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西加勒比海环礁的珊瑚礁退化。

Coral reef degradation at an atoll of the Western Colombian Caribbean.

机构信息

Programa de Biodiversidad y Ecosistemas Marinos, Instituto de Investigaciones Marinas y Costeras-INVEMAR, Santa Marta, Colombia.

Laboratorio de Biología Molecular Marina-BIOMMAR, Universidad de los Andes, Bogotá, Colombia.

出版信息

PeerJ. 2023 Apr 12;11:e15057. doi: 10.7717/peerj.15057. eCollection 2023.

DOI:10.7717/peerj.15057
PMID:37070090
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC10105559/
Abstract

Coral reef decline is an issue of concern around the globe. Remote and uninhabited coral areas are not exempt from facing changes in species composition and functionality due to global drivers. Quitasueño is a remote atoll within the Seaflower Biosphere Reserve, in the Southwestern Caribbean Sea. To evaluate the current status of the coral reefs in Quitasueño we sampled 120 stations through Rapid Ecological Assessment and evaluated four stations through Planar Point Intercept to compare the current percent cover of benthic groups with previous studies in the area. We found pronounced changes in coral and macroalgae covers in time, and great conspicuousness of multiple conditions of deterioration along Quitasueño, including diseases, coral predation, and aggression and invasion of coral colonies by macroalgae and sponges. The reef ecosystem seems to be facing a phase shift, in which the benthic cover previously dominated by hard corals is currently dominated by fleshy macroalgae. It is essential to evaluate the possible drivers of the extent of degradation of Quitasueño to understand the process of deterioration and mitigate the impacts.

摘要

珊瑚礁衰退是一个全球性关注的问题。由于全球驱动因素的影响,偏远和无人居住的珊瑚区域也不能免除物种组成和功能变化的影响。Quitasueno 是加勒比海南部海花生物保护区内的一个偏远环礁。为了评估 Quitasueño 珊瑚礁的现状,我们通过快速生态评估对 120 个站点进行了采样,并通过平面点截距对 4 个站点进行了评估,以比较当前底栖生物组的覆盖率与该地区以前的研究。我们发现,珊瑚和大型藻类的覆盖在时间上发生了明显变化,而且 Quitasueño 出现了多种恶化情况,包括疾病、珊瑚捕食、珊瑚群落被藻类和海绵侵袭和侵占等,情况非常明显。珊瑚礁生态系统似乎正在经历一个阶段转变,以前由硬珊瑚主导的底栖覆盖物目前由肉质大型藻类主导。评估 Quitasueño 退化程度的可能驱动因素至关重要,以便了解恶化过程并减轻其影响。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1030/10105559/c513224be41d/peerj-11-15057-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1030/10105559/7763952a840d/peerj-11-15057-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1030/10105559/2c5f3eb90fff/peerj-11-15057-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1030/10105559/4ed8a8290709/peerj-11-15057-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1030/10105559/5759df8a75c0/peerj-11-15057-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1030/10105559/c513224be41d/peerj-11-15057-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1030/10105559/7763952a840d/peerj-11-15057-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1030/10105559/2c5f3eb90fff/peerj-11-15057-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1030/10105559/4ed8a8290709/peerj-11-15057-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1030/10105559/5759df8a75c0/peerj-11-15057-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1030/10105559/c513224be41d/peerj-11-15057-g005.jpg

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本文引用的文献

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R Soc Open Sci. 2019 Oct 23;6(10):190298. doi: 10.1098/rsos.190298. eCollection 2019 Oct.
2
Long-term impacts of rising sea temperature and sea level on shallow water coral communities over a ~40 year period.在大约 40 年的时间里,海水温度和海平面上升对浅水珊瑚群落的长期影响。
Sci Rep. 2019 Jun 19;9(1):8826. doi: 10.1038/s41598-019-45188-x.
3
Loss of coral reef growth capacity to track future increases in sea level.
沿热带沿海生态系统水温与浊度梯度,底栖生物群落优势种的转变。
PeerJ. 2024 Apr 22;12:e17132. doi: 10.7717/peerj.17132. eCollection 2024.
珊瑚礁生长能力丧失,无法跟踪未来海平面的上升。
Nature. 2018 Jun;558(7710):396-400. doi: 10.1038/s41586-018-0194-z. Epub 2018 Jun 14.
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Local Stressors, Resilience, and Shifting Baselines on Coral Reefs.珊瑚礁上的局部压力源、恢复力和移动基线
PLoS One. 2016 Nov 30;11(11):e0166319. doi: 10.1371/journal.pone.0166319. eCollection 2016.
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Assessing evidence of phase shifts from coral to macroalgal dominance on coral reefs.评估珊瑚礁上从珊瑚主导转变为大型藻类主导的相移证据。
Ecology. 2009 Jun;90(6):1478-84. doi: 10.1890/08-1781.1.
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