Biomarker concentrations in gravity core MSM45_19-2 ...
Sea ice and paleoenvironmental conditions were reconstructed based on gravity core MSM45_19-2 from the northern Labrador Shelf. Gravity core MSM45_19-2 was obtained during R/V Maria S. Merian expedition MSM45 (58°45.68'N, 61°56.25'W, water depth: 202 m) in 2015 (Schneider et al., 2016).For...
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Online Access: | https://dx.doi.org/10.1594/pangaea.949065 https://doi.pangaea.de/10.1594/PANGAEA.949065 |
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ftdatacite:10.1594/pangaea.949065 2024-03-31T07:53:13+00:00 Biomarker concentrations in gravity core MSM45_19-2 ... Kolling, Henriette Marie Schneider, Ralph R Stein, Ruediger Fahl, Kirsten 2022 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.949065 https://doi.pangaea.de/10.1594/PANGAEA.949065 en eng PANGAEA https://dx.doi.org/10.1029/2022pa004578 https://dx.doi.org/10.2312/cr_msm45 https://dx.doi.org/10.1016/j.epsl.2015.09.020 https://dx.doi.org/10.1016/j.epsl.2012.07.009 https://dx.doi.org/10.1016/j.orggeochem.2015.12.007 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 8.2 ka event Biomarker brassica sterol campesterol dionsterol HBI III Holocene IP25 Labrador Shelf primary production Sea ice Terrigenious input DEPTH, sediment/rock Accumulation rate per year 2,6,10,14-Tetramethyl-7-3-methylpent-4-enylpentadecane per unit sediment mass 2,6,10,14-Tetramethyl-7-3-methylpent-4-enylpentadecane, per unit mass total organic carbon Accumulation rate, 2,6,10,14-Tetramethyl-7-3-methylpent-4-enylpentadecane per year Highly branched isoprenoids Z, triunsatured per unit sediment mass Highly branched isoprenoids Z, triunsatured, per unit mass total organic carbon Accumulation rate, highly branched isoprenoids Z, triunsatured per year 24-Methylcholesta-5,22E-dien-3beta-ol per unit sediment mass 24-Methylcholesta-5,22E-dien-3beta-ol, per unit mass total organic carbon Accumulation rate, 24-Methylcholesta-5,22E-dien-3beta-ol per year 4alpha,23,24-Trimethyl-5alpha-cholest-22E-en-3beta-ol per unit sediment mass 4alpha,23,24-Trimethyl-5alpha-cholest-22E-en-3beta-ol, per unit mass total organic carbon Accumulation rate, 4alpha,23,24-Trimethyl-5alpha-cholest-22E-en-3beta-ol per year 24-Methylcholest-5-en-3beta-ol per unit sediment mass 24-Methylcholest-5-en-3beta-ol, per unit mass total organic carbon Accumulation rate, 24-Methylcholest-5-en-3beta-ol per year Gravity corer MSM45 Maria S. Merian dataset Dataset 2022 ftdatacite https://doi.org/10.1594/pangaea.94906510.1029/2022pa00457810.2312/cr_msm4510.1016/j.epsl.2015.09.02010.1016/j.epsl.2012.07.00910.1016/j.orggeochem.2015.12.007 2024-03-04T13:55:22Z Sea ice and paleoenvironmental conditions were reconstructed based on gravity core MSM45_19-2 from the northern Labrador Shelf. Gravity core MSM45_19-2 was obtained during R/V Maria S. Merian expedition MSM45 (58°45.68'N, 61°56.25'W, water depth: 202 m) in 2015 (Schneider et al., 2016).For paleoenvironmental reconstructions of the last 9,000 years BP, biomarkers representing sea ice algae productivity (IP25), open-water phytoplankton productivity (brassicasterol, dinosterol and HBI III (Z)) and terrigenous input (campesterol) where analyzed. Aim of this study was to investigate (i) the role sea ice played before and during the final demise of the Laurentide Ice Sheet between 8.7 and 8.2 kyr BP, and (ii) the effects of meltwater events on remaining sea-ice cover and primary productivity.Concentrations of specific biomarkers were analyzed. 4-5 g of each sediment sample were extracted by sonication (3 x 15 min) using dichloromethane:methanol (2:1 v/v; 30 ml) as solvent. Prior to biomarker extraction two ... Dataset ice algae Ice Sheet Sea ice DataCite Metadata Store (German National Library of Science and Technology) Labrador Shelf ENVELOPE(-58.000,-58.000,56.000,56.000) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
8.2 ka event Biomarker brassica sterol campesterol dionsterol HBI III Holocene IP25 Labrador Shelf primary production Sea ice Terrigenious input DEPTH, sediment/rock Accumulation rate per year 2,6,10,14-Tetramethyl-7-3-methylpent-4-enylpentadecane per unit sediment mass 2,6,10,14-Tetramethyl-7-3-methylpent-4-enylpentadecane, per unit mass total organic carbon Accumulation rate, 2,6,10,14-Tetramethyl-7-3-methylpent-4-enylpentadecane per year Highly branched isoprenoids Z, triunsatured per unit sediment mass Highly branched isoprenoids Z, triunsatured, per unit mass total organic carbon Accumulation rate, highly branched isoprenoids Z, triunsatured per year 24-Methylcholesta-5,22E-dien-3beta-ol per unit sediment mass 24-Methylcholesta-5,22E-dien-3beta-ol, per unit mass total organic carbon Accumulation rate, 24-Methylcholesta-5,22E-dien-3beta-ol per year 4alpha,23,24-Trimethyl-5alpha-cholest-22E-en-3beta-ol per unit sediment mass 4alpha,23,24-Trimethyl-5alpha-cholest-22E-en-3beta-ol, per unit mass total organic carbon Accumulation rate, 4alpha,23,24-Trimethyl-5alpha-cholest-22E-en-3beta-ol per year 24-Methylcholest-5-en-3beta-ol per unit sediment mass 24-Methylcholest-5-en-3beta-ol, per unit mass total organic carbon Accumulation rate, 24-Methylcholest-5-en-3beta-ol per year Gravity corer MSM45 Maria S. Merian |
spellingShingle |
8.2 ka event Biomarker brassica sterol campesterol dionsterol HBI III Holocene IP25 Labrador Shelf primary production Sea ice Terrigenious input DEPTH, sediment/rock Accumulation rate per year 2,6,10,14-Tetramethyl-7-3-methylpent-4-enylpentadecane per unit sediment mass 2,6,10,14-Tetramethyl-7-3-methylpent-4-enylpentadecane, per unit mass total organic carbon Accumulation rate, 2,6,10,14-Tetramethyl-7-3-methylpent-4-enylpentadecane per year Highly branched isoprenoids Z, triunsatured per unit sediment mass Highly branched isoprenoids Z, triunsatured, per unit mass total organic carbon Accumulation rate, highly branched isoprenoids Z, triunsatured per year 24-Methylcholesta-5,22E-dien-3beta-ol per unit sediment mass 24-Methylcholesta-5,22E-dien-3beta-ol, per unit mass total organic carbon Accumulation rate, 24-Methylcholesta-5,22E-dien-3beta-ol per year 4alpha,23,24-Trimethyl-5alpha-cholest-22E-en-3beta-ol per unit sediment mass 4alpha,23,24-Trimethyl-5alpha-cholest-22E-en-3beta-ol, per unit mass total organic carbon Accumulation rate, 4alpha,23,24-Trimethyl-5alpha-cholest-22E-en-3beta-ol per year 24-Methylcholest-5-en-3beta-ol per unit sediment mass 24-Methylcholest-5-en-3beta-ol, per unit mass total organic carbon Accumulation rate, 24-Methylcholest-5-en-3beta-ol per year Gravity corer MSM45 Maria S. Merian Kolling, Henriette Marie Schneider, Ralph R Stein, Ruediger Fahl, Kirsten Biomarker concentrations in gravity core MSM45_19-2 ... |
topic_facet |
8.2 ka event Biomarker brassica sterol campesterol dionsterol HBI III Holocene IP25 Labrador Shelf primary production Sea ice Terrigenious input DEPTH, sediment/rock Accumulation rate per year 2,6,10,14-Tetramethyl-7-3-methylpent-4-enylpentadecane per unit sediment mass 2,6,10,14-Tetramethyl-7-3-methylpent-4-enylpentadecane, per unit mass total organic carbon Accumulation rate, 2,6,10,14-Tetramethyl-7-3-methylpent-4-enylpentadecane per year Highly branched isoprenoids Z, triunsatured per unit sediment mass Highly branched isoprenoids Z, triunsatured, per unit mass total organic carbon Accumulation rate, highly branched isoprenoids Z, triunsatured per year 24-Methylcholesta-5,22E-dien-3beta-ol per unit sediment mass 24-Methylcholesta-5,22E-dien-3beta-ol, per unit mass total organic carbon Accumulation rate, 24-Methylcholesta-5,22E-dien-3beta-ol per year 4alpha,23,24-Trimethyl-5alpha-cholest-22E-en-3beta-ol per unit sediment mass 4alpha,23,24-Trimethyl-5alpha-cholest-22E-en-3beta-ol, per unit mass total organic carbon Accumulation rate, 4alpha,23,24-Trimethyl-5alpha-cholest-22E-en-3beta-ol per year 24-Methylcholest-5-en-3beta-ol per unit sediment mass 24-Methylcholest-5-en-3beta-ol, per unit mass total organic carbon Accumulation rate, 24-Methylcholest-5-en-3beta-ol per year Gravity corer MSM45 Maria S. Merian |
description |
Sea ice and paleoenvironmental conditions were reconstructed based on gravity core MSM45_19-2 from the northern Labrador Shelf. Gravity core MSM45_19-2 was obtained during R/V Maria S. Merian expedition MSM45 (58°45.68'N, 61°56.25'W, water depth: 202 m) in 2015 (Schneider et al., 2016).For paleoenvironmental reconstructions of the last 9,000 years BP, biomarkers representing sea ice algae productivity (IP25), open-water phytoplankton productivity (brassicasterol, dinosterol and HBI III (Z)) and terrigenous input (campesterol) where analyzed. Aim of this study was to investigate (i) the role sea ice played before and during the final demise of the Laurentide Ice Sheet between 8.7 and 8.2 kyr BP, and (ii) the effects of meltwater events on remaining sea-ice cover and primary productivity.Concentrations of specific biomarkers were analyzed. 4-5 g of each sediment sample were extracted by sonication (3 x 15 min) using dichloromethane:methanol (2:1 v/v; 30 ml) as solvent. Prior to biomarker extraction two ... |
format |
Dataset |
author |
Kolling, Henriette Marie Schneider, Ralph R Stein, Ruediger Fahl, Kirsten |
author_facet |
Kolling, Henriette Marie Schneider, Ralph R Stein, Ruediger Fahl, Kirsten |
author_sort |
Kolling, Henriette Marie |
title |
Biomarker concentrations in gravity core MSM45_19-2 ... |
title_short |
Biomarker concentrations in gravity core MSM45_19-2 ... |
title_full |
Biomarker concentrations in gravity core MSM45_19-2 ... |
title_fullStr |
Biomarker concentrations in gravity core MSM45_19-2 ... |
title_full_unstemmed |
Biomarker concentrations in gravity core MSM45_19-2 ... |
title_sort |
biomarker concentrations in gravity core msm45_19-2 ... |
publisher |
PANGAEA |
publishDate |
2022 |
url |
https://dx.doi.org/10.1594/pangaea.949065 https://doi.pangaea.de/10.1594/PANGAEA.949065 |
long_lat |
ENVELOPE(-58.000,-58.000,56.000,56.000) |
geographic |
Labrador Shelf |
geographic_facet |
Labrador Shelf |
genre |
ice algae Ice Sheet Sea ice |
genre_facet |
ice algae Ice Sheet Sea ice |
op_relation |
https://dx.doi.org/10.1029/2022pa004578 https://dx.doi.org/10.2312/cr_msm45 https://dx.doi.org/10.1016/j.epsl.2015.09.020 https://dx.doi.org/10.1016/j.epsl.2012.07.009 https://dx.doi.org/10.1016/j.orggeochem.2015.12.007 |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.1594/pangaea.94906510.1029/2022pa00457810.2312/cr_msm4510.1016/j.epsl.2015.09.02010.1016/j.epsl.2012.07.00910.1016/j.orggeochem.2015.12.007 |
_version_ |
1795032795964243968 |