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Exotic Halophila stipulacea is an introduced carbon sink for the Eastern Mediterranean Sea
Carbon and nitrogen storage in exotic Halophila stipulacea were compared to that in native Posidonia oceanica and Cymodocea nodosa meadows and adjacent unvegetated sediments of the Eastern Mediterranean Sea and to that in native H. stipulacea of the Red Sea at sites with different biogeochemical con...
Autores principales: | , , , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2019
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6610076/ https://www.ncbi.nlm.nih.gov/pubmed/31270338 http://dx.doi.org/10.1038/s41598-019-45046-w |
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author | Apostolaki, Eugenia T. Vizzini, Salvatrice Santinelli, Veronica Kaberi, Helen Andolina, Cristina Papathanassiou, Evangelos |
author_facet | Apostolaki, Eugenia T. Vizzini, Salvatrice Santinelli, Veronica Kaberi, Helen Andolina, Cristina Papathanassiou, Evangelos |
author_sort | Apostolaki, Eugenia T. |
collection | PubMed |
description | Carbon and nitrogen storage in exotic Halophila stipulacea were compared to that in native Posidonia oceanica and Cymodocea nodosa meadows and adjacent unvegetated sediments of the Eastern Mediterranean Sea and to that in native H. stipulacea of the Red Sea at sites with different biogeochemical conditions and level of human pressure. Exotic H. stipulacea possessed considerable storing capacity, with 2-fold higher C(org) stock (0.71 ± 0.05 kg m(−2) in the top 20 cm of sediment) and burial (14.78 gC(org) m(−2) y(−1)) than unvegetated areas and C. nodosa meadows and, surprisingly, comparable to P. oceanica. N (0.07 ± 0.01 kg m(−2)) and C(inorg) (14.06 ± 8.02 kg m(−2)) stocks were similar between H. stipulacea and C. nodosa or unvegetated sediments, but different to P. oceanica. C(org) and N stocks were higher in exotic than native H. stipulacea populations. Based on isotopic mixing model, organic material trapped in H. stipulacea sediments was mostly allochthonous (seagrass detritus 17% vs seston 67%). C(org) stock was similar between monospecific and invaded C. nodosa meadows by H. stipulacea. Higher stocks were measured in the higher human pressure site. H. stipulacea introduction may contribute in the increase of carbon sequestration in the Eastern Mediterranean. |
format | Online Article Text |
id | pubmed-6610076 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2019 |
publisher | Nature Publishing Group UK |
record_format | MEDLINE/PubMed |
spelling | pubmed-66100762019-07-14 Exotic Halophila stipulacea is an introduced carbon sink for the Eastern Mediterranean Sea Apostolaki, Eugenia T. Vizzini, Salvatrice Santinelli, Veronica Kaberi, Helen Andolina, Cristina Papathanassiou, Evangelos Sci Rep Article Carbon and nitrogen storage in exotic Halophila stipulacea were compared to that in native Posidonia oceanica and Cymodocea nodosa meadows and adjacent unvegetated sediments of the Eastern Mediterranean Sea and to that in native H. stipulacea of the Red Sea at sites with different biogeochemical conditions and level of human pressure. Exotic H. stipulacea possessed considerable storing capacity, with 2-fold higher C(org) stock (0.71 ± 0.05 kg m(−2) in the top 20 cm of sediment) and burial (14.78 gC(org) m(−2) y(−1)) than unvegetated areas and C. nodosa meadows and, surprisingly, comparable to P. oceanica. N (0.07 ± 0.01 kg m(−2)) and C(inorg) (14.06 ± 8.02 kg m(−2)) stocks were similar between H. stipulacea and C. nodosa or unvegetated sediments, but different to P. oceanica. C(org) and N stocks were higher in exotic than native H. stipulacea populations. Based on isotopic mixing model, organic material trapped in H. stipulacea sediments was mostly allochthonous (seagrass detritus 17% vs seston 67%). C(org) stock was similar between monospecific and invaded C. nodosa meadows by H. stipulacea. Higher stocks were measured in the higher human pressure site. H. stipulacea introduction may contribute in the increase of carbon sequestration in the Eastern Mediterranean. Nature Publishing Group UK 2019-07-03 /pmc/articles/PMC6610076/ /pubmed/31270338 http://dx.doi.org/10.1038/s41598-019-45046-w Text en © The Author(s) 2019 Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/. |
spellingShingle | Article Apostolaki, Eugenia T. Vizzini, Salvatrice Santinelli, Veronica Kaberi, Helen Andolina, Cristina Papathanassiou, Evangelos Exotic Halophila stipulacea is an introduced carbon sink for the Eastern Mediterranean Sea |
title | Exotic Halophila stipulacea is an introduced carbon sink for the Eastern Mediterranean Sea |
title_full | Exotic Halophila stipulacea is an introduced carbon sink for the Eastern Mediterranean Sea |
title_fullStr | Exotic Halophila stipulacea is an introduced carbon sink for the Eastern Mediterranean Sea |
title_full_unstemmed | Exotic Halophila stipulacea is an introduced carbon sink for the Eastern Mediterranean Sea |
title_short | Exotic Halophila stipulacea is an introduced carbon sink for the Eastern Mediterranean Sea |
title_sort | exotic halophila stipulacea is an introduced carbon sink for the eastern mediterranean sea |
topic | Article |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6610076/ https://www.ncbi.nlm.nih.gov/pubmed/31270338 http://dx.doi.org/10.1038/s41598-019-45046-w |
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