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在退化的混浊珊瑚礁系统上的壳状珊瑚藻的生长和碳酸盐生产。

Growth and carbonate production of crustose coralline algae on a degraded turbid reef system.

机构信息

Department of Biological Sciences, National University of Singapore, 117543, Singapore.

Department of Biological Sciences, National University of Singapore, 117543, Singapore.

出版信息

Mar Pollut Bull. 2021 Dec;173(Pt B):113135. doi: 10.1016/j.marpolbul.2021.113135. Epub 2021 Nov 19.

DOI:10.1016/j.marpolbul.2021.113135
PMID:34801889
Abstract

Crustose coralline algae (CCA) and other encrusting calcifiers drive carbonate production on coral reefs. However, little is known about the rates of growth and calcification of these organisms within degraded turbid reef systems. Here we deployed settlement cards (N = 764) across seven reefs in Singapore for two years to examine spatio-temporal variation in encrusting community composition and CCA carbonate production. Our results showed that CCA was the dominant encrusting taxa (63.7% ± 18.3SD) across reefs. CCA carbonate production rates (0.009-0.052 g cm yr) were less than half of those reported for most Indo-Pacific reefs, but similar to other turbid reef systems. Highest CCA carbonate production rates were observed furthest from Singapore's main shipping port, due to a relative increase in CCA cover on the offshore reefs. Our results suggest that proximity to areas of high industrialisation and ship traffic may reduce the cover of encrusting calcifying organisms and CCA production rates which may have negative, long-term implications for the stabilisation of nearshore reefs in urbanised settings.

摘要

有孔虫珊瑚(CCA)和其他附生钙化生物驱动着珊瑚礁的碳酸盐产生。然而,对于退化浑浊的珊瑚礁系统中这些生物的生长和钙化速度,我们知之甚少。在这里,我们在新加坡的七个珊瑚礁上部署了沉降卡(N=764)两年,以研究附生群落组成和 CCA 碳酸盐产生的时空变化。我们的结果表明,CCA 是各珊瑚礁上的主要附生类群(63.7%±18.3SD)。CCA 碳酸盐产生速率(0.009-0.052 g cm yr)不到大多数印度洋-太平洋珊瑚礁报道的一半,但与其他浑浊的珊瑚礁系统相似。由于离新加坡主要航运港口越远的近海珊瑚礁上 CCA 覆盖率相对增加,因此观察到最高的 CCA 碳酸盐产生速率。我们的结果表明,接近高工业化和船舶交通区域可能会降低附生钙化生物的覆盖率和 CCA 产生速率,这可能对城市化地区近岸珊瑚礁的稳定产生长期的负面影响。

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