id ftdatacite:10.1594/pangaea.79362
record_format openpolar
spelling ftdatacite:10.1594/pangaea.79362 2024-03-31T07:54:12+00:00 Dinocyst assemblages of site HM52-43 ... de Vernal, Anne Hillaire-Marcel, Claude Turon, Jean-Louis Matthiessen, Jens 2000 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.79362 https://doi.pangaea.de/10.1594/PANGAEA.79362 en eng PANGAEA https://dx.doi.org/10.1139/cjes-37-5-725 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 DEPTH, sediment/rock Nematosphaeropsis labyrinthus Peridinium faeroense Trinovantedinium capitatum Algidasphaeridium minutum Brigantedinium spp. Peridinoid type Polykrikos schwarzii Multispinula quanta Alexandrium excavatum Bitectatodinium tepikiense Impagidinium aculeatum Impagidinium patulum Impagidinium paradoxum Impagidinium sphaericum Operculodinium centrocarpum Spiniferites spp. Spiniferites bentori Spiniferites ramosus Spiniferites elongatus Spiniferites membranaceus Spiniferites mirabilis Lingulodinium machaerophorum Pyxidinopsis reticulata Ataxiodinium choane Impagidinium pallidum Algidasphaeridium minutum var. cesare Gravity corer Counting, dinoflagellate cysts Multiproxy Approach for the Reconstruction of the Glacial Ocean surface MARGO dataset Dataset Supplementary Dataset 2000 ftdatacite https://doi.org/10.1594/pangaea.7936210.1139/cjes-37-5-725 2024-03-04T14:22:19Z Past sea-surface conditions over the northern North Atlantic during the last glacial maximum were examined from the study of 61 deep-sea cores. The last glacial maximum time slice studied here corresponds to an interval between Heinrich layers H2 and H1, and spanning about 20-16 ka on a 14C time scale. Transfer functions based on dinocyst assemblages were used to reconstruct sea-surface temperature, salinity, and sea-ice cover. The results illustrate extensive sea-ice cover along the eastern Canadian margins and sea-ice spreading, only during winter, over most of the northern North Atlantic. On the whole, much colder winter prevailed, despite relatively mild conditions in August (10-15°C at most offshore sites), thus suggesting a larger seasonal contrast of temperatures than today. Lower salinity than at present is reconstructed, especially along the eastern Canadian and Scandinavian margins, likely because of meltwater supply from the surrounding ice sheets. These reconstructions contrast with those ... : Supplement to: de Vernal, Anne; Hillaire-Marcel, Claude; Turon, Jean-Louis; Matthiessen, Jens (2000): Reconstruction of sea-surface temperature, salinity, and sea-ice cover in the northern North Atlantic during the last glacial maximum based on dinocyst assemblages. Canadian Journal of Earth Sciences, 37(5), 725-750 ... Dataset North Atlantic Sea ice DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic DEPTH, sediment/rock
Nematosphaeropsis labyrinthus
Peridinium faeroense
Trinovantedinium capitatum
Algidasphaeridium minutum
Brigantedinium spp.
Peridinoid type
Polykrikos schwarzii
Multispinula quanta
Alexandrium excavatum
Bitectatodinium tepikiense
Impagidinium aculeatum
Impagidinium patulum
Impagidinium paradoxum
Impagidinium sphaericum
Operculodinium centrocarpum
Spiniferites spp.
Spiniferites bentori
Spiniferites ramosus
Spiniferites elongatus
Spiniferites membranaceus
Spiniferites mirabilis
Lingulodinium machaerophorum
Pyxidinopsis reticulata
Ataxiodinium choane
Impagidinium pallidum
Algidasphaeridium minutum var. cesare
Gravity corer
Counting, dinoflagellate cysts
Multiproxy Approach for the Reconstruction of the Glacial Ocean surface MARGO
spellingShingle DEPTH, sediment/rock
Nematosphaeropsis labyrinthus
Peridinium faeroense
Trinovantedinium capitatum
Algidasphaeridium minutum
Brigantedinium spp.
Peridinoid type
Polykrikos schwarzii
Multispinula quanta
Alexandrium excavatum
Bitectatodinium tepikiense
Impagidinium aculeatum
Impagidinium patulum
Impagidinium paradoxum
Impagidinium sphaericum
Operculodinium centrocarpum
Spiniferites spp.
Spiniferites bentori
Spiniferites ramosus
Spiniferites elongatus
Spiniferites membranaceus
Spiniferites mirabilis
Lingulodinium machaerophorum
Pyxidinopsis reticulata
Ataxiodinium choane
Impagidinium pallidum
Algidasphaeridium minutum var. cesare
Gravity corer
Counting, dinoflagellate cysts
Multiproxy Approach for the Reconstruction of the Glacial Ocean surface MARGO
de Vernal, Anne
Hillaire-Marcel, Claude
Turon, Jean-Louis
Matthiessen, Jens
Dinocyst assemblages of site HM52-43 ...
topic_facet DEPTH, sediment/rock
Nematosphaeropsis labyrinthus
Peridinium faeroense
Trinovantedinium capitatum
Algidasphaeridium minutum
Brigantedinium spp.
Peridinoid type
Polykrikos schwarzii
Multispinula quanta
Alexandrium excavatum
Bitectatodinium tepikiense
Impagidinium aculeatum
Impagidinium patulum
Impagidinium paradoxum
Impagidinium sphaericum
Operculodinium centrocarpum
Spiniferites spp.
Spiniferites bentori
Spiniferites ramosus
Spiniferites elongatus
Spiniferites membranaceus
Spiniferites mirabilis
Lingulodinium machaerophorum
Pyxidinopsis reticulata
Ataxiodinium choane
Impagidinium pallidum
Algidasphaeridium minutum var. cesare
Gravity corer
Counting, dinoflagellate cysts
Multiproxy Approach for the Reconstruction of the Glacial Ocean surface MARGO
description Past sea-surface conditions over the northern North Atlantic during the last glacial maximum were examined from the study of 61 deep-sea cores. The last glacial maximum time slice studied here corresponds to an interval between Heinrich layers H2 and H1, and spanning about 20-16 ka on a 14C time scale. Transfer functions based on dinocyst assemblages were used to reconstruct sea-surface temperature, salinity, and sea-ice cover. The results illustrate extensive sea-ice cover along the eastern Canadian margins and sea-ice spreading, only during winter, over most of the northern North Atlantic. On the whole, much colder winter prevailed, despite relatively mild conditions in August (10-15°C at most offshore sites), thus suggesting a larger seasonal contrast of temperatures than today. Lower salinity than at present is reconstructed, especially along the eastern Canadian and Scandinavian margins, likely because of meltwater supply from the surrounding ice sheets. These reconstructions contrast with those ... : Supplement to: de Vernal, Anne; Hillaire-Marcel, Claude; Turon, Jean-Louis; Matthiessen, Jens (2000): Reconstruction of sea-surface temperature, salinity, and sea-ice cover in the northern North Atlantic during the last glacial maximum based on dinocyst assemblages. Canadian Journal of Earth Sciences, 37(5), 725-750 ...
format Dataset
author de Vernal, Anne
Hillaire-Marcel, Claude
Turon, Jean-Louis
Matthiessen, Jens
author_facet de Vernal, Anne
Hillaire-Marcel, Claude
Turon, Jean-Louis
Matthiessen, Jens
author_sort de Vernal, Anne
title Dinocyst assemblages of site HM52-43 ...
title_short Dinocyst assemblages of site HM52-43 ...
title_full Dinocyst assemblages of site HM52-43 ...
title_fullStr Dinocyst assemblages of site HM52-43 ...
title_full_unstemmed Dinocyst assemblages of site HM52-43 ...
title_sort dinocyst assemblages of site hm52-43 ...
publisher PANGAEA
publishDate 2000
url https://dx.doi.org/10.1594/pangaea.79362
https://doi.pangaea.de/10.1594/PANGAEA.79362
genre North Atlantic
Sea ice
genre_facet North Atlantic
Sea ice
op_relation https://dx.doi.org/10.1139/cjes-37-5-725
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.7936210.1139/cjes-37-5-725
_version_ 1795034911312183296