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在近期海洋变暖的情况下,耐热共生体的优势增加,从而使珊瑚礁具有更强的恢复力。

Increased dominance of heat-tolerant symbionts creates resilient coral reefs in near-term ocean warming.

机构信息

Department of Marine Biology and Ecology, Rosenstiel School of Marine, Atmospheric, and Earth Science, University of Miami, Miami, FL 33149.

Cooperative Institute for Marine and Atmospheric Studies, Rosenstiel School of Marine and Atmospheric Science, University of Miami, Miami, FL 33149.

出版信息

Proc Natl Acad Sci U S A. 2023 Feb 21;120(8):e2202388120. doi: 10.1073/pnas.2202388120. Epub 2023 Feb 13.

DOI:10.1073/pnas.2202388120
PMID:36780524
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC9974440/
Abstract

Climate change is radically altering coral reef ecosystems, mainly through increasingly frequent and severe bleaching events. Yet, some reefs have exhibited higher thermal tolerance after bleaching severely the first time. To understand changes in thermal tolerance in the eastern tropical Pacific (ETP), we compiled four decades of temperature, coral cover, coral bleaching, and mortality data, including three mass bleaching events during the 1982 to 1983, 1997 to 1998 and 2015 to 2016 El Niño heatwaves. Higher heat resistance in later bleaching events was detected in the dominant framework-building genus, while other coral taxa exhibited similar susceptibility across events. Genetic analyses of spp colonies and their algal symbionts (2014 to 2016) revealed that one of two lineages present in the region (type 1") increased its association with thermotolerant algal symbionts () during the 2015 to 2016 heat stress event. This lineage experienced lower bleaching and mortality compared with "type 3", which did not acquire . Under projected thermal stress, ETP reefs may be able to preserve high coral cover through the 2060s or later, mainly composed of colonies that associate with . However, although the low-diversity, high-cover reefs of the ETP could illustrate a potential functional state for some future reefs, this state may only be temporary unless global greenhouse gas emissions and resultant global warming are curtailed.

摘要

气候变化正在彻底改变珊瑚礁生态系统,主要是通过越来越频繁和严重的白化事件。然而,一些珊瑚礁在第一次严重白化后表现出更高的耐热性。为了了解东热带太平洋(ETP)热耐受性的变化,我们汇编了四十年来的温度、珊瑚覆盖率、珊瑚白化和死亡率数据,其中包括 1982 年至 1983 年、1997 年至 1998 年和 2015 年至 2016 年厄尔尼诺热浪期间的三次大规模白化事件。在后来的白化事件中,占主导地位的造礁属的耐热性更高,而其他珊瑚类群在各次事件中的易感性相似。对 spp 群体及其共生藻(2014 年至 2016 年)的遗传分析表明,在该地区存在的两个谱系之一(“type 1”)在 2015 年至 2016 年的热胁迫事件中增加了与耐热共生藻()的关联。与“type 3”相比,该谱系经历的白化和死亡率较低,“type 3”没有获得 。在预计的热胁迫下,ETP 珊瑚礁可能能够在 2060 年代或以后保持高珊瑚覆盖率,主要由与 共生的 群体组成。然而,尽管 ETP 的低多样性、高覆盖率的珊瑚礁可能代表了一些未来珊瑚礁的潜在功能状态,但这种状态可能只是暂时的,除非全球温室气体排放和由此产生的全球变暖得到遏制。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c85d/9974440/f0d1e23d666f/pnas.2202388120fig05.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c85d/9974440/017677af2ffb/pnas.2202388120fig01.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c85d/9974440/b5c2410062da/pnas.2202388120fig02.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c85d/9974440/e9501dbebcbc/pnas.2202388120fig03.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c85d/9974440/69529a1d79c1/pnas.2202388120fig04.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c85d/9974440/f0d1e23d666f/pnas.2202388120fig05.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c85d/9974440/017677af2ffb/pnas.2202388120fig01.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c85d/9974440/b5c2410062da/pnas.2202388120fig02.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c85d/9974440/e9501dbebcbc/pnas.2202388120fig03.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c85d/9974440/69529a1d79c1/pnas.2202388120fig04.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c85d/9974440/f0d1e23d666f/pnas.2202388120fig05.jpg

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