A global compilation of diatom silica oxygen isotope records from lake sediment: individual datasets in a single table

doi:doi:10.1594/PANGAEA.957167

A global compilation of diatom silica oxygen isotope records from lake sediment: individual datasets in a single table

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).

BibTex:

@dataset{Meister_Philip_and_Alexandre_Anne_and_Bailey_Hannah_and_Barker_Philip_and_Biskaborn_Boris_K_and_Broadman_Ellie_and_Cartier_Rosine_and_Chapligin_Bernhard_and_Couapel_Martine_JJ_and_Dean_Jonathan_R_and_Diekmann_Bernhard_and_Harding_Poppy_and_Henderson_Andrew_and_Hernandez_Armand_and_Herzschuh_Ulrike_and_Kostrova_Svetlana_S_and_Lacey_Jack_H_and_Leng_Melanie_J_and_Lücke_Andreas_and_Mackay_Anson_W_and_Magyari_Eniko_Katalin_and_Narancic_Biljana_and_Porchier_Cécile_and_Rosqvist_Gunhild_C_and_Shemesh_Aldo_and_Sonzogni_Corinne_and_Swann_George_E_A_and_Sylvestre_Florence_and_Meyer_Hanno_2024,
    abstract = {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).},
    author = {Meister, Philip and Alexandre, Anne and Bailey, Hannah and Barker, Philip and Biskaborn, Boris K and Broadman, Ellie and Cartier, Rosine and Chapligin, Bernhard and Couapel, Martine JJ and Dean, Jonathan R and Diekmann, Bernhard and Harding, Poppy and Henderson, Andrew and Hernandez, Armand and Herzschuh, Ulrike and Kostrova, Svetlana S and Lacey, Jack H and Leng, Melanie J and Lücke, Andreas and Mackay, Anson W and Magyari, Eniko Katalin and Narancic, Biljana and Porchier, Cécile and Rosqvist, Gunhild C and Shemesh, Aldo and Sonzogni, Corinne and Swann, George E A and Sylvestre, Florence and Meyer, Hanno},
    doi = {10.1594/PANGAEA.957167},
    institution = {PANGAEA (Chemistry)},
    keyword = {'18', 'Compilation', 'Diatom', 'Lake sediment core', 'delta O', 'paleoclimate proxy'},
    title = {A global compilation of diatom silica oxygen isotope records from lake sediment: individual datasets in a single table},
    url = {https://service.tib.eu/ldmservice/vdataset/png-doi-10-1594-pangaea-957167},
    year = {2024}
}