果阿河口地区的底栖有孔虫生物群落

IF 1.6 3区 地球科学 Q2 GEOLOGY
M. G. A. PADMANABHA SETTY
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引用次数: 0

摘要

底栖有孔虫对河口环境的微妙变化反应灵敏。有鉴于此,我们对从果阿的曼多维-祖阿里河口和相连的长而窄的 Cumbarjua 运河采集的样本进行了底栖有孔虫的定性分析。河流下游的底质主要是沙子,而河口上游地区的底质是淤泥质沙子,运河地区的底质是粘土。有孔虫生物主要分布在河流的上游河口区和 Cumbarjua 运河交界区,以氨有孔虫和 Miliammina fusca 为特征;而运河区则富含凝集型有孔虫。氨藻类-鹅膏藻类群在河口下游区域占主导地位,表明这里是典型的海洋环境。有机物含量较高,尤其是在运河区,这是由于附近的农药厂和航行的驳船以及渔业的其他机械化船只不断排放污染物造成的。氨菌及其变种和其他凝集物种在这里占主导地位。钙质物种的减少和死亡试验的稀疏导致它们最终被毁,这可能是由于它们易受水体酸性的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
BENTHIC FORAMINIFERAL BIOCOENOSES IN THE ESTUARINE REGIMES OF GOA
Benthic Foraminifera are highly responsive to subtle changes in the estuarine environment. Keeping this in view, a qualitative analysis of living benthic Foraminifera was made of the samples collected from the Mandovi—Zuari estuaries and the connecting long and narrow Cumbarjua canal of Goa. The lower reaches of the rivers are paved with a substrate consisting mostly of sand while it is silty—sand in the upper estuarine zones and clayey in the canal zone. The living Foraminifera are abundant in the upper estuarine zones of the rivers and the Cumbarjua canal junction zones, and characterised by the Ammonia—Trochammina suite with Miliammina fusca; while the canal zone is enriched by agglutinated formes. The Ammonia—Elphidium suite dominates the lower estuarine zones indicating a typical marine environment. The high organic matter content particularly in the Canal Zone is due to the inflow of pollutan ts from the nearby pesticide factory and the constant contaminating discharge of navigating barges and other mechanised boats of the fishing industry. Ammonia sp. and its variants and other agglutinated species become dominant here. The decline in calcareous species and thinning of the dead tests leading to their eventual destruction may be attributed to their susceptibility to acidity in the waters.
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来源期刊
CiteScore
3.60
自引率
4.30%
发文量
28
审稿时长
>12 weeks
期刊介绍: The Rivista Italiana di Paleontologia e Stratigrafia was founded in 1895. It publishes original papers dealing with all fields of paleontology and of stratigraphy, from Italy and the Mediterranean to the Tethys, as well across the globe from China to North America.
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