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Geochemical data (XRF-scanner) for core LC7 sediment record from Blaso, a large, epishelf lake in NW Greenland collected July-August 2017

The dataset comprises multi-proxy analyses of sediment core, LC7, extracted from Blaso, a large epishelf lake on the margin of 79 degrees N Ice Shelf, NW Greenland in July-August 2017. The data are used to constrain ice shelf dynamics over the last ~8500 calibrated years before present (cal. years B.P., where present is A.D. 1950).



A 2 m-long sediment core was recovered with a UWITEC KOL 'Kolbenlot' percussion piston corer to a total sediment depth of 3.74m.



Core LC7: 87 m water depth; 79.589 degrees N, 22.494 degrees E.



Geochemical data for the LC7 sediment records consists of XRF-scanner data.





This project was funded by the Natural Environment Research Council (NERC) through Standard Grant NE/N011228/1. We thank the Alfred Wegner Institute, and particularly Angelika Humbert and Hicham Rafiq, for their significant logistic support through the iGRIFF project. Additional support was provided from Station Nord (Jorgen Skafte), Nordland Air, Air Greenland and the Joint Arctic Command. Naalakkersuisut, Government of Greenland, provided Scientific Survey (VU-00121) and Export (046/2017) licences for this work.

Simple

Date (Creation)
2022-09-14
Date (Revision)
2022-09-14
Date (Publication)
2022-09-14
Date (released)
2022-09-14
Edition

1.0

Unique resource identifier
https://doi.org/10.5285/71c64bf8-671e-4f22-b4e9-b67b76dc35c8
Codespace

doi

Unique resource identifier
GB/NERC/BAS/PDC/01666
Codespace

https://data.bas.ac.uk/

Unique resource identifier
NE/N011228/1
Codespace

award

Other citation details

Please cite this item as: Smith, J., Callard, L., Sánchez Montes, M., McClymont, E., Lloyd, J., Ehrmann, W., Roberts, D., Bentley, M., Jamieson, S., Lane, T., & Darvill, C. (2022). Geochemical data (XRF-scanner) for core LC7 sediment record from Blaso, a large, epishelf lake in NW Greenland collected July-August 2017 (Version 1.0) [Data set]. NERC EDS UK Polar Data Centre. https://doi.org/10.5285/71c64bf8-671e-4f22-b4e9-b67b76dc35c8

Credit

No credit.

Status
Completed
Point of contact
Organisation name Individual name Electronic mail address Role
British Antarctic Survey Smith, James A. Author
Newcastle University Callard, Louise Author
University of Colorado Boulder Sánchez Montes, Maria Luisa Author
Durham University McClymont, Erin L. Author
Durham University Lloyd, Jeremy M. Author
University of Leipzig Ehrmann, Werner Author
Durham University

Roberts, David

Author
Durham University Bentley, Michael J. Author
Durham University Jamieson, Stewart S. R. Author
Liverpool John Moores University Lane, Timothy P. Author
University of Manchester Darvill, Christopher M. Author
NERC EDS UK Polar Data Centre

PDCServiceDesk@bas.ac.uk

Point of contact
Maintenance and update frequency
As needed
Maintenance note
Completed
Global Change Master Directory (GCMD) Science Keywords
  • EARTH SCIENCE > Paleoclimate > Ocean/Lake Records > Sediments
Theme
  • 79 degrees N

  • Greenland

  • Holocene

  • epishelf lake

  • ice shelf history

  • palaeolimnology

Place
  • Blaso, NW Greenland Greenland

GEMET - INSPIRE themes, version 1.0

  • Geology
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no limitations to public access
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no limitations
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Open Government Licence v3.0
Use constraints
Other restrictions
Other constraints

Data released under Open Government Licence V3.0:

Use constraints
Other restrictions
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No restrictions apply.

Unique resource identifier
url
Codespace

url

Association Type
Cross reference
Unique resource identifier
url
Codespace

url

Association Type
Cross reference
Unique resource identifier
url
Codespace

url

Association Type
Cross reference
Unique resource identifier
url
Codespace

url

Association Type
Cross reference
Unique resource identifier
url
Codespace

url

Association Type
Cross reference
Spatial representation type
Text, table
Language
English
Character set
UTF8
Topic category
  • Geoscientific information
N
S
E
W
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Begin date
2017-07-20
End date
2017-08-16
Supplemental Information

It is recommended that careful attention be paid to the contents of any data, and that the author be contacted with any questions regarding appropriate use. If you find any errors or omissions, please report them to polardatacentre@bas.ac.uk.

Title

European Petroleum Survey Group (EPSG) Geodetic Parameter Registry

Date (Publication)
2008-11-12
Cited responsible party
Organisation name Individual name Electronic mail address Role

European Petroleum Survey Group

EPSGadministrator@iogp.org

Publisher
Unique resource identifier
urn:ogc:def:crs:EPSG::3031
Version

6.18.3

Distributor

Distributor contact
Organisation name Individual name Electronic mail address Role
NERC EDS UK Polar Data Centre

PDCServiceDesk@bas.ac.uk

Distributor
Units of distribution

bytes

Transfer size
250880
OnLine resource
Protocol Linkage Name

WWW:LINK-1.0-http--link

https://ramadda.data.bas.ac.uk/repository/entry/show?entryid=71c64bf8-671e-4f22-b4e9-b67b76dc35c8

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Dataset
Statement

Methodology:

A 2 m-long sediment core was recovered with a UWITEC KOL 'Kolbenlot' percussion piston corer to a total sediment depth of 3.74 m (LC7) in Blaso (LC7: 79.589 degrees N, 22.494 degrees E, 87m).





Prior to analysis sediment samples were treated with 20 percent hydrogen peroxide to digest the organic material. Once the organic material has been digested the sample was centrifuged and then 20 ml distilled water plus 2 ml sodium hexametaphosphate was added to defloculate the sample. High-resolution elemental abundances were measured on the split core using a GEOTEK X-ray Fluorescence (MSCL-XRF) at 1 mm resolution. We use elemental ratios Ti/Ca as a proxy for terrigenous flux, while Mn/Fe and Br concentrations provides semi-quantitative information about lake oxygenation (Naeher et al., 2013) and marine organic carbon content (Ziegler et al., 2008) respectively. Ti contents in marine sediments is directly linked to terrigenous (siliciclastic) sediment supply delivered by fluvial and/or aeolian transport processes (Arz et al., 1999; Nace et al., 2014), while Ca concentrations reflect changes in the production of calcium carbonate (CaCO3) by marine plankton (Bahr et al., 2005). High Ti/Ca ratios are indicative of an increased terrigenous flux. The behaviour of Fe and Mn is strongly dependent on processes of oxidation and reduction. Reducing conditions are the result of O2 consumption during organic matter (OM) remineralisation, which releases Fe and Mn. Because Fe oxidises faster than Mn, high Mn accumulation and thus high(low) Mn/Fe ratios reflect oxic (anoxic) conditions. Bromine (Br) is used as a proxy for marine organic carbon, since bromine is found at higher concentrations in marine, compared to terrestrial, organic matter (Ziegler et al., 2008; Seki et al., 2019).

Data collection:

UWITEC KOL 'Kolbenlot' percussion piston corer



GEOTEK X-ray Fluorescence (MSCL-XRF)

Metadata

File identifier
71c64bf8-671e-4f22-b4e9-b67b76dc35c8 XML
Metadata language
English
Character set
UTF8
Hierarchy level
Dataset
Hierarchy level name

dataset

Date stamp
2022-09-14
Metadata standard name

ISO 19115 Geographic Information - Metadata

Metadata standard version

ISO 19115:2003(E)

Metadata author
Organisation name Individual name Electronic mail address Role
NERC EDS UK Polar Data Centre

polardatacentre@bas.ac.uk

Point of contact
 
 

Overviews

Spatial extent

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Keywords

79 degrees N Greenland Holocene epishelf lake ice shelf history palaeolimnology
GEMET - INSPIRE themes, version 1.0

Geology
Global Change Master Directory (GCMD) Science Keywords

EARTH SCIENCE > Paleoclimate > Ocean/Lake Records > Sediments


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