow for quantitative reconstruction of past hydroclimate and proxy–model comparison in terrestrial environments. The signals of individual records have been attributed to different factors, such as air temperature (T air ), atmospheric circulation patterns, hydrological changes and lake evaporation. Here, we provide 55 composite down–core records published to date and complemented with additional lake basin parameters (e.g. lake water residence time and catchment size) to best characterize the signal properties. Records feature widely different temporal coverage and resolution ranging from decadal–scale records covering the last 150 years to records with multi–millennial scale resolution spanning glacial–interglacial cycles. Best coverage in number of records (N=37) and datapoints (N=2112) is available for northern hemispheric (NH) extra–tropic regions throughout the Holocene (corresponding to Marine Isotope Stage 1; MIS 1).
doi_str_mv 10.1594/pangaea.957160
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identifier DOI: 10.1594/pangaea.957160
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language eng
recordid cdi_datacite_primary_10_1594_pangaea_957160
source DataCite
subjects Compilation
delta O-18
Diatom
Lake sediment core
paleoclimate proxy
title A global compilation of diatom silica oxygen isotope records from lake sediment
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