Opal (Zn/Si) ratios as a nearshore geochemical proxy in coastal Antarctica
Author Posting. © American Geophysical Union, 2008. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Paleoceanography 23 (2008): PA2218, doi:10.1029/2007PA001576. During the last 50 years, the An...
Published in: | Paleoceanography |
---|---|
Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
American Geophysical Union
2008
|
Subjects: | |
Online Access: | https://hdl.handle.net/1912/4813 |
id |
ftwhoas:oai:darchive.mblwhoilibrary.org:1912/4813 |
---|---|
record_format |
openpolar |
spelling |
ftwhoas:oai:darchive.mblwhoilibrary.org:1912/4813 2023-05-15T13:53:14+02:00 Opal (Zn/Si) ratios as a nearshore geochemical proxy in coastal Antarctica Hendry, Katharine R. Rickaby, Rosalind E. M. 2008-06-18 application/pdf text/plain image/tiff https://hdl.handle.net/1912/4813 en_US eng American Geophysical Union https://doi.org/10.1029/2007PA001576 Paleoceanography 23 (2008): PA2218 https://hdl.handle.net/1912/4813 doi:10.1029/2007PA001576 Paleoceanography 23 (2008): PA2218 doi:10.1029/2007PA001576 Opal Zinc Salinity Article 2008 ftwhoas https://doi.org/10.1029/2007PA001576 2022-05-28T22:58:27Z Author Posting. © American Geophysical Union, 2008. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Paleoceanography 23 (2008): PA2218, doi:10.1029/2007PA001576. During the last 50 years, the Antarctic Peninsula has experienced rapid warming with associated retreat of 87% of marine and tidewater glacier fronts. Accelerated glacial retreat and iceberg calving may have a significant impact on the freshwater and nutrient supply to the phytoplankton communities of the highly productive coastal regions. However, commonly used biogenic carbonate proxies for nutrient and salinity conditions are not preserved in sediments from coastal Antarctica. Here we describe a method for the measurement of zinc to silicon ratios in diatom opal, (Zn/Si)opal, which is a potential archive in Antarctic marine sediments. A core top calibration from the West Antarctic Peninsula shows (Zn/Si)opal is a proxy for mixed layer salinity. We present down-core (Zn/Si)opal paleosalinity records from two rapidly accumulating sites taken from nearshore environments off the West Antarctic Peninsula which show an increase in meltwater input in recent decades. Our records show that the recent melting in this region is unprecedented for over 120 years. The work was funded as part of NERC Antarctic Funding Initiative AFI4– 02. K.R.H. is funded by NERC grant NER/S/A/2004/12390. Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Antarctica Iceberg* Tidewater Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server) Antarctic The Antarctic Antarctic Peninsula Ner ENVELOPE(6.622,6.622,62.612,62.612) Paleoceanography 23 2 n/a n/a |
institution |
Open Polar |
collection |
Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server) |
op_collection_id |
ftwhoas |
language |
English |
topic |
Opal Zinc Salinity |
spellingShingle |
Opal Zinc Salinity Hendry, Katharine R. Rickaby, Rosalind E. M. Opal (Zn/Si) ratios as a nearshore geochemical proxy in coastal Antarctica |
topic_facet |
Opal Zinc Salinity |
description |
Author Posting. © American Geophysical Union, 2008. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Paleoceanography 23 (2008): PA2218, doi:10.1029/2007PA001576. During the last 50 years, the Antarctic Peninsula has experienced rapid warming with associated retreat of 87% of marine and tidewater glacier fronts. Accelerated glacial retreat and iceberg calving may have a significant impact on the freshwater and nutrient supply to the phytoplankton communities of the highly productive coastal regions. However, commonly used biogenic carbonate proxies for nutrient and salinity conditions are not preserved in sediments from coastal Antarctica. Here we describe a method for the measurement of zinc to silicon ratios in diatom opal, (Zn/Si)opal, which is a potential archive in Antarctic marine sediments. A core top calibration from the West Antarctic Peninsula shows (Zn/Si)opal is a proxy for mixed layer salinity. We present down-core (Zn/Si)opal paleosalinity records from two rapidly accumulating sites taken from nearshore environments off the West Antarctic Peninsula which show an increase in meltwater input in recent decades. Our records show that the recent melting in this region is unprecedented for over 120 years. The work was funded as part of NERC Antarctic Funding Initiative AFI4– 02. K.R.H. is funded by NERC grant NER/S/A/2004/12390. |
format |
Article in Journal/Newspaper |
author |
Hendry, Katharine R. Rickaby, Rosalind E. M. |
author_facet |
Hendry, Katharine R. Rickaby, Rosalind E. M. |
author_sort |
Hendry, Katharine R. |
title |
Opal (Zn/Si) ratios as a nearshore geochemical proxy in coastal Antarctica |
title_short |
Opal (Zn/Si) ratios as a nearshore geochemical proxy in coastal Antarctica |
title_full |
Opal (Zn/Si) ratios as a nearshore geochemical proxy in coastal Antarctica |
title_fullStr |
Opal (Zn/Si) ratios as a nearshore geochemical proxy in coastal Antarctica |
title_full_unstemmed |
Opal (Zn/Si) ratios as a nearshore geochemical proxy in coastal Antarctica |
title_sort |
opal (zn/si) ratios as a nearshore geochemical proxy in coastal antarctica |
publisher |
American Geophysical Union |
publishDate |
2008 |
url |
https://hdl.handle.net/1912/4813 |
long_lat |
ENVELOPE(6.622,6.622,62.612,62.612) |
geographic |
Antarctic The Antarctic Antarctic Peninsula Ner |
geographic_facet |
Antarctic The Antarctic Antarctic Peninsula Ner |
genre |
Antarc* Antarctic Antarctic Peninsula Antarctica Iceberg* Tidewater |
genre_facet |
Antarc* Antarctic Antarctic Peninsula Antarctica Iceberg* Tidewater |
op_source |
Paleoceanography 23 (2008): PA2218 doi:10.1029/2007PA001576 |
op_relation |
https://doi.org/10.1029/2007PA001576 Paleoceanography 23 (2008): PA2218 https://hdl.handle.net/1912/4813 doi:10.1029/2007PA001576 |
op_doi |
https://doi.org/10.1029/2007PA001576 |
container_title |
Paleoceanography |
container_volume |
23 |
container_issue |
2 |
container_start_page |
n/a |
op_container_end_page |
n/a |
_version_ |
1766258235483881472 |