Alkenone analyses of sediment core MSM45/19_2

The presented data originates from the 1306cm long gravity core MSM45-19-2 (58°45.68 N, 61°56.25 W, 202m water depth) taken during R/V Maria S. Merian cruise MSM45 in August 2015 at 202 m water depth on the northern Labrador Shelf, northeast Canada, northwest Atlantic. In order to fully understand t...

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Bibliographic Details
Main Authors: Lochte, Annalena Antonia, Schneider, Ralph R
Format: Dataset
Language:English
Published: PANGAEA 2022
Subjects:
sum
GC
SST
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.945742
https://doi.org/10.1594/PANGAEA.945742
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.945742
record_format openpolar
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic 8.2 ka event
Alkenone
C37:4
sum
DEPTH
sediment/rock
GC
Gravity corer
Holocene
Labrador Sea
Maria S. Merian
MSM45
MSM45_418-2
MSM45-19-2
SST
spellingShingle 8.2 ka event
Alkenone
C37:4
sum
DEPTH
sediment/rock
GC
Gravity corer
Holocene
Labrador Sea
Maria S. Merian
MSM45
MSM45_418-2
MSM45-19-2
SST
Lochte, Annalena Antonia
Schneider, Ralph R
Alkenone analyses of sediment core MSM45/19_2
topic_facet 8.2 ka event
Alkenone
C37:4
sum
DEPTH
sediment/rock
GC
Gravity corer
Holocene
Labrador Sea
Maria S. Merian
MSM45
MSM45_418-2
MSM45-19-2
SST
description The presented data originates from the 1306cm long gravity core MSM45-19-2 (58°45.68 N, 61°56.25 W, 202m water depth) taken during R/V Maria S. Merian cruise MSM45 in August 2015 at 202 m water depth on the northern Labrador Shelf, northeast Canada, northwest Atlantic. In order to fully understand the dynamics that contributed to the establishment of modern Labrador Sea circulation, detailed reconstructions of the major paleoceanographic changes through the Holocene are critical. Therefore, this study aims to provide new information on bottom (i.e. subsurface) water mass composition as well as on changes in primary productivity and sea-ice conditions in the LC during the Holocene. Reconstructions are based on alkenone biomarker concentrations to provide a better understanding of the dynamics of different water masses that contributed to the establishment of modern Labrador Sea. circulation. Long-chain alkenones are biosynthesized by haptophytes (e.g. the coccolithophorid Emiliania huxleyi) living in surface waters. They consist of 37 carbon atoms with 2, 3, or 4 double bonds (C37:2, C37:3, and C37:4, respectively). Alkenone analyses were carried out at the Biomarker Laboratory at Kiel University. In total, 290 samples were analyzed in 5-cm intervals. Long-chained alkenones (C37) were extracted from 2 to 3 g of homogenized bulk sediment, using an Accelerated Solvent Extractor (Dionex ASE-200) with a mixture of 9:1 (v/v) of dichloromethane: methanol (DCM: MeOH) at 100°C and 100 bar N2 (g) pressure for 20 min. Extracts were cooled at −20°C and brought to near dryness by Syncore polyvap at 40°C and 490 mbar. For the identification and quantification of C37:2, C37:3, and C37:4 compounds, we used a multi-dimensional, double gas column chromatography (MD-GC) set up with two Agilent 6890 gas chromatographs (Etourneau et al., 2010). The addition of an internal standard prior to extraction (cholestane (C27H48) and hexatriacontane (C36H74)) allowed quantification of the three different compounds in nanograms per gram dry ...
format Dataset
author Lochte, Annalena Antonia
Schneider, Ralph R
author_facet Lochte, Annalena Antonia
Schneider, Ralph R
author_sort Lochte, Annalena Antonia
title Alkenone analyses of sediment core MSM45/19_2
title_short Alkenone analyses of sediment core MSM45/19_2
title_full Alkenone analyses of sediment core MSM45/19_2
title_fullStr Alkenone analyses of sediment core MSM45/19_2
title_full_unstemmed Alkenone analyses of sediment core MSM45/19_2
title_sort alkenone analyses of sediment core msm45/19_2
publisher PANGAEA
publishDate 2022
url https://doi.pangaea.de/10.1594/PANGAEA.945742
https://doi.org/10.1594/PANGAEA.945742
op_coverage LATITUDE: 58.761330 * LONGITUDE: -61.937500 * DATE/TIME START: 2015-08-10T18:20:00 * DATE/TIME END: 2015-08-10T18:20:00 * MINIMUM DEPTH, sediment/rock: 0.03 m * MAXIMUM DEPTH, sediment/rock: 13.03 m
long_lat ENVELOPE(-58.000,-58.000,56.000,56.000)
ENVELOPE(-61.937500,-61.937500,58.761330,58.761330)
geographic Canada
Labrador Shelf
geographic_facet Canada
Labrador Shelf
genre Labrador Sea
Northwest Atlantic
Sea ice
genre_facet Labrador Sea
Northwest Atlantic
Sea ice
op_relation Lochte, Annalena Antonia; Repschläger, Janne; Seidenkrantz, Marit-Solveig; Kienast, Markus; Blanz, Thomas; Schneider, Ralph R (2019): Holocene water mass changes in the Labrador Current. The Holocene, 29(4), 676-690, https://doi.org/10.1177/0959683618824752
Blanz, Thomas; Emeis, Kay-Christian; Siegel, Herbert (2005): Controls on alkenone unsaturation ratios along the salinity gradient between the open ocean and the Baltic Sea. Geochimica et Cosmochimica Acta, 69(14), 3589-3600, https://doi.org/10.1016/j.gca.2005.02.026
Etourneau, Johan; Schneider, Ralph R; Blanz, Thomas; Martinez, Philippe (2010): Intensification of the Walker and Hadley atmospheric circulations during the Pliocene-Pleistocene climate transition. Earth and Planetary Science Letters, 297(1-2), 103-110, https://doi.org/10.1016/j.epsl.2010.06.010
https://doi.pangaea.de/10.1594/PANGAEA.945742
https://doi.org/10.1594/PANGAEA.945742
op_rights CC-BY-4.0: Creative Commons Attribution 4.0 International
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.1594/PANGAEA.94574210.1177/095968361882475210.1016/j.gca.2005.02.02610.1016/j.epsl.2010.06.010
_version_ 1802646586781597696
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.945742 2024-06-23T07:54:26+00:00 Alkenone analyses of sediment core MSM45/19_2 Lochte, Annalena Antonia Schneider, Ralph R LATITUDE: 58.761330 * LONGITUDE: -61.937500 * DATE/TIME START: 2015-08-10T18:20:00 * DATE/TIME END: 2015-08-10T18:20:00 * MINIMUM DEPTH, sediment/rock: 0.03 m * MAXIMUM DEPTH, sediment/rock: 13.03 m 2022 text/tab-separated-values, 398 data points https://doi.pangaea.de/10.1594/PANGAEA.945742 https://doi.org/10.1594/PANGAEA.945742 en eng PANGAEA Lochte, Annalena Antonia; Repschläger, Janne; Seidenkrantz, Marit-Solveig; Kienast, Markus; Blanz, Thomas; Schneider, Ralph R (2019): Holocene water mass changes in the Labrador Current. The Holocene, 29(4), 676-690, https://doi.org/10.1177/0959683618824752 Blanz, Thomas; Emeis, Kay-Christian; Siegel, Herbert (2005): Controls on alkenone unsaturation ratios along the salinity gradient between the open ocean and the Baltic Sea. Geochimica et Cosmochimica Acta, 69(14), 3589-3600, https://doi.org/10.1016/j.gca.2005.02.026 Etourneau, Johan; Schneider, Ralph R; Blanz, Thomas; Martinez, Philippe (2010): Intensification of the Walker and Hadley atmospheric circulations during the Pliocene-Pleistocene climate transition. Earth and Planetary Science Letters, 297(1-2), 103-110, https://doi.org/10.1016/j.epsl.2010.06.010 https://doi.pangaea.de/10.1594/PANGAEA.945742 https://doi.org/10.1594/PANGAEA.945742 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess 8.2 ka event Alkenone C37:4 sum DEPTH sediment/rock GC Gravity corer Holocene Labrador Sea Maria S. Merian MSM45 MSM45_418-2 MSM45-19-2 SST Dataset 2022 ftpangaea https://doi.org/10.1594/PANGAEA.94574210.1177/095968361882475210.1016/j.gca.2005.02.02610.1016/j.epsl.2010.06.010 2024-06-12T14:17:12Z The presented data originates from the 1306cm long gravity core MSM45-19-2 (58°45.68 N, 61°56.25 W, 202m water depth) taken during R/V Maria S. Merian cruise MSM45 in August 2015 at 202 m water depth on the northern Labrador Shelf, northeast Canada, northwest Atlantic. In order to fully understand the dynamics that contributed to the establishment of modern Labrador Sea circulation, detailed reconstructions of the major paleoceanographic changes through the Holocene are critical. Therefore, this study aims to provide new information on bottom (i.e. subsurface) water mass composition as well as on changes in primary productivity and sea-ice conditions in the LC during the Holocene. Reconstructions are based on alkenone biomarker concentrations to provide a better understanding of the dynamics of different water masses that contributed to the establishment of modern Labrador Sea. circulation. Long-chain alkenones are biosynthesized by haptophytes (e.g. the coccolithophorid Emiliania huxleyi) living in surface waters. They consist of 37 carbon atoms with 2, 3, or 4 double bonds (C37:2, C37:3, and C37:4, respectively). Alkenone analyses were carried out at the Biomarker Laboratory at Kiel University. In total, 290 samples were analyzed in 5-cm intervals. Long-chained alkenones (C37) were extracted from 2 to 3 g of homogenized bulk sediment, using an Accelerated Solvent Extractor (Dionex ASE-200) with a mixture of 9:1 (v/v) of dichloromethane: methanol (DCM: MeOH) at 100°C and 100 bar N2 (g) pressure for 20 min. Extracts were cooled at −20°C and brought to near dryness by Syncore polyvap at 40°C and 490 mbar. For the identification and quantification of C37:2, C37:3, and C37:4 compounds, we used a multi-dimensional, double gas column chromatography (MD-GC) set up with two Agilent 6890 gas chromatographs (Etourneau et al., 2010). The addition of an internal standard prior to extraction (cholestane (C27H48) and hexatriacontane (C36H74)) allowed quantification of the three different compounds in nanograms per gram dry ... Dataset Labrador Sea Northwest Atlantic Sea ice PANGAEA - Data Publisher for Earth & Environmental Science Canada Labrador Shelf ENVELOPE(-58.000,-58.000,56.000,56.000) ENVELOPE(-61.937500,-61.937500,58.761330,58.761330)