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地貌控制下的西加勒比海退化浅礁区珊瑚分布

Geomorphically controlled coral distribution in degraded shallow reefs of the Western Caribbean.

机构信息

Posgrado en Ciencias del Mar y Limnología, Universidad Nacional Autónoma de México, Coyoacán, Ciudad de México, Mexico.

Reef Geoscience Group, Unidad Académica de Sistemas Arrecifales Instituto de Ciencias de Mar y Limnología, Universidad Nacional Autónoma de México, Puerto Morelos, Quintana Roo, Mexico.

出版信息

PeerJ. 2022 Mar 14;10:e12590. doi: 10.7717/peerj.12590. eCollection 2022.

Abstract

The development of coral reefs results from the interaction between ecological and geological processes in space and time. Their difference in scale, however, makes it difficult to detect the impact of ecological changes on geological reef development. The decline of coral cover over the last 50 years, for example, has dramatically impaired the function of ecological processes on reefs. Yet given the limited-resolution of their Holocene record, it is uncertain how this will impact accretion and structural integrity over longer timescales. In addition, reports of this ecological decline have focused on intrinsic parameters such as coral cover and colony size at the expense of extrinsic ones such as geomorphic and environmental variables. Despite these problems, several attempts have been made to predict the long-term accretion status of reefs based entirely on the contemporary health status of benthic communities. Here we explore how this ecological decline is represented within the reef geomorphic structure, which represents the long-term expression of reef development. Using a detailed geomorphic zonation scheme, we analyze the distribution and biodiversity of reef-building corals in fringing-reef systems of the Mesoamerican Reef tract. We find a depth-related pattern in community structure which shows that the relative species distribution between geomorphic zones is statistically different. Despite these differences, contemporary coral assemblages in all zones are dominated by the same group of pioneer generalist species. These findings imply that first, coral species distribution is still controlled by extrinsic processes that generate the geomorphic zonation; second, that coral biodiversity still reflects species zonation patterns reported by early studies; and third that dominance of pioneer species implies that modern coral assemblages are in a prolonged post-disturbance adjustment stage. In conclusion, any accurate assessment of the future viability of reefs requires a consideration of the geomorphic context or risks miscalculating the impact of ecological changes on long-term reef development.

摘要

珊瑚礁的发展是生态和地质过程在时空上相互作用的结果。然而,由于它们在规模上的差异,很难检测到生态变化对地质礁发展的影响。例如,过去 50 年来珊瑚覆盖率的下降,极大地削弱了生态过程在珊瑚礁上的功能。然而,由于其全新世记录的分辨率有限,尚不确定这将如何影响更长时间尺度上的堆积和结构完整性。此外,关于这种生态衰退的报告主要集中在珊瑚覆盖率和群体大小等内在参数上,而忽略了地貌和环境变量等外在参数。尽管存在这些问题,但已经有几次尝试完全基于底栖生物群落的当代健康状况来预测珊瑚礁的长期堆积状况。在这里,我们探讨了这种生态衰退是如何在代表珊瑚礁发展长期表现的礁体地貌结构中体现出来的。我们使用详细的地貌分区方案,分析了中美洲珊瑚礁带边缘礁系统中造礁珊瑚的分布和生物多样性。我们发现群落结构存在与深度相关的模式,表明地貌区之间的相对物种分布在统计学上是不同的。尽管存在这些差异,但所有区带的当代珊瑚组合都由同一组先锋广义物种主导。这些发现意味着,第一,珊瑚物种的分布仍然受到产生地貌分区的外在过程的控制;第二,珊瑚生物多样性仍然反映了早期研究报告的物种分区模式;第三,先锋物种的主导地位意味着现代珊瑚组合正处于长期的灾后调整阶段。总之,任何对珊瑚礁未来生存能力的准确评估都需要考虑地貌背景,否则可能会错误估计生态变化对长期珊瑚礁发展的影响。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b5de/8929170/d08fe59361b4/peerj-10-12590-g001.jpg

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