4.7 Article

Linked variations in sediment accumulation rates and sea-level in Guanabara Bay, Brazil, over the last 6000 years

期刊

出版社

ELSEVIER SCIENCE BV
DOI: 10.1016/j.palaeo.2014.08.027

关键词

Guanabara Bay; Accumulation rates; Sea-level; Brazil; Sedimentation

资金

  1. Brazilian National Research Council (CNPq)

向作者/读者索取更多资源

Variable sediment accumulation rates in cores collected in Guanabara Bay, Rio de Janeiro State, indicate that filling of the bay started before 6000 years ago and that it was not uniform through time. Comparison of these variable sediment accumulation rates and sea-level fluctuations over the last 5500 years suggests a linear relation between them. The sea-level drop between 5500 and 5000 years ago, for example, corresponds to higher accumulation rates between 5130 and 4350 calendar years BP. At this time, the sea-level change from 5 to 2 m above present sea-level caused a drop of wave base level and consequently an increase of sediment supply to deeper parts of Guanabara Bay. Between approximately 4350 and 2000-1800 years ago sea level became stable with consequent reduction in the accumulation rate. From this time until approximately 500 years ago accumulation rates increased again because of another sea-level drop from 2 m to the present sea-level. The rate of the second sea-level drop was not as high as the first one, and neither was the accumulation rate increase. Although radiocarbon dates suggest a dramatic reduction of accumulation rates between similar to 4000-2000 years ago, estimates for the last 150 years based on Pb-210 indicate a progressive increase in the accumulation rates despite the presumed stability and perhaps even a small elevation of modern sea-level in the last 150 years as deduced from tide gauge records. Accumulation rates increase from 0.14 cm.yr(-1) to 0.49 cm.yr(-1) for the period of 1922 to 1951 and reach 0.60 cm.yr(-1) from 1963 to 1993. In the last five years accumulation rates double, increasing from 0.60 cm.yr(-1) to 1.25 cm.yr(-1). These higher accumulation rates during stable or rising sea-level are likely due to local increases in deforestation, expansion of farming land, dredging of channels, and increased paving of roadways. (C) 2014 Elsevier B.V. All rights reserved.

作者

我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。

评论

主要评分

4.7
评分不足

次要评分

新颖性
-
重要性
-
科学严谨性
-
评价这篇论文

推荐

暂无数据
暂无数据