中新世晚期的降温对印度洋-太平洋中部珊瑚礁消失的影响

IF 3.8 2区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
Benjamin Fredericks Petrick, Lars Reuning, Miriam Pfeiffer, Gerald Auer, Lorenz Schwark
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引用次数: 0

摘要

摘要晚中新世降温(LMC)被认为是气候记录中的一个全球性事件,并被认为是现代生态系统的开始。虽然现代陆地生态系统的变化发生在 7.0 - 5.5 Ma 全球范围内,但人们对水生生态系统的变化知之甚少。尤其是浅水碳酸盐生态系统,如珊瑚礁,几乎没有良好的替代记录。在中印度洋-太平洋地区的上新世,存在着一个 "珊瑚礁缺口",即在梅西尼期(7 - 5 Ma)出现的珊瑚礁在上新世早期(5 - 3 Ma)被淹没。在此,我们展示了珊瑚海基于 TEX86H 的海表温度(SST)记录,表明 LMC 比以前认为的更为明显。在LMC期间,ODP 811站点的海表温度下降了约2 °C,降温从7 Ma持续到可能的5 Ma。这种程度的降温也出现在印度洋-太平洋中部的其他地区。以前的研究表明,整个中印度洋-太平洋地区的珊瑚礁经历了一次重大的生态系统变化,导致珊瑚礁在 5 Ma 前崩溃。这一事件导致上新世期间珊瑚礁的缺乏,这一事件经常被描述为 "上新世珊瑚礁缺口"。这一事件发生的时间与记录中的降温时间相吻合。这表明,LMC 是导致珊瑚礁崩溃的最终压力源,因此也是造成 "上新世珊瑚礁缺口 "的潜在原因。相对快速和强烈的海温变化以及与降温相关的其他压力因素导致整个中印度洋-太平洋地区的珊瑚礁系统崩溃。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Impact of the Late Miocene Cooling on the loss of coral reefs in the Central Indo-Pacific
Abstract. The Late Miocene Cooling (LMC) has been recognized as a global event in the climate record and posited as the start of modern ecosystems. Whereas shifts in modern terrestrial ecosystems around 7.0 – 5.5 Ma occur globally, little is known about changes in aquatic ecosystems. This is especially true of shallow water carbonate ecosystems, such as coral reefs, where few good proxy records exist. A “reef gap” existed during the Pliocene in the area of the Central Indo-Pacific, where reefs that had been present during the Messinian (7 – 5 Ma) drowned by the Early Pliocene (5 – 3 Ma). Here, we present a TEX86H-based sea surface temperature (SST) record for the Coral Sea, suggesting that the LMC was more pronounced than previously thought. During the LMC, the SSTs at ODP Site 811 declined by about 2 °C, and cooling lasted from 7 Ma to possibly as late as 5 Ma. This level of cooling has also been seen in other parts of the Central Indo-Pacific. Previous research showed that coral reefs across the Central Indo-Pacific experienced a major ecosystem change, leading to the collapse of the coral reefs by 5 Ma. This event led to a lack of coral reefs during the Pliocene, an event that has often been described as the “Pliocene reef gap.” The timing of the onset of this event matches the cooling in the records. This suggests that the LMC was a final stressor that provided a regional driver for the collapse of reefs and, therefore, a potential cause for the “Pliocene Coral Gap.” The relatively rapid and intense change in SST and other stressors associated with the cooling caused coral reef systems to collapse across the Central Indo-Pacific.
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来源期刊
Climate of The Past
Climate of The Past 地学-气象与大气科学
CiteScore
7.40
自引率
14.00%
发文量
120
审稿时长
4-8 weeks
期刊介绍: Climate of the Past (CP) is a not-for-profit international scientific journal dedicated to the publication and discussion of research articles, short communications, and review papers on the climate history of the Earth. CP covers all temporal scales of climate change and variability, from geological time through to multidecadal studies of the last century. Studies focusing mainly on present and future climate are not within scope. The main subject areas are the following: reconstructions of past climate based on instrumental and historical data as well as proxy data from marine and terrestrial (including ice) archives; development and validation of new proxies, improvements of the precision and accuracy of proxy data; theoretical and empirical studies of processes in and feedback mechanisms between all climate system components in relation to past climate change on all space scales and timescales; simulation of past climate and model-based interpretation of palaeoclimate data for a better understanding of present and future climate variability and climate change.
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