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珊瑚藻钡作为 20 世纪西北北大西洋表层海洋淡水变化的指示剂。

Coralline algal barium as indicator for 20th century northwestern North Atlantic surface ocean freshwater variability.

机构信息

CPS-Department, University of Toronto Mississauga, 3359 Mississauga Rd. N, Mississauga, ON, L5L 1C6, Canada.

出版信息

Sci Rep. 2013;3:1761. doi: 10.1038/srep01761.

Abstract

During the past decades climate and freshwater dynamics in the northwestern North Atlantic have undergone major changes. Large-scale freshening episodes, related to polar freshwater pulses, have had a strong influence on ocean variability in this climatically important region. However, little is known about variability before 1950, mainly due to the lack of long-term high-resolution marine proxy archives. Here we present the first multidecadal-length records of annually resolved Ba/Ca variations from Northwest Atlantic coralline algae. We observe positive relationships between algal Ba/Ca ratios from two Newfoundland sites and salinity observations back to 1950. Both records capture episodical multi-year freshening events during the 20th century. Variability in algal Ba/Ca is sensitive to freshwater-induced changes in upper ocean stratification, which affect the transport of cold, Ba-enriched deep waters onto the shelf (highly stratified equals less Ba/Ca). Algal Ba/Ca ratios therefore may serve as a new resource for reconstructing past surface ocean freshwater changes.

摘要

在过去几十年中,北大西洋西北部的气候和淡水动态发生了重大变化。与极地淡水脉冲有关的大规模淡水事件对这个气候重要地区的海洋变率产生了强烈影响。然而,由于缺乏长期的高分辨率海洋代用记录,人们对 1950 年以前的变化知之甚少。在这里,我们展示了北大西洋珊瑚藻类中首次获得的具有数十年长度的年度分辨率钡/钙变化记录。我们观察到来自纽芬兰两个地点的藻类钡/钙比值与回溯到 1950 年的盐度观测之间存在正相关关系。这两个记录都捕捉到了 20 世纪期间多次发生的多年期淡水事件。藻类钡/钙的变化对上层海洋分层引起的淡水变化敏感,这会影响富含钡的冷深水流输送到大陆架上(分层度高表示钡/钙比值低)。因此,藻类钡/钙比值可能成为重建过去表层海洋淡水变化的新资源。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/462c/3641520/1a730f277ffb/srep01761-f1.jpg

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