HIGH-RESOLUTION MG/CA RATIOS IN A CORALLINE RED ALGA AS A PROXY FOR BERING SEA TEMPERATURE VARIATIONS FROM 1902 TO 1967

被引:57
|
作者
Hetzinger, Steffen [1 ]
Halfar, Jochen [1 ]
Kronz, Andreas [2 ]
Steneck, Robert S. [3 ]
Adey, Walter [4 ]
Lebednik, Phillip A. [5 ]
Schoene, Bernd R. [6 ]
机构
[1] Univ Toronto, Dept Chem & Phys Sci, Mississauga, ON L5L 1C6, Canada
[2] Univ Gottingen, Geowissensch Zentrum, D-3400 Gottingen, Germany
[3] Univ Maine, Darling Marine Ctr, Walpole, ME 04573 USA
[4] Smithsonian Inst, Dept Bot, Washington, DC 20560 USA
[5] LFR Inc, Ecosyst Serv Grp, Emeryville, CA USA
[6] Johannes Gutenberg Univ Mainz, Dept Appl & Analyt Paleontol, Inst Geosci, Mainz, Germany
基金
加拿大自然科学与工程研究理事会;
关键词
ELECTRON-MICROPROBE; GROWTH; CLIMATE; RECONSTRUCTION;
D O I
10.2110/palo.2008.p08-116r
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
We present the first continuous, high-resolution record of Mg/Ca variations within an encrusting coralline red alga, Clathromorphum nereostratum, from Amchitka Island, Aleutian Islands. Mg/Ca ratios of individual growth increments were analyzed by measuring a single-point, electron-microprobe transect, yielding a resolution of similar to 15 samples/year and a 65-year record (1902-1967) of variations. Results show that Mg/Ca ratios in the high-Mg calcite algal framework display pronounced annual cyclicity and archive late spring-late fall sea-surface temperatures (SST) corresponding to the main season of algal growth. Mg/Ca values correlate well to local SST, as well as to an air temperature record from the same region. High spatial correlation to large-scale SST variability in the subarctic North Pacific is observed, with patterns of strongest correlation following the direction of major oceanographic features that play a key role in the exchange of water masses between the North Pacific and the Bering Sea. Our data correlate well with a shorter Mg/Ca record from a second site, corroborating the ability of the alga to reliably record regional environmental signals. In addition, Mg/Ca ratios relate well to a 29-year delta O-18 time series measured on the same sample, providing additional support for the use of Mg in coralline red algae as a paleotemperature proxy that, unlike algal-delta O-18, is not influenced by salinity fluctuations. Moreover, electron microprobe-based analysis enables higher sampling resolution and faster analysis, thus providing a promising approach for future studies of longer C. nereostratum records and applications to other coralline species.
引用
收藏
页码:406 / 412
页数:7
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