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Jérôme OLLIER

Distribution Pattern of the Benthic Meiofaunal Community Along the Depth Gradient of th... - 0 views

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    The continental margin harbors a variety of habitats that support incredible biodiversity and the function of their oceans' ecosystems. The meiofauna is considered a significant component of the benthic faunal community from the polar to the tropical regions. The meiofaunal community in the deep Indian Ocean, especially along the depth gradient, is poorly investigated. The present study aims to explore the benthic meiofaunal community structure along the depth gradients and its associated environment in the western Indian continental margin (WICM) and abyssal plain in the eastern Arabian Sea. Sediment samples were collected from seven different depths (111-3,918 m) along the WICM including the oxygen minimum zone (OMZ) and abyssal plain. A total of 22 taxa (groups) were encountered along the WICM. The nematodes (85%) were the most dominant taxa in all the depths, followed by copepods (11%), nauplii (5%), and polychaetes (1.36%). Our results suggest that (a) the organic matter has accumulated in OMZ sites; (b) a high amount of total organic carbon did not influence the meiofaunal density or biomass; (c) oxygen and depth gradients were significant drivers of the meiofaunal community, low levels of oxygen contributed to lower taxa diversity and density at 485 and 724 m depths; (d) a significant relationship of meiofaunal density and biomass with chloroplastic pigment equivalent (CPE) values indicates pelagic-benthic coupling. Copepods, nauplii, tanaidaceans, isopods, kinorhynchs, and cumaceans were affected by the low-oxygen conditions at the OMZ sites. Enhanced meiofaunal diversity, density, and biomass at deeper sites (non-OMZ-D) was attributed to increased abundance of copepods, nauplii, tanaidaceans, isopods, kinorhynchs, and cumaceans and were mostly concentrated on the surface sediment (0-4 cm) triggered by enhanced bottom-water oxygen and freshness of available food outside the OMZ except 3,918 m. Therefore, the present study showed the meiofaunal community
Jérôme OLLIER

Bacterial and Fungal Diversity in Sediment and Water Column From the Abyssal Regions of... - 0 views

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    The deep sea is the largest environment on Earth, comprising important resources of commercial interest. It is composed of a wide variety of ecosystems, which is home to often unique organisms that are yet to be described. The deep-sea is one of the least studied environments, where research is strongly linked to technological access and advances. With the recent advances in the next-generation sequencing and bioinformatics tools, there is an enhanced understanding of microbial diversity and ecological functions in deep sea. Multidisciplinary programs are being undertaken to investigate into microbial communities in diverse marine environments. As compared to other Oceans, the deeper parts of Indian Ocean are still poorly sampled and studied for bacterial, and more so fungal diversity. The studies reporting usage of modern sequencing tools to describe uncultured microbial diversity have seen a rise in numbers in the last decade. In this review, we summarize the important findings of research works carried on bacterial and fungal diversity from the abyssal regions of the Indian Ocean and provide our views on possible future paths.
Jérôme OLLIER

Scientists go back to the abyss - tropical edition! - @CSIRO - 0 views

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    CSIRO's research vessel (RV) Investigator departed Darwin for a 45-day voyage of biodiversity discovery in the tropical waters of the Indian Ocean.
Jérôme OLLIER

Le balisage des requins est prêt à débuter : "Une première" - Zinfos974 - 0 views

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    Le balisage des requins est prêt à débuter : "Une première".
Jérôme OLLIER

Via @leguen - Research project aims to unravel the mystery of deep-sea whales... - 0 views

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    Research project aims to unravel the mystery of deep-sea whales off Fujairah's coast.
Jérôme OLLIER

Seafloor Shapes on the Flanks of Mid-Ocean Ridges Linked to Magma Supply - @AGU_Eos - 0 views

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    New research suggests the source of morphologic variation on mid-ocean ridges might be deeper than scientists thought.
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