Ice-rafting history in the Labrador Sea during the last millennium ...

Arctic freshwater discharges to the Labrador Sea from melting glaciers and sea-ice can have a deep impact on ocean circulation dynamics in the North Atlantic, modifying climate and deep water formation in this region. In this study, we present for the first time a high resolution record of ice-rafti...

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Main Authors: Alonso-Garcia, Montserrat, Kleiven, Helga F, McManus, Jerry F, Moffa-Sanchez, Paola, Broecker, Wallace S, Flower, Benjamin P
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2017
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.874286
https://doi.pangaea.de/10.1594/PANGAEA.874286
id ftdatacite:10.1594/pangaea.874286
record_format openpolar
spelling ftdatacite:10.1594/pangaea.874286 2024-04-28T08:10:53+00:00 Ice-rafting history in the Labrador Sea during the last millennium ... Alonso-Garcia, Montserrat Kleiven, Helga F McManus, Jerry F Moffa-Sanchez, Paola Broecker, Wallace S Flower, Benjamin P 2017 application/zip https://dx.doi.org/10.1594/pangaea.874286 https://doi.pangaea.de/10.1594/PANGAEA.874286 en eng PANGAEA https://dx.doi.org/10.5194/cp-13-317-2017 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Gravity corer article Supplementary Publication Series of Datasets Collection 2017 ftdatacite https://doi.org/10.1594/pangaea.87428610.5194/cp-13-317-2017 2024-04-02T10:00:39Z Arctic freshwater discharges to the Labrador Sea from melting glaciers and sea-ice can have a deep impact on ocean circulation dynamics in the North Atlantic, modifying climate and deep water formation in this region. In this study, we present for the first time a high resolution record of ice-rafting in the Labrador Sea over the last millennium to assess the effects of freshwater discharges in this region on ocean circulation and climate. The occurrence of ice-rafted debris (IRD) in the Labrador Sea was studied using sediments from Site GS06-144-03 (57.29° N, 48.37° W, 3432 m water depth). IRD from the fraction 63-150 µm shows particularly high concentrations during the intervals: ~1000-1100, ~ 1150-1250, ~1400-1450, ~1650-1700 and ~1750-1800 yr AD. The first two intervals occurred during the Medieval Climate Anomaly (MCA), whereas the others took place within the Little Ice Age (LIA). Mineralogical identification indicates that the main IRD source during the MCA was SE Greenland. In contrast, the ... : Supplement to: Alonso-Garcia, Montserrat; Kleiven, Helga F; McManus, Jerry F; Moffa-Sanchez, Paola; Broecker, Wallace S; Flower, Benjamin P (2017): Freshening of the Labrador Sea as a trigger for Little Ice Age development. Climate of the Past, 13(4), 317-331 ... Article in Journal/Newspaper Arctic Greenland Labrador Sea 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 Gravity corer
spellingShingle Gravity corer
Alonso-Garcia, Montserrat
Kleiven, Helga F
McManus, Jerry F
Moffa-Sanchez, Paola
Broecker, Wallace S
Flower, Benjamin P
Ice-rafting history in the Labrador Sea during the last millennium ...
topic_facet Gravity corer
description Arctic freshwater discharges to the Labrador Sea from melting glaciers and sea-ice can have a deep impact on ocean circulation dynamics in the North Atlantic, modifying climate and deep water formation in this region. In this study, we present for the first time a high resolution record of ice-rafting in the Labrador Sea over the last millennium to assess the effects of freshwater discharges in this region on ocean circulation and climate. The occurrence of ice-rafted debris (IRD) in the Labrador Sea was studied using sediments from Site GS06-144-03 (57.29° N, 48.37° W, 3432 m water depth). IRD from the fraction 63-150 µm shows particularly high concentrations during the intervals: ~1000-1100, ~ 1150-1250, ~1400-1450, ~1650-1700 and ~1750-1800 yr AD. The first two intervals occurred during the Medieval Climate Anomaly (MCA), whereas the others took place within the Little Ice Age (LIA). Mineralogical identification indicates that the main IRD source during the MCA was SE Greenland. In contrast, the ... : Supplement to: Alonso-Garcia, Montserrat; Kleiven, Helga F; McManus, Jerry F; Moffa-Sanchez, Paola; Broecker, Wallace S; Flower, Benjamin P (2017): Freshening of the Labrador Sea as a trigger for Little Ice Age development. Climate of the Past, 13(4), 317-331 ...
format Article in Journal/Newspaper
author Alonso-Garcia, Montserrat
Kleiven, Helga F
McManus, Jerry F
Moffa-Sanchez, Paola
Broecker, Wallace S
Flower, Benjamin P
author_facet Alonso-Garcia, Montserrat
Kleiven, Helga F
McManus, Jerry F
Moffa-Sanchez, Paola
Broecker, Wallace S
Flower, Benjamin P
author_sort Alonso-Garcia, Montserrat
title Ice-rafting history in the Labrador Sea during the last millennium ...
title_short Ice-rafting history in the Labrador Sea during the last millennium ...
title_full Ice-rafting history in the Labrador Sea during the last millennium ...
title_fullStr Ice-rafting history in the Labrador Sea during the last millennium ...
title_full_unstemmed Ice-rafting history in the Labrador Sea during the last millennium ...
title_sort ice-rafting history in the labrador sea during the last millennium ...
publisher PANGAEA
publishDate 2017
url https://dx.doi.org/10.1594/pangaea.874286
https://doi.pangaea.de/10.1594/PANGAEA.874286
genre Arctic
Greenland
Labrador Sea
North Atlantic
Sea ice
genre_facet Arctic
Greenland
Labrador Sea
North Atlantic
Sea ice
op_relation https://dx.doi.org/10.5194/cp-13-317-2017
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.87428610.5194/cp-13-317-2017
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