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Journal ArticleDOI

Bathyal meiobenthos of the western Coral Sea: distribution and abundance in relation to microbial standing stocks and environmental factors

Daniel M. Alongi, +1 more
- Vol. 35, Iss: 4, pp 491-503
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TLDR
Densities of Foraminifera and other protozoans increased with bathymetric depth, indicating their ability to exploit oligotrophic conditions and to gain numerical dominance in benthic food webs of the deep sea.
Abstract
The distribution and abundance of meiobenthos in relation to microbial densities and environmental factors were examined at 24 stations in a bathyal (298–1610 m) region of the western Coral Sea. Densities of metazoan meiofauna were low (x = 57; range: 19–170 individuals 10 cm−2) compared with other bathyal communtiesm but when densities of living Foraminifera (x = 560; range: 0–3410 individuals 10 cm−2) were included, total faunal densities were high (x = 610 10 cm−2) and ranged from 73 to 3465 individuals 10 cm−2. Soft-bodied (non-chitinous) taxa (e.g. turbellarians) were not detected beyond the continental slope. Densities of all metazoan taxa, excluding nematodes, decreased significantly with bathymetric depth. When the effect of ocean depth was held constant, only a few significant correlations of meiobenthos with microbes and sediment characteristics were found. Our data, coupled with earlier findings of low bacterial densities and organic conditions, suggest that low densities of metazoan meiobenthos in the western Coral Sea are due to low rates of detrital input. However, densities of Foraminifera and other protozoans increased with bathymetric depth (Alongi, 1987, Deep-Sea Research, 34, 1245–1254), indicating their ability to exploit oligotrophic conditions and to gain numerical dominance in benthic food webs of the deep sea.

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Citations
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Journal ArticleDOI

Responses by benthic organisms to inputs of organic material to the ocean floor:a review.

TL;DR: In this article, it has been shown that macroaggregates originating from the euphotic zone settle at a rate of approximately 100-150 m d -1 to form a deposit (phytodetritus) on the sediment surface.
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Global bathymetric patterns of standing stock and body size in the deep-sea benthos

TL;DR: The first global-scale analysis of standing stock (abundance and biomass) for 4 major size classes of deep-sea biota: bacteria, meta- zoan meiofauna, macrofauna and megafauna shows a dramatic decrease in total community standing stock and the ascendancy of smaller organisms with depth.
Journal ArticleDOI

Distribution of rose bengal stained deep-sea benthic foraminifera from the Nova Scotian continental margin and Gulf of Maine

TL;DR: In this article, foraminifera are vertically stratified within surficial sediments raised from 200 to 3000 m water depth, and a shallow habitat depth of 3 cm exists in shallow water (a 202 m core) in the Gulf of Maine.
Book ChapterDOI

The role of benthic foraminifera in deep-sea food webs and carbon cycling

TL;DR: Foraminifera playa largely unquantified but potentially significant role in deep-sea carbon cycling is potentially significant.
Journal ArticleDOI

Benthic response to particulate fluxes in different trophic environments: a comparison between the Gulf of Lions–Catalan Sea (western-Mediterranean) and the Cretan Sea (eastern-Mediterranean)

TL;DR: In this paper, particle fluxes, sedimentary OM composition, microbial and meiofaunal parameters are summarised from various stations in the Gulf of Lions and Catalan Sea (North-Western Mediterranean) and in the Cretan Sea (Eastern Mediterranean), investigated between 1993 and 1996.
References
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Book

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TL;DR: In this article, the Straight Line Case is used to fit a straight line by least squares, and the Durbin-Watson Test is used for checking the straight line fit.
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Ivan Valiela
TL;DR: In this paper, the authors studied the role of primary producers in marine ecosystems and their role in the formation of organic matter in photosynthesis and secondary production of marine organisms, as well as the effect of other factors on primary production.
Journal ArticleDOI

Seasonal sedimentation of phytoplankton to the deep-sea benthos

TL;DR: In this article, a similar seasonal pulse of detrital material to bathyal and abyssal depths in temperate latitudes is presented, this material seems to be derived directly from the surface primary production and to sink rapidly to the deep-sea benthos.
Journal ArticleDOI

Microhabitats of benthic foraminifera within deep-sea sediments

TL;DR: In this article, an analysis of living (stained) benthic foraminifera within the upper 15 cm of deep-sea sediments, which reveals species-specific microhabitat preferences, with distinct morphological features found with epifaunal and infaunal species.
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