印度东南海岸泰米尔纳德邦卡达洛尔加迪拉姆河口岩心沉积物中的梭形纲动物的纹理特征和分布情况

Elumalai K, Ramachandran A, Hussain S M, Stephen Pitchaimani V
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引用次数: 0

摘要

为了解咸水梭形纲动物的分布情况并研究沉积物特征,我们从加地拉姆河口采集了一个 105 厘米长的岩芯,并以 5 厘米宽的固定间隔将其分成 21 个样本。所有沉积物样本都按照标准的微古生物学技术进行了分析,以研究浮游动物的分布和出现情况。根据已发表的文章,共鉴定出隶属于 Podocopida 目 16 属、12 科、3 超科和 2 亚目的 27 种介孔动物分类群。岩芯中广泛分布着 Kalingella mckenziei 和 Jankeijcythere mckenziei 两种桡足类,它们的数量超过了其他物种。所记录的动物群落属于热带、咸水至沼泽(浅海)和底栖动物(Hemicytheridea paiki、 Hemicytheridea bhatiai、Jankeijcythere mckenziei、Kalingella mckenziei、Neosinocythere dekrooni、Paijenborchellina sp.、Stigmatocythere indica 和 Tanella gracilis)。在分析的岩芯中,80-85 厘米和 95-105 厘米深处没有动物群落。此外,还测定了碳酸钙、有机质和砂-淤泥-粘土比率等沉积物特征,并将其与观察到的底栖生物种群进行了相关分析。根据详细研究,发现沉积物中的高碳酸钙和低有机质有利于种群数量的增加。从所有子样本中的梭口鱼总体分布情况来看,淤泥质沙是梭口鱼繁衍生息的理想基质。研究了梭口蟹腕瓣比的统计方面,以确定沉积速率,从而推断出加迪拉姆河河口沉积物的沉积速率较快。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Textural characteristics and distribution of ostracoda in core sediments from the Gadilam river estuary, Cuddalore, Tamil Nadu, southeast coast of India
To know the distribution of brackish water Ostracoda and to investigate the sediment characteristics, a core (105 cm) has been collected from the Gadilam river estuary and it was sub-sampled into 21 samples at 5 cm width regular interval. All the sediment samples were analyzed as per standard micropaleontological techniques in order to investigate the distribution and occurrence of ostracod fauna. A total of 27 ostracod taxa belonging to 16 genera, 12 families, 3 superfamilies and 2 sub-order of the order Podocopida, have been identified based on published articles Throughout the core (from top to bottom) the calcareous forms were noticed. The ostracod species Kalingella mckenziei and Jankeijcythere mckenziei are widely distributed in the core and they outnumbered the rest of the species. The faunal assemblages recorded are tropical, brackish to neritic (shallow marine) and benthic in nature (Hemicytheridea paiki, Hemicytheridea bhatiai, Jankeijcythere mckenziei, Kalingella mckenziei, Neosinocythere dekrooni, Paijenborchellina sp., Stigmatocythere indica and Tanella gracilis). In the analyzed core, there is no faunal assemblage at the depth between 80-85 and 95-105 cm. The sediment characteristics such as calcium carbonate, organic matter and sand-silt-clay ratio also determined and correlated with the observed ostracod populations. Based on the detailed study, it is noticed that high calcium carbonate and low organic matter of the sediment are congenial for population abundance. From the overall distribution of Ostracoda in all the subsamples, siltysand is found to an accommodative substrate for the prosperity of Ostracoda. The statistical aspect of ostracod carapace-valve ratio has been studied to identify the rate of sedimentation which infers a faster rate of deposition of sediments in the Gadilam River estuary.
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