Isotopic composition and physical oceanography of water profiles from Greenland ...

Isotopic composition of strontium and oxygen and strontium concentrations from 4 hydrographic sites in Scoresby Sund Fjord and 6 rivers draining the adjacent Jameson Land have been investigated. Schuchert Flod, the major river on Jameson Land, erodes a large celestite (SrSO4) deposit. Dissolved Sr i...

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Main Authors: Israelson, C, Buchardt, B
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2009
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.729429
https://doi.pangaea.de/10.1594/PANGAEA.729429
id ftdatacite:10.1594/pangaea.729429
record_format openpolar
spelling ftdatacite:10.1594/pangaea.729429 2024-09-15T18:04:20+00:00 Isotopic composition and physical oceanography of water profiles from Greenland ... Israelson, C Buchardt, B 2009 application/zip https://dx.doi.org/10.1594/pangaea.729429 https://doi.pangaea.de/10.1594/PANGAEA.729429 en eng PANGAEA https://dx.doi.org/10.1016/s0031-0182(99)00068-1 https://dx.doi.org/10.1016/0031-0182(94)90351-4 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Giant box corer Bio-Rosette ARK-VII/1 ARK-VII/3b Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Quaternary Environment of the Eurasian North QUEEN article Collection Supplementary Publication Series of Datasets 2009 ftdatacite https://doi.org/10.1594/pangaea.72942910.1016/s0031-0182(99)00068-110.1016/0031-0182(94)90351-4 2024-07-03T13:10:33Z Isotopic composition of strontium and oxygen and strontium concentrations from 4 hydrographic sites in Scoresby Sund Fjord and 6 rivers draining the adjacent Jameson Land have been investigated. Schuchert Flod, the major river on Jameson Land, erodes a large celestite (SrSO4) deposit. Dissolved Sr in Schuchert Flod has 87Sr/86Sr = 0.7137 and is responsible for most of the continental Sr flux to the fjord. The Sr isotope data have been used to construct a mixing model for the surface water in Scoresby Sund Fjord. Salinity (S) and Sr concentrations (CSr) of brackish water from the fjord show conservative mixing between river water and seawater. Results of the 87Sr/86Sr–salinity mixing model of seawater and fresh water were used to interpret the isotopic composition of Sr (87Sr/86Sr) and oxygen (d18Oc) of recent and interglacial (Eemian ~120 ka) shallow-water bivalve shells from the coast of Jameson Land. Because of the high CSr in some of the rivers draining Jameson Land, a correlation exists between 87Sr/86Sr ... : Supplement to: Israelson, C; Buchardt, B (1999): Strontium and oxygen isotope composition of East Greenland rivers and surface waters: Implication for palaeoenvironmental interpretation. Palaeogeography, Palaeoclimatology, Palaeoecology, 153(1-4), 93-104 ... Article in Journal/Newspaper East Greenland Greenland Scoresby Sund DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Giant box corer
Bio-Rosette
ARK-VII/1
ARK-VII/3b
Polarstern
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
Quaternary Environment of the Eurasian North QUEEN
spellingShingle Giant box corer
Bio-Rosette
ARK-VII/1
ARK-VII/3b
Polarstern
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
Quaternary Environment of the Eurasian North QUEEN
Israelson, C
Buchardt, B
Isotopic composition and physical oceanography of water profiles from Greenland ...
topic_facet Giant box corer
Bio-Rosette
ARK-VII/1
ARK-VII/3b
Polarstern
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
Quaternary Environment of the Eurasian North QUEEN
description Isotopic composition of strontium and oxygen and strontium concentrations from 4 hydrographic sites in Scoresby Sund Fjord and 6 rivers draining the adjacent Jameson Land have been investigated. Schuchert Flod, the major river on Jameson Land, erodes a large celestite (SrSO4) deposit. Dissolved Sr in Schuchert Flod has 87Sr/86Sr = 0.7137 and is responsible for most of the continental Sr flux to the fjord. The Sr isotope data have been used to construct a mixing model for the surface water in Scoresby Sund Fjord. Salinity (S) and Sr concentrations (CSr) of brackish water from the fjord show conservative mixing between river water and seawater. Results of the 87Sr/86Sr–salinity mixing model of seawater and fresh water were used to interpret the isotopic composition of Sr (87Sr/86Sr) and oxygen (d18Oc) of recent and interglacial (Eemian ~120 ka) shallow-water bivalve shells from the coast of Jameson Land. Because of the high CSr in some of the rivers draining Jameson Land, a correlation exists between 87Sr/86Sr ... : Supplement to: Israelson, C; Buchardt, B (1999): Strontium and oxygen isotope composition of East Greenland rivers and surface waters: Implication for palaeoenvironmental interpretation. Palaeogeography, Palaeoclimatology, Palaeoecology, 153(1-4), 93-104 ...
format Article in Journal/Newspaper
author Israelson, C
Buchardt, B
author_facet Israelson, C
Buchardt, B
author_sort Israelson, C
title Isotopic composition and physical oceanography of water profiles from Greenland ...
title_short Isotopic composition and physical oceanography of water profiles from Greenland ...
title_full Isotopic composition and physical oceanography of water profiles from Greenland ...
title_fullStr Isotopic composition and physical oceanography of water profiles from Greenland ...
title_full_unstemmed Isotopic composition and physical oceanography of water profiles from Greenland ...
title_sort isotopic composition and physical oceanography of water profiles from greenland ...
publisher PANGAEA
publishDate 2009
url https://dx.doi.org/10.1594/pangaea.729429
https://doi.pangaea.de/10.1594/PANGAEA.729429
genre East Greenland
Greenland
Scoresby Sund
genre_facet East Greenland
Greenland
Scoresby Sund
op_relation https://dx.doi.org/10.1016/s0031-0182(99)00068-1
https://dx.doi.org/10.1016/0031-0182(94)90351-4
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.72942910.1016/s0031-0182(99)00068-110.1016/0031-0182(94)90351-4
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