印度孙德尔本斯三角洲群岛红树林地表下沉积物岩心中的硅藻

Manjushree Mandal, B. Biswas, S. Sekh, N. S. Sarkar
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引用次数: 3

摘要

沉积物中组成硅藻组合的物种提供了过去和现在与土壤和水物理化学有关的环境条件和生物多样性动态数据的重要信息。这些信息可以揭示该地区的发展历史。硅藻对环境的随机变化非常敏感,这使它们成为非常可靠的生物指标。本研究的目的是破译来自印度孙德尔本斯的硅藻组合提供的生物多样性相关信息。在两个沉积物岩心的顶部50 cm层中发现了硅藻:一个是新淤积的三角洲地块,红树林处于演替早期阶段,另一个是保护区网络内的一个岛屿,红树林处于演替后期。鉴定并描述了15种过去在印度孙德尔本斯沉积物中没有记录的硅藻。其中有四种浮游植物曾在孙德尔本斯群岛的浮游植物记录中被偶尔提及,但未在分类学上得到证实。本文提供了所有15种的鉴定和命名注释。中心形态Coscinodiscus spp.、Cyclotella spp.和Thalassiosira spp.的丰度和物种丰富度都很高,这是由于它们靠近河口河流,并且经常被淹没,导致沉积物岩心内浮游生物形态的沉降。在该地区首次报道的许多pennate形式,即Amphicampa eruca, Amphora holsatica, Diploneis spp.(除了Z). smithii), Epithemia turgida, eunotiapecectinalis, Giffenia cocconeiformis和Rhaphoneis rhombus,从未被描述为河口水域浮游生物群落的一部分,验证了它们的“土壤硅藻”地位。沉积物中典型的浅水硅藻,即肉芽藻和膨乳藻,表明这些地区的盐度较低,并不比现在早多少。
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Diatoms in Sub-Surface Sediment Cores from Mangrove Forest Floors of Deltaic Islands in Sundarbans, India
Species constituting diatom assemblages in sediments provide important information regarding the past and present environmental conditions related to soil and water physico-chemistry and also biodiversity dynamics data. This information can reveal the developmental history of the region. Diatoms are sensitive to stochastic changes in the environment, making them extremely reliable bio-indicators. The purpose of the present study was to decipher such biodiversity related information provided by the diatom assemblages from the Indian Sundarbans. Diatoms were identified in the top 50 cm layer of two sediment cores: a newly silted up deltaic landmass with mangroves in early succession stage, and an island within the Protected Area Network with mangroves in late succession stage. Fifteen diatom species, with no past records in the sediments of Indian Sundarbans were identified and described. Four species among them are sporadically mentioned in previous phytoplankton records fi-om the Sundarbans, but these are not confirmed taxonomically. This paper provides identification and nomenclatural notes on all 15 species. High abundance and species richness of the centric forms Coscinodiscus spp., Cyclotella spp., and Thalassiosira spp. at both the sites is attributed to their proximity to estuarine rivers and their regular inundation, leading to settling of planktonic forms within sediment cores. Many pennate forms, namely Amphicampa eruca, Amphora holsatica, Diploneis spp. (except Z). smithii), Epithemia turgida, Eunotiapectinalis, Giffenia cocconeiformis , and Rhaphoneis rhombus which are being reported for the first time fi-om this region have never been part of described planktonic communities in estuarine waters, validating their' soil diatom' status. Typical fi-eshwater diatoms, namely Aulacoseira granulata and Epithemia turgida, in the sediments indicate lower salinity in these areas, not much earlier than present times.
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Journal of the Bombay Natural History Society
Journal of the Bombay Natural History Society Environmental Science-Nature and Landscape Conservation
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