佛得角群岛第四纪珊瑚的系统学和古生物地理学

IF 1.7 3区 地球科学 Q3 GEOGRAPHY, PHYSICAL Quaternary Research Pub Date : 2024-05-20 DOI:10.1017/qua.2024.20
Anne-Sophie Reeb, A. Rebelo, Ricardo S. Ramalho, J. Madeira, M. Rasser
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引用次数: 0

摘要

虽然佛得角群岛的化石记录中很少有真正珊瑚礁的报道,但在这些岛屿的海啸沉积物和陆上隆起的海洋阶地中,可以发现许多单个珊瑚化石和珊瑚群。这项研究首次对群岛 10 个岛屿中 7 个岛屿的珊瑚化石进行了详细调查,样本来自更新世海洋阶地和海啸沉积物。共对 168 种硬骨鱼类珊瑚进行了分析和属和/或种的鉴定。共鉴定出 Acroporidae、Dendrophylliidae、Faviidae、Pocilloporidae、Poritidae 和 Rhizangiidae 科中的 13 个分类群。在佛得角群岛发现的变色珊瑚化石很可能是从加勒比海迁移到西非海岸的,而无色珊瑚物种很可能来自印度洋-太平洋。现今珊瑚群与化石群之间的差异被认为是环境因素变化造成的。虽然出现了造礁类群(如茯苓),但却没有广泛的珊瑚礁框架。
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Systematics and paleobiogeography of Quaternary corals from Cabo Verde Archipelago
Although true coral reefs have seldom been reported from the fossil record of the Cabo Verde Archipelago, many single fossil corals and coral colonies can be found reworked in tsunami deposits and in raised marine terraces onshore on these islands. This study provides the first detailed survey of fossil corals from 7 of the 10 islands of the archipelago, sampled from Pleistocene marine terraces and tsunami deposits. A total of 168 scleractinian corals were analyzed and identified to genus and/or species level. Thirteen taxa from the families Acroporidae, Dendrophylliidae, Faviidae, Pocilloporidae, Poritidae, and Rhizangiidae were identified. The zooxanthellate fossil corals found on the Cape Verde Archipelago likely migrated from the Caribbean to the West African coast, while azooxanthellate species likely originated from the Indo-Pacific. Differences between present-day coral assemblages and fossil assemblages are assumed to result from changing environmental factors. Although reef-building taxa occur (e.g., Porites), extensive reef frameworks are absent.
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来源期刊
Quaternary Research
Quaternary Research 地学-地球科学综合
CiteScore
4.70
自引率
8.70%
发文量
57
审稿时长
3 months
期刊介绍: Quaternary Research is an international journal devoted to the advancement of the interdisciplinary understanding of the Quaternary Period. We aim to publish articles of broad interest with relevance to more than one discipline, and that constitute a significant new contribution to Quaternary science. The journal’s scope is global, building on its nearly 50-year history in advancing the understanding of earth and human history through interdisciplinary study of the last 2.6 million years.
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