Geochemistry of a coral from Bermuda ...
We present a 55-year-long record (1928-1982) of Sr/Ca in a Bermuda coral (Diploria strigosa), which we use to reconstruct local twentieth century climate features. The clearest climate signal emerges for the late-year Sr/Ca. Although the coral was collected in shallow water (12 m), the correlation w...
Main Authors: | , , |
---|---|
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
PANGAEA
2005
|
Subjects: | |
Online Access: | https://dx.doi.org/10.1594/pangaea.738188 https://doi.pangaea.de/10.1594/PANGAEA.738188 |
id |
ftdatacite:10.1594/pangaea.738188 |
---|---|
record_format |
openpolar |
spelling |
ftdatacite:10.1594/pangaea.738188 2024-03-31T07:54:13+00:00 Geochemistry of a coral from Bermuda ... Kuhnert, Henning Crüger, Traute Pätzold, Jürgen 2005 application/zip https://dx.doi.org/10.1594/pangaea.738188 https://doi.pangaea.de/10.1594/PANGAEA.738188 en eng PANGAEA https://dx.doi.org/10.1029/2004gc000786 Data access is restricted (moratorium, sensitive data, license constraints) Licensing unknown: Please contact principal investigator/authors to gain access and request licensing terms unknown CORCLIM Core wireline system Bermuda84 Bermuda Bio Station Center for Marine Environmental Sciences MARUM Supplementary Publication Series of Datasets article Collection 2005 ftdatacite https://doi.org/10.1594/pangaea.73818810.1029/2004gc000786 2024-03-04T13:35:39Z We present a 55-year-long record (1928-1982) of Sr/Ca in a Bermuda coral (Diploria strigosa), which we use to reconstruct local twentieth century climate features. The clearest climate signal emerges for the late-year Sr/Ca. Although the coral was collected in shallow water (12 m), the correlation with station data is highest for temperatures at 50 m depth (r = -0.70), suggesting that local temperatures at the collection site are not representative for the sea surface temperatures in the adjacent open ocean. The most striking feature of the coral record is the persistent and significant correlation (r = -0.50) with the North Atlantic Oscillation (NAO) index. Field correlations of fall Sr/Ca with the winter sea level pressure (SLP) show the typical spatial NAO pattern. The stable relationship with the NAO shows that Sr/Ca in Bermuda corals is a suitable tool for the reconstruction of North Atlantic climate variability. ... : Supplement to: Kuhnert, Henning; Crüger, Traute; Pätzold, Jürgen (2005): NAO signature in a Bermuda coral Sr/Ca record. Geochemistry, Geophysics, Geosystems, 6, Q04004 ... Article in Journal/Newspaper North Atlantic North Atlantic oscillation DataCite Metadata Store (German National Library of Science and Technology) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
CORCLIM Core wireline system Bermuda84 Bermuda Bio Station Center for Marine Environmental Sciences MARUM |
spellingShingle |
CORCLIM Core wireline system Bermuda84 Bermuda Bio Station Center for Marine Environmental Sciences MARUM Kuhnert, Henning Crüger, Traute Pätzold, Jürgen Geochemistry of a coral from Bermuda ... |
topic_facet |
CORCLIM Core wireline system Bermuda84 Bermuda Bio Station Center for Marine Environmental Sciences MARUM |
description |
We present a 55-year-long record (1928-1982) of Sr/Ca in a Bermuda coral (Diploria strigosa), which we use to reconstruct local twentieth century climate features. The clearest climate signal emerges for the late-year Sr/Ca. Although the coral was collected in shallow water (12 m), the correlation with station data is highest for temperatures at 50 m depth (r = -0.70), suggesting that local temperatures at the collection site are not representative for the sea surface temperatures in the adjacent open ocean. The most striking feature of the coral record is the persistent and significant correlation (r = -0.50) with the North Atlantic Oscillation (NAO) index. Field correlations of fall Sr/Ca with the winter sea level pressure (SLP) show the typical spatial NAO pattern. The stable relationship with the NAO shows that Sr/Ca in Bermuda corals is a suitable tool for the reconstruction of North Atlantic climate variability. ... : Supplement to: Kuhnert, Henning; Crüger, Traute; Pätzold, Jürgen (2005): NAO signature in a Bermuda coral Sr/Ca record. Geochemistry, Geophysics, Geosystems, 6, Q04004 ... |
format |
Article in Journal/Newspaper |
author |
Kuhnert, Henning Crüger, Traute Pätzold, Jürgen |
author_facet |
Kuhnert, Henning Crüger, Traute Pätzold, Jürgen |
author_sort |
Kuhnert, Henning |
title |
Geochemistry of a coral from Bermuda ... |
title_short |
Geochemistry of a coral from Bermuda ... |
title_full |
Geochemistry of a coral from Bermuda ... |
title_fullStr |
Geochemistry of a coral from Bermuda ... |
title_full_unstemmed |
Geochemistry of a coral from Bermuda ... |
title_sort |
geochemistry of a coral from bermuda ... |
publisher |
PANGAEA |
publishDate |
2005 |
url |
https://dx.doi.org/10.1594/pangaea.738188 https://doi.pangaea.de/10.1594/PANGAEA.738188 |
genre |
North Atlantic North Atlantic oscillation |
genre_facet |
North Atlantic North Atlantic oscillation |
op_relation |
https://dx.doi.org/10.1029/2004gc000786 |
op_rights |
Data access is restricted (moratorium, sensitive data, license constraints) Licensing unknown: Please contact principal investigator/authors to gain access and request licensing terms unknown |
op_doi |
https://doi.org/10.1594/pangaea.73818810.1029/2004gc000786 |
_version_ |
1795034917866831872 |