Feeding Preferences of Abyssal Macrofauna Inferred from In Situ Pulse Chase Experiments
Feeding Preferences of Abyssal Macrofauna Inferred from In Situ Pulse Chase Experiments
Climatic fluctuations may significantly alter the taxonomic and biochemical composition of phytoplankton blooms and subsequently phytodetritus, the food source for the majority of deep-sea communities. To examine the response of abyssal benthic communities to different food resources we simulated a food sedimentation event containing diatoms and coccolithophorids at Station M in the NE Pacific. In one set of experiments we measured incorporation of diatomC and coccoN into the macrofauna using isotopically enriched 13C-diatoms and 15N-coccolithophores. In a second experiment we measured incorporation of C and N from dual-labelled (13C and 15N) diatoms. The second experiment was repeated 2 months later to assess the effect of seasonality. The simulated food pulses represented additions of 650 – 800 mg C m?2 and 120 mg N m?2 to the seafloor. In all cases rapid incorporation of tracer was observed within 4 days, with between 20% and 52% of the macrofauna displaying evidence of enrichment. However, incorporation levels of both diatomC and coccoN were low (<0.05% and 0.005% of the added C and N). Incorporation of labelled diatoms was similar during both June and September suggesting that the community was not food limited during either period. We found no evidence for selective ingestion of the different food types in the metazoan fauna suggesting that macrofauna do not have strong preferences for diatom vs. coccolithophore dominated phytodetrital pulses. C:N ratios from both experiments suggest that the metazoan macrofauna community appear to have higher C demands and/or assimilation efficiencies compared to N. Concomitantly, the foraminifera preferentially selected for diatomN over coccoN, and we suggest that this may be related to foraminiferal requirements for intracellular nitrate. These experiments provide evidence that abyssal faunal feeding strategies are in part driven by an organism's internal stoichiometric budgets and biochemical requirements.
e80510
Jeffreys, Rachel M.
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Burke, Ciara
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Jamieson, Alan J.
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Narayanaswamy, Bhavani E.
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Ruhl, Henry A.
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Smith, Kenneth L.
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Witte, Ursula
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26 November 2013
Jeffreys, Rachel M.
00be4640-1d07-4f82-964a-0a61b50322c4
Burke, Ciara
e706a0d7-a655-4fad-908e-0e71a8047d67
Jamieson, Alan J.
ab7c9067-fe1d-47f9-921f-c57108b6f23c
Narayanaswamy, Bhavani E.
fcecfc2f-1db0-4786-a379-78411de47a3d
Ruhl, Henry A.
177608ef-7793-4911-86cf-cd9960ff22b6
Smith, Kenneth L.
c282f721-59cf-4caa-a344-f4a26f6b534c
Witte, Ursula
b7f0d0ef-2b87-4259-b803-a752262d5de2
Jeffreys, Rachel M., Burke, Ciara, Jamieson, Alan J., Narayanaswamy, Bhavani E., Ruhl, Henry A., Smith, Kenneth L. and Witte, Ursula
(2013)
Feeding Preferences of Abyssal Macrofauna Inferred from In Situ Pulse Chase Experiments.
PLoS ONE, 8 (11), .
(doi:10.1371/journal.pone.0080510).
Abstract
Climatic fluctuations may significantly alter the taxonomic and biochemical composition of phytoplankton blooms and subsequently phytodetritus, the food source for the majority of deep-sea communities. To examine the response of abyssal benthic communities to different food resources we simulated a food sedimentation event containing diatoms and coccolithophorids at Station M in the NE Pacific. In one set of experiments we measured incorporation of diatomC and coccoN into the macrofauna using isotopically enriched 13C-diatoms and 15N-coccolithophores. In a second experiment we measured incorporation of C and N from dual-labelled (13C and 15N) diatoms. The second experiment was repeated 2 months later to assess the effect of seasonality. The simulated food pulses represented additions of 650 – 800 mg C m?2 and 120 mg N m?2 to the seafloor. In all cases rapid incorporation of tracer was observed within 4 days, with between 20% and 52% of the macrofauna displaying evidence of enrichment. However, incorporation levels of both diatomC and coccoN were low (<0.05% and 0.005% of the added C and N). Incorporation of labelled diatoms was similar during both June and September suggesting that the community was not food limited during either period. We found no evidence for selective ingestion of the different food types in the metazoan fauna suggesting that macrofauna do not have strong preferences for diatom vs. coccolithophore dominated phytodetrital pulses. C:N ratios from both experiments suggest that the metazoan macrofauna community appear to have higher C demands and/or assimilation efficiencies compared to N. Concomitantly, the foraminifera preferentially selected for diatomN over coccoN, and we suggest that this may be related to foraminiferal requirements for intracellular nitrate. These experiments provide evidence that abyssal faunal feeding strategies are in part driven by an organism's internal stoichiometric budgets and biochemical requirements.
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Published date: 26 November 2013
Organisations:
Marine Biogeochemistry
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Local EPrints ID: 360175
URI: http://eprints.soton.ac.uk/id/eprint/360175
ISSN: 1932-6203
PURE UUID: 98c7fafc-e664-47d2-8f71-d95230833682
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Date deposited: 27 Nov 2013 16:16
Last modified: 14 Mar 2024 15:33
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Author:
Rachel M. Jeffreys
Author:
Ciara Burke
Author:
Alan J. Jamieson
Author:
Bhavani E. Narayanaswamy
Author:
Henry A. Ruhl
Author:
Kenneth L. Smith
Author:
Ursula Witte
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