From Corals to Canyons: The Great Barrier Reef Margin
From Corals to Canyons: The Great Barrier Reef Margin
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从珊瑚到峡谷：大堡礁边缘
DOI：
10.1029/2008eo240002
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发表时间：
2011
期刊：
影响因子：
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通讯作者：
Webster J
中科院分区：
文献类型：
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作者：
Webster J
在加勒比海[费尔班克斯，1989年]和印度太平洋（见Montaggioni [2005]摘要）的调查以及最近在塔希提岛的综合大洋钻探计划（IODP）活动[Camoin等人，2007年]。沿着沿着大堡礁（GBR）的边缘保存着类似的淹没（40-130米）珊瑚礁结构，但尚未对其进行系统研究。淹没珊瑚礁有可能提供关于过去全球海平面和气候变化的性质以及GBR对这些过去和未来环境变化的响应的关键新信息[Beaman等人，2008年]。对于GBR海洋公园管理者来说，同样重要的是有关珊瑚礁作为现代生物群落栖息地和基质的作用的信息。
The significance of submerged fossil coral reefs as important archives of abrupt global sea level rise and climate change has been confirmed by investigations in the Caribbean [Fairbanks, 1989] and the Indo‐ Pacific (seeMontaggioni[2005] for a summary) and by recent Integrated Ocean Drilling Program (IODP) activities in Tahiti [Camoin et al., 2007]. Similar submerged (40–130 meters) reef structures are preserved along the margin of the Great Barrier Reef (GBR), but they have not yet been systematically studied.The submerged reefs have the potential to provide critical new information about the nature of past global sea level and climate variability and about the response of the GBR to these past and perhaps future environmental changes [Beaman et al., 2008]. Equally important for GBR Marine Park managers is information about the role of the reefs as habitats and substrates for modern biological communities.
DOI：
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发表时间：
2007
期刊：
影响因子：
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作者：
Principal Investigators;J. Webster;P. Davies;R. Beaman;Stefan B. Williams;M. Byrne
通讯作者：
M. Byrne