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红海北部模式珊瑚石珊瑚浅水区和深水区群体之间固氮的季节对比响应。

Contrasting seasonal responses in dinitrogen fixation between shallow and deep-water colonies of the model coral Stylophora pistillata in the northern Red Sea.

机构信息

Coral Reef Ecology Group, Leibniz Centre for Tropical Marine Research (ZMT), Bremen, Germany.

Marine Department, Centre Scientifique de Monaco, Principality of Monaco.

出版信息

PLoS One. 2018 Jun 14;13(6):e0199022. doi: 10.1371/journal.pone.0199022. eCollection 2018.

DOI:10.1371/journal.pone.0199022
PMID:29902263
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC6002246/
Abstract

Tropical corals are often associated with dinitrogen (N2)-fixing bacteria (diazotrophs), and seasonal changes in key environmental parameters, such as dissolved inorganic nitrogen (DIN) availability and seawater temperature, are known to affect N2 fixation in coral-microbial holobionts. Despite, then, such potential for seasonal and depth-related changes in N2 fixation in reef corals, such variation has not yet been investigated. Therefore, this study quantified seasonal (winter vs. summer) N2 fixation rates associated with the reef-building coral Stylophora pistillata collected from depths of 5, 10 and 20 m in the northern Gulf of Aqaba (Red Sea). Findings revealed that corals from all depths exhibited the highest N2 fixation rates during the oligotrophic summer season, when up to 11% of their photo-metabolic nitrogen demand (CPND) could be met by N2 fixation. While N2 fixation remained seasonally stable for deep corals (20 m), it significantly decreased for the shallow corals (5 and 10 m) during the DIN-enriched winter season, accounting for less than 2% of the corals' CPND. This contrasting seasonal response in N2 fixation across corals of different depths could be driven by 1) release rates of coral-derived organic matter, 2) the community composition of the associated diazotrophs, and/or 3) nutrient acquisition by the Symbiodinium community.

摘要

热带珊瑚通常与固氮细菌(固氮生物)相关联,而关键环境参数(如溶解无机氮(DIN)的可利用性和海水温度)的季节性变化已知会影响珊瑚微生物共生体中的固氮作用。尽管珊瑚中的固氮作用存在季节性和深度相关的变化潜力,但这种变化尚未得到研究。因此,本研究定量了从亚喀巴湾北部(红海) 5、10 和 20 米深处采集的造礁珊瑚石珊瑚(Stylophora pistillata)的季节性(冬季与夏季)固氮速率。研究结果表明,所有深度的珊瑚在贫营养的夏季表现出最高的固氮速率,此时高达 11%的光代谢氮需求(CPND)可以通过固氮来满足。虽然深层珊瑚(20 米)的固氮作用在季节上保持稳定,但在富含 DIN 的冬季,浅层珊瑚(5 和 10 米)的固氮作用显著下降,仅占珊瑚 CPND 的不到 2%。不同深度的珊瑚在固氮作用上的这种相反的季节性响应可能是由以下因素驱动的:1)珊瑚源有机质的释放率,2)相关固氮生物的群落组成,和/或 3)共生体对营养物质的获取。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/46f8/6002246/53c25cd5e575/pone.0199022.g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/46f8/6002246/a7de1d8dd471/pone.0199022.g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/46f8/6002246/53c25cd5e575/pone.0199022.g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/46f8/6002246/a7de1d8dd471/pone.0199022.g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/46f8/6002246/53c25cd5e575/pone.0199022.g002.jpg

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