Down-core geochemical data from Disko 2 lake sediment core (West Greenland) collected in April 2013 ...

Lake sediment samples were taken in April 2013 from the ice by drilling through lake ice and recovering an undisturbed core using a HON-Kajak sediment corer. Samples were analysed for pigments (University of Nottingham), carbon isotopes and C/N ratios (BGS, Keyworth), lipid biomarkers (Newcastle Uni...

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Bibliographic Details
Main Authors: Stevenson, Mark A, McGowan, Suzanne, Pearson, Emma J, Swann, George E A, Leng, Melanie J, Jones, Vivienne J, Bailey, Joseph J, Huang, Xianyu, Whiteford, Erika
Format: Dataset
Language:English
Published: PANGAEA 2021
Subjects:
Age
Online Access:https://dx.doi.org/10.1594/pangaea.927276
https://doi.pangaea.de/10.1594/PANGAEA.927276
id ftdatacite:10.1594/pangaea.927276
record_format openpolar
spelling ftdatacite:10.1594/pangaea.927276 2024-06-09T07:44:32+00:00 Down-core geochemical data from Disko 2 lake sediment core (West Greenland) collected in April 2013 ... Stevenson, Mark A McGowan, Suzanne Pearson, Emma J Swann, George E A Leng, Melanie J Jones, Vivienne J Bailey, Joseph J Huang, Xianyu Whiteford, Erika 2021 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.927276 https://doi.pangaea.de/10.1594/PANGAEA.927276 en eng PANGAEA https://dx.doi.org/10.5194/bg-18-2465-2021 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Arctic carbon isotope analysis Disko Island Greenland Lake sediment Organic Geochemistry DEPTH, sediment/rock Depth, top/min Depth, bottom/max Dry mass per area Lead-210 Lead-210, error Lead-210, supported Lead-210, supported, error Lead-210, unsupported Lead-210, unsupported, error Lead-210, unsupported, cumulative Lead-210, unsupported, cumulative, error Caesium-137 Caesium-137, error Americium-241 Americium-241, error Age Age, standard error Accumulation rate per year Sedimentation rate per year Sedimentation rate, error Accumulation rate, dry mass Accumulation rate, carbon, per year Carbon, organic, total δ13C, organic carbon Carbon/Nitrogen ratio beta-Carotene, per unit mass total organic carbon Carbon Preference Index 2, n-Alkanes C23+C25+C27 +C25+C27+C29/2*C24+C26+C28 Terrigenous/aquatic ratio Index of waxy n-alkanes to total hydrocarbons C27+C29+C31/C23+C25+C29+C31 n-alkane C27/sum n-alkanes Carbon Preference Index, n-Alkanoic acids n-Alkanoic acid C30/sum n-Alkanoic acid ratio n-Alkanol C16/sum n-Alkanols n-Alkanol C24/sum n-Alkanols 24-Methylcholesta-5,22E-dien-3beta-ol/sum sterols n-Alkanoic acid C280, δ13C HON-Kajak sediment corer Calculated Reverse Coaxial Radiation Detector, ORTEC, HPGe GWL CRS model Constant Rate of Supply Element analyser CHN ECS4010, Costech coupled to a VG Triple Trap and a VG Optima dual-inlet mass spectrometer MS High performance liquid chromatography HPLC, Agilent 1200 Calculation according to Marzi et al. 1993 Dataset dataset 2021 ftdatacite https://doi.org/10.1594/pangaea.92727610.5194/bg-18-2465-2021 2024-05-13T13:18:55Z Lake sediment samples were taken in April 2013 from the ice by drilling through lake ice and recovering an undisturbed core using a HON-Kajak sediment corer. Samples were analysed for pigments (University of Nottingham), carbon isotopes and C/N ratios (BGS, Keyworth), lipid biomarkers (Newcastle University) and compound-specific carbon isotopes (CUG, Wuhan). The purpose of the analyses was to develop an environmental reconstruction of carbon cycling for an upland lake (named Disko 2) to encompass the Little Ice Age to recent warming climate periods. Analyses were completed as part of Mark A. Stevenson's PhD research while based at the University of Nottingham, UK (Stevenson, 2017, http://eprints.nottingham.ac.uk/46579).²¹⁰Pb, ²²⁶Ra, ¹³⁷Cs and ²⁴¹Am concentrations were measured by direct gamma assay in the Environmental Radiometric Facility at University College London (Dr Handong Yang), using an ORTEC HPGe GWL series well-type coaxial low background intrinsic germanium detector. Radiometric dating techniques ... : ± errors derived from counting statisitcs. The absolute efficiencies of the detector were determined using calibrated sources and sediment samples of known activity. See Appleby et al, 1986 (doi:10.1007/0-306-47669-X), Appleby et al, 1992 (doi:10.1016/0168-583X(92)95328-O) and Appleby, 2001 (doi:10.1007/BF00026640). ... Dataset Arctic Greenland DataCite Metadata Store (German National Library of Science and Technology) Appleby ENVELOPE(59.611,59.611,-67.408,-67.408) Arctic Greenland
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Arctic
carbon isotope analysis
Disko Island
Greenland
Lake sediment
Organic Geochemistry
DEPTH, sediment/rock
Depth, top/min
Depth, bottom/max
Dry mass per area
Lead-210
Lead-210, error
Lead-210, supported
Lead-210, supported, error
Lead-210, unsupported
Lead-210, unsupported, error
Lead-210, unsupported, cumulative
Lead-210, unsupported, cumulative, error
Caesium-137
Caesium-137, error
Americium-241
Americium-241, error
Age
Age, standard error
Accumulation rate per year
Sedimentation rate per year
Sedimentation rate, error
Accumulation rate, dry mass
Accumulation rate, carbon, per year
Carbon, organic, total
δ13C, organic carbon
Carbon/Nitrogen ratio
beta-Carotene, per unit mass total organic carbon
Carbon Preference Index 2, n-Alkanes C23+C25+C27 +C25+C27+C29/2*C24+C26+C28
Terrigenous/aquatic ratio
Index of waxy n-alkanes to total hydrocarbons C27+C29+C31/C23+C25+C29+C31
n-alkane C27/sum n-alkanes
Carbon Preference Index, n-Alkanoic acids
n-Alkanoic acid C30/sum n-Alkanoic acid ratio
n-Alkanol C16/sum n-Alkanols
n-Alkanol C24/sum n-Alkanols
24-Methylcholesta-5,22E-dien-3beta-ol/sum sterols
n-Alkanoic acid C280, δ13C
HON-Kajak sediment corer
Calculated
Reverse Coaxial Radiation Detector, ORTEC, HPGe GWL
CRS model Constant Rate of Supply
Element analyser CHN ECS4010, Costech coupled to a VG Triple Trap and a VG Optima dual-inlet mass spectrometer MS
High performance liquid chromatography HPLC, Agilent 1200
Calculation according to Marzi et al. 1993
spellingShingle Arctic
carbon isotope analysis
Disko Island
Greenland
Lake sediment
Organic Geochemistry
DEPTH, sediment/rock
Depth, top/min
Depth, bottom/max
Dry mass per area
Lead-210
Lead-210, error
Lead-210, supported
Lead-210, supported, error
Lead-210, unsupported
Lead-210, unsupported, error
Lead-210, unsupported, cumulative
Lead-210, unsupported, cumulative, error
Caesium-137
Caesium-137, error
Americium-241
Americium-241, error
Age
Age, standard error
Accumulation rate per year
Sedimentation rate per year
Sedimentation rate, error
Accumulation rate, dry mass
Accumulation rate, carbon, per year
Carbon, organic, total
δ13C, organic carbon
Carbon/Nitrogen ratio
beta-Carotene, per unit mass total organic carbon
Carbon Preference Index 2, n-Alkanes C23+C25+C27 +C25+C27+C29/2*C24+C26+C28
Terrigenous/aquatic ratio
Index of waxy n-alkanes to total hydrocarbons C27+C29+C31/C23+C25+C29+C31
n-alkane C27/sum n-alkanes
Carbon Preference Index, n-Alkanoic acids
n-Alkanoic acid C30/sum n-Alkanoic acid ratio
n-Alkanol C16/sum n-Alkanols
n-Alkanol C24/sum n-Alkanols
24-Methylcholesta-5,22E-dien-3beta-ol/sum sterols
n-Alkanoic acid C280, δ13C
HON-Kajak sediment corer
Calculated
Reverse Coaxial Radiation Detector, ORTEC, HPGe GWL
CRS model Constant Rate of Supply
Element analyser CHN ECS4010, Costech coupled to a VG Triple Trap and a VG Optima dual-inlet mass spectrometer MS
High performance liquid chromatography HPLC, Agilent 1200
Calculation according to Marzi et al. 1993
Stevenson, Mark A
McGowan, Suzanne
Pearson, Emma J
Swann, George E A
Leng, Melanie J
Jones, Vivienne J
Bailey, Joseph J
Huang, Xianyu
Whiteford, Erika
Down-core geochemical data from Disko 2 lake sediment core (West Greenland) collected in April 2013 ...
topic_facet Arctic
carbon isotope analysis
Disko Island
Greenland
Lake sediment
Organic Geochemistry
DEPTH, sediment/rock
Depth, top/min
Depth, bottom/max
Dry mass per area
Lead-210
Lead-210, error
Lead-210, supported
Lead-210, supported, error
Lead-210, unsupported
Lead-210, unsupported, error
Lead-210, unsupported, cumulative
Lead-210, unsupported, cumulative, error
Caesium-137
Caesium-137, error
Americium-241
Americium-241, error
Age
Age, standard error
Accumulation rate per year
Sedimentation rate per year
Sedimentation rate, error
Accumulation rate, dry mass
Accumulation rate, carbon, per year
Carbon, organic, total
δ13C, organic carbon
Carbon/Nitrogen ratio
beta-Carotene, per unit mass total organic carbon
Carbon Preference Index 2, n-Alkanes C23+C25+C27 +C25+C27+C29/2*C24+C26+C28
Terrigenous/aquatic ratio
Index of waxy n-alkanes to total hydrocarbons C27+C29+C31/C23+C25+C29+C31
n-alkane C27/sum n-alkanes
Carbon Preference Index, n-Alkanoic acids
n-Alkanoic acid C30/sum n-Alkanoic acid ratio
n-Alkanol C16/sum n-Alkanols
n-Alkanol C24/sum n-Alkanols
24-Methylcholesta-5,22E-dien-3beta-ol/sum sterols
n-Alkanoic acid C280, δ13C
HON-Kajak sediment corer
Calculated
Reverse Coaxial Radiation Detector, ORTEC, HPGe GWL
CRS model Constant Rate of Supply
Element analyser CHN ECS4010, Costech coupled to a VG Triple Trap and a VG Optima dual-inlet mass spectrometer MS
High performance liquid chromatography HPLC, Agilent 1200
Calculation according to Marzi et al. 1993
description Lake sediment samples were taken in April 2013 from the ice by drilling through lake ice and recovering an undisturbed core using a HON-Kajak sediment corer. Samples were analysed for pigments (University of Nottingham), carbon isotopes and C/N ratios (BGS, Keyworth), lipid biomarkers (Newcastle University) and compound-specific carbon isotopes (CUG, Wuhan). The purpose of the analyses was to develop an environmental reconstruction of carbon cycling for an upland lake (named Disko 2) to encompass the Little Ice Age to recent warming climate periods. Analyses were completed as part of Mark A. Stevenson's PhD research while based at the University of Nottingham, UK (Stevenson, 2017, http://eprints.nottingham.ac.uk/46579).²¹⁰Pb, ²²⁶Ra, ¹³⁷Cs and ²⁴¹Am concentrations were measured by direct gamma assay in the Environmental Radiometric Facility at University College London (Dr Handong Yang), using an ORTEC HPGe GWL series well-type coaxial low background intrinsic germanium detector. Radiometric dating techniques ... : ± errors derived from counting statisitcs. The absolute efficiencies of the detector were determined using calibrated sources and sediment samples of known activity. See Appleby et al, 1986 (doi:10.1007/0-306-47669-X), Appleby et al, 1992 (doi:10.1016/0168-583X(92)95328-O) and Appleby, 2001 (doi:10.1007/BF00026640). ...
format Dataset
author Stevenson, Mark A
McGowan, Suzanne
Pearson, Emma J
Swann, George E A
Leng, Melanie J
Jones, Vivienne J
Bailey, Joseph J
Huang, Xianyu
Whiteford, Erika
author_facet Stevenson, Mark A
McGowan, Suzanne
Pearson, Emma J
Swann, George E A
Leng, Melanie J
Jones, Vivienne J
Bailey, Joseph J
Huang, Xianyu
Whiteford, Erika
author_sort Stevenson, Mark A
title Down-core geochemical data from Disko 2 lake sediment core (West Greenland) collected in April 2013 ...
title_short Down-core geochemical data from Disko 2 lake sediment core (West Greenland) collected in April 2013 ...
title_full Down-core geochemical data from Disko 2 lake sediment core (West Greenland) collected in April 2013 ...
title_fullStr Down-core geochemical data from Disko 2 lake sediment core (West Greenland) collected in April 2013 ...
title_full_unstemmed Down-core geochemical data from Disko 2 lake sediment core (West Greenland) collected in April 2013 ...
title_sort down-core geochemical data from disko 2 lake sediment core (west greenland) collected in april 2013 ...
publisher PANGAEA
publishDate 2021
url https://dx.doi.org/10.1594/pangaea.927276
https://doi.pangaea.de/10.1594/PANGAEA.927276
long_lat ENVELOPE(59.611,59.611,-67.408,-67.408)
geographic Appleby
Arctic
Greenland
geographic_facet Appleby
Arctic
Greenland
genre Arctic
Greenland
genre_facet Arctic
Greenland
op_relation https://dx.doi.org/10.5194/bg-18-2465-2021
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.92727610.5194/bg-18-2465-2021
_version_ 1801373260006293504