Cargando…

Major Sources of Organic Matter in a Complex Coral Reef Lagoon: Identification from Isotopic Signatures (δ(13)C and δ(15)N)

A wide investigation was conducted into the main organic matter (OM) sources supporting coral reef trophic networks in the lagoon of New Caledonia. Sampling included different reef locations (fringing, intermediate and barrier reef), different associated ecosystems (mangroves and seagrass beds) and...

Descripción completa

Detalles Bibliográficos
Autores principales: Briand, Marine J., Bonnet, Xavier, Goiran, Claire, Guillou, Gaël, Letourneur, Yves
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Public Library of Science 2015
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4509575/
https://www.ncbi.nlm.nih.gov/pubmed/26134985
http://dx.doi.org/10.1371/journal.pone.0131555
_version_ 1782382054043811840
author Briand, Marine J.
Bonnet, Xavier
Goiran, Claire
Guillou, Gaël
Letourneur, Yves
author_facet Briand, Marine J.
Bonnet, Xavier
Goiran, Claire
Guillou, Gaël
Letourneur, Yves
author_sort Briand, Marine J.
collection PubMed
description A wide investigation was conducted into the main organic matter (OM) sources supporting coral reef trophic networks in the lagoon of New Caledonia. Sampling included different reef locations (fringing, intermediate and barrier reef), different associated ecosystems (mangroves and seagrass beds) and rivers. In total, 30 taxa of macrophytes, plus pools of particulate and sedimentary OM (POM and SOM) were sampled. Isotopic signatures (C and N) of each OM sources was characterized and the composition of OM pools assessed. In addition, spatial and seasonal variations of reef OM sources were examined. Mangroves isotopic signatures were the most C-depleted (-30.17 ± 0.41 ‰) and seagrass signatures were the most C-enriched (-4.36 ± 0.72 ‰). Trichodesmium spp. had the most N-depleted signatures (-0.14 ± 0.03 ‰) whereas mangroves had the most N-enriched signatures (6.47 ± 0.41 ‰). The composition of POM and SOM varied along a coast-to-barrier reef gradient. River POM and marine POM contributed equally to coastal POM, whereas marine POM represented 90% of the POM on barrier reefs, compared to 10% river POM. The relative importance of river POM, marine POM and mangroves to the SOM pool decreased from fringing to barrier reefs. Conversely, the relative importance of seagrass, Trichodesmium spp. and macroalgae increased along this gradient. Overall, spatial fluctuations in POM and SOM were much greater than in primary producers. Seasonal fluctuations were low for all OM sources. Our results demonstrated that a large variety of OM sources sustain coral reefs, varying in their origin, composition and role and suggest that δ(13)C was a more useful fingerprint than δ(15)N in this endeavour. This study also suggested substantial OM exchanges and trophic connections between coral reefs and surrounding ecosystems. Finally, the importance of accounting for environmental characteristics at small temporal and spatial scales before drawing general patterns is highlighted.
format Online
Article
Text
id pubmed-4509575
institution National Center for Biotechnology Information
language English
publishDate 2015
publisher Public Library of Science
record_format MEDLINE/PubMed
spelling pubmed-45095752015-07-24 Major Sources of Organic Matter in a Complex Coral Reef Lagoon: Identification from Isotopic Signatures (δ(13)C and δ(15)N) Briand, Marine J. Bonnet, Xavier Goiran, Claire Guillou, Gaël Letourneur, Yves PLoS One Research Article A wide investigation was conducted into the main organic matter (OM) sources supporting coral reef trophic networks in the lagoon of New Caledonia. Sampling included different reef locations (fringing, intermediate and barrier reef), different associated ecosystems (mangroves and seagrass beds) and rivers. In total, 30 taxa of macrophytes, plus pools of particulate and sedimentary OM (POM and SOM) were sampled. Isotopic signatures (C and N) of each OM sources was characterized and the composition of OM pools assessed. In addition, spatial and seasonal variations of reef OM sources were examined. Mangroves isotopic signatures were the most C-depleted (-30.17 ± 0.41 ‰) and seagrass signatures were the most C-enriched (-4.36 ± 0.72 ‰). Trichodesmium spp. had the most N-depleted signatures (-0.14 ± 0.03 ‰) whereas mangroves had the most N-enriched signatures (6.47 ± 0.41 ‰). The composition of POM and SOM varied along a coast-to-barrier reef gradient. River POM and marine POM contributed equally to coastal POM, whereas marine POM represented 90% of the POM on barrier reefs, compared to 10% river POM. The relative importance of river POM, marine POM and mangroves to the SOM pool decreased from fringing to barrier reefs. Conversely, the relative importance of seagrass, Trichodesmium spp. and macroalgae increased along this gradient. Overall, spatial fluctuations in POM and SOM were much greater than in primary producers. Seasonal fluctuations were low for all OM sources. Our results demonstrated that a large variety of OM sources sustain coral reefs, varying in their origin, composition and role and suggest that δ(13)C was a more useful fingerprint than δ(15)N in this endeavour. This study also suggested substantial OM exchanges and trophic connections between coral reefs and surrounding ecosystems. Finally, the importance of accounting for environmental characteristics at small temporal and spatial scales before drawing general patterns is highlighted. Public Library of Science 2015-07-02 /pmc/articles/PMC4509575/ /pubmed/26134985 http://dx.doi.org/10.1371/journal.pone.0131555 Text en © 2015 Briand et al http://creativecommons.org/licenses/by/4.0/ This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are properly credited.
spellingShingle Research Article
Briand, Marine J.
Bonnet, Xavier
Goiran, Claire
Guillou, Gaël
Letourneur, Yves
Major Sources of Organic Matter in a Complex Coral Reef Lagoon: Identification from Isotopic Signatures (δ(13)C and δ(15)N)
title Major Sources of Organic Matter in a Complex Coral Reef Lagoon: Identification from Isotopic Signatures (δ(13)C and δ(15)N)
title_full Major Sources of Organic Matter in a Complex Coral Reef Lagoon: Identification from Isotopic Signatures (δ(13)C and δ(15)N)
title_fullStr Major Sources of Organic Matter in a Complex Coral Reef Lagoon: Identification from Isotopic Signatures (δ(13)C and δ(15)N)
title_full_unstemmed Major Sources of Organic Matter in a Complex Coral Reef Lagoon: Identification from Isotopic Signatures (δ(13)C and δ(15)N)
title_short Major Sources of Organic Matter in a Complex Coral Reef Lagoon: Identification from Isotopic Signatures (δ(13)C and δ(15)N)
title_sort major sources of organic matter in a complex coral reef lagoon: identification from isotopic signatures (δ(13)c and δ(15)n)
topic Research Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4509575/
https://www.ncbi.nlm.nih.gov/pubmed/26134985
http://dx.doi.org/10.1371/journal.pone.0131555
work_keys_str_mv AT briandmarinej majorsourcesoforganicmatterinacomplexcoralreeflagoonidentificationfromisotopicsignaturesd13candd15n
AT bonnetxavier majorsourcesoforganicmatterinacomplexcoralreeflagoonidentificationfromisotopicsignaturesd13candd15n
AT goiranclaire majorsourcesoforganicmatterinacomplexcoralreeflagoonidentificationfromisotopicsignaturesd13candd15n
AT guillougael majorsourcesoforganicmatterinacomplexcoralreeflagoonidentificationfromisotopicsignaturesd13candd15n
AT letourneuryves majorsourcesoforganicmatterinacomplexcoralreeflagoonidentificationfromisotopicsignaturesd13candd15n