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Controls on the organic chemical composition of settling particles in the northeast Atlantic Ocean

Controls on the organic chemical composition of settling particles in the northeast Atlantic Ocean
Controls on the organic chemical composition of settling particles in the northeast Atlantic Ocean
The organic matter of sinking particulate material collected in the Northeast Atlantic Ocean (ca. 49°N, 16°W) was investigated in order to determine temporal and depth-related variability in its composition. Three sediment traps were deployed at nominal depths of 1000 m (below the permanent thermocline), 3000 m (representing the deep-water fluxes) and at 4700 m, about 100 m above the seafloor (just above the benthic boundary layer). The samples span a 28-month sampling period from October 1995 until February 1998, each sample representing a period of between 7 and 28 days.
Total organic carbon and total nitrogen contents decrease with depth, as did the absolute concentrations of most biochemicals measured in this study, such as intact proteins and individual lipids. However, concentrations of proteins relative to total organic carbon and total nitrogen did not show any significant change with depth, implying that they are not being rapidly degraded and so may provide an important supply of nitrogen to the benthos. Fluxes of protein, TN and TOC are significantly correlated at all depths.
Lipid compositions vary temporally. During periods of high flux, particularly in the summer, the lipids are richer in ‘labile components’, namely unsaturated fatty acids and low molecular weight alcohols. During periods of low flux other compounds, such as sterols, steroidal ketones and a trisnorhopan-21-one are more abundant. One sample, taken close to the seafloor, was highly enriched in lipids, sterols and fatty acids in particular; this may represent detritus derived from bottom-dwelling invertebrates.
northeast atlantic ocean, sampling, sinking particles, lipids, organic carbon, nitrogen
0079-6611
65-87
Kiriakoulakis, Konstadinos
8bca3454-1cd7-4ecc-b5a6-27a99b8836fd
Stutt, Edward
99e05d61-f33e-4672-86fd-b93fffaffe62
Rowland, Steven J.
1f11586f-fda1-4e78-9c78-febdea0dc81c
Vangriesheim, Annick
69938cad-1af6-4a53-b1d3-f7bba8b6daeb
Lampitt, Richard S.
dfc3785c-fc7d-41fa-89ee-d0c6e27503ad
Wolff, George A.
6b29d886-06f9-4405-8fab-33cfb436acaa
Kiriakoulakis, Konstadinos
8bca3454-1cd7-4ecc-b5a6-27a99b8836fd
Stutt, Edward
99e05d61-f33e-4672-86fd-b93fffaffe62
Rowland, Steven J.
1f11586f-fda1-4e78-9c78-febdea0dc81c
Vangriesheim, Annick
69938cad-1af6-4a53-b1d3-f7bba8b6daeb
Lampitt, Richard S.
dfc3785c-fc7d-41fa-89ee-d0c6e27503ad
Wolff, George A.
6b29d886-06f9-4405-8fab-33cfb436acaa

Kiriakoulakis, Konstadinos, Stutt, Edward, Rowland, Steven J., Vangriesheim, Annick, Lampitt, Richard S. and Wolff, George A. (2001) Controls on the organic chemical composition of settling particles in the northeast Atlantic Ocean. Progress in Oceanography, 50 (1/4), 65-87. (doi:10.1016/S0079-6611(01)00048-9).

Record type: Article

Abstract

The organic matter of sinking particulate material collected in the Northeast Atlantic Ocean (ca. 49°N, 16°W) was investigated in order to determine temporal and depth-related variability in its composition. Three sediment traps were deployed at nominal depths of 1000 m (below the permanent thermocline), 3000 m (representing the deep-water fluxes) and at 4700 m, about 100 m above the seafloor (just above the benthic boundary layer). The samples span a 28-month sampling period from October 1995 until February 1998, each sample representing a period of between 7 and 28 days.
Total organic carbon and total nitrogen contents decrease with depth, as did the absolute concentrations of most biochemicals measured in this study, such as intact proteins and individual lipids. However, concentrations of proteins relative to total organic carbon and total nitrogen did not show any significant change with depth, implying that they are not being rapidly degraded and so may provide an important supply of nitrogen to the benthos. Fluxes of protein, TN and TOC are significantly correlated at all depths.
Lipid compositions vary temporally. During periods of high flux, particularly in the summer, the lipids are richer in ‘labile components’, namely unsaturated fatty acids and low molecular weight alcohols. During periods of low flux other compounds, such as sterols, steroidal ketones and a trisnorhopan-21-one are more abundant. One sample, taken close to the seafloor, was highly enriched in lipids, sterols and fatty acids in particular; this may represent detritus derived from bottom-dwelling invertebrates.

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More information

Published date: 2001
Keywords: northeast atlantic ocean, sampling, sinking particles, lipids, organic carbon, nitrogen

Identifiers

Local EPrints ID: 7833
URI: http://eprints.soton.ac.uk/id/eprint/7833
ISSN: 0079-6611
PURE UUID: a1be92c6-5284-4ac4-84ca-dcb118de9681

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Date deposited: 01 Jul 2004
Last modified: 15 Mar 2024 04:49

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Contributors

Author: Konstadinos Kiriakoulakis
Author: Edward Stutt
Author: Steven J. Rowland
Author: Annick Vangriesheim
Author: Richard S. Lampitt
Author: George A. Wolff

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