Quaternary coral, coralline algal and vermetid assemblages as sea-level indicators: a review

J. Braga, M. Humblet, Dino A. Ramos, B. Dechnik, J. Webster
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Abstract

Corals, coralline algae and vermetid gastropods are indirect (marine limiting) relative sea-level (RSL) indicators. The precision in sea-level reconstruction based on fossils of those organisms depends on the probable palaeodepth in which they grew. Constraining such palaeodepth depends, in turn, on the available information about the habitats of their living counterparts. Diverse genera, species and species assemblages of corals, coralline algae and vermetid gastropods have historically been proposed as reliable indicators of narrow, shallow depth ranges. However, the increased information on depth distribution of marine benthos in the last two decades has challenged some early assumptions about depth ranges of taxa considered diagnostic of precise palaeodepths. Here, the authors test the reliability of coral, coralline algal and vermetid assemblages that have been extensively used in RSL reconstructions in the light of data from Ocean Biogeographical Information System (OBIS) and other recently published data. In the Indo-Pacific province, these data support the use of the robust-branching and the shallow, high-energy encrusting coral assemblages with a 0 to 10 m uncertainty. In both cases many component species have unimodal distributions and both median and average water depths are shallower than 10 m. The reliability of these coral assemblages as indicative of shallow water depths is strengthened when corals are encrusted by thick plants of the coralline alga Porolithon gr. onkodes. According to OBIS data, coralline algae of this species group in the Indo-Pacific are restricted to very shallow waters (95% probability of occurrence shallower than 0.2 m and in 99.6% of records shallower than 6 m). However, such a narrow depth range and the overall scarce data on coralline algal species in the OBIS database are questionable due to difficulties of coralline algal species identification with the naked eye. A comprehensive survey of the modern distribution of coralline algae at One Tree Reef (southern Great Barrier Reef) indicates that P. gr. onkodes has a log-normal distribution with median depth of less than 5 m and 95% of occurrence probability of thick crusts (> 0.2 mm) shallower than 8.8 m. Data on modern distribution of vermetids are scarce. In the OBIS database, vermetid species are reported from relatively wide depth ranges. However, relatively high densities (> 10 individuals per m2) on coral and coralline algal surfaces only occur from above mean low tide to some 6 m depth. In the Western Atlantic-Caribbean province Acropora palmata is the most precise RSL marker and no additional components of fossil assemblages improve its palaeodepth information. The confident use of coralgal and vermetid assemblages as RSL indicators relies on the identification of fossil corals and coralline algae at the species or species-group level. The scarcity of available data highlights the need for further studies on distribution of coralline algal species and vermetid in modern coral reefs from a variety of oceans and reef settings.
第四纪珊瑚、珊瑚藻和蚓类组合作为海平面指示物的研究进展
珊瑚、珊瑚藻和蛭形腹足类动物是间接(海洋限制)相对海平面(RSL)指标。基于这些生物化石重建海平面的精确度取决于它们生长的可能古深度。反过来,限制这样的古深度取决于现有的与之相对应的生物栖息地的信息。珊瑚、珊瑚藻类和蛭形腹足类的不同属、种和种组合历来被认为是狭窄、浅的深度范围的可靠指标。然而,近二十年来海洋底栖生物深度分布信息的增加,挑战了一些早期关于分类群深度范围的假设,这些假设被认为是精确古深度的诊断。在这里,作者根据海洋生物地理信息系统(OBIS)的数据和其他最近发表的数据,测试了在RSL重建中广泛使用的珊瑚、珊瑚藻和顶点生物组合的可靠性。在印度-太平洋省,这些数据支持使用坚固分支和浅层高能量的外壳珊瑚组合,具有0到10米的不确定性。在这两种情况下,许多组分都具有单峰分布,中位水深和平均水深都小于10米。当珊瑚被厚厚的珊瑚藻(Porolithon gr. onkodes)覆盖时,这些珊瑚组合作为浅水深度指示物的可靠性就得到了加强。根据OBIS的数据,该物种群在印度太平洋的珊瑚藻仅限于非常浅的水域(95%的概率出现在0.2米以下,99.6%的记录出现在6米以下)。然而,由于OBIS数据库中珊瑚藻的深度范围太窄,而且总体上缺乏珊瑚藻物种的数据,因此肉眼很难识别珊瑚藻物种,这是值得怀疑的。对大堡礁南部One Tree Reef珊瑚藻现代分布的综合调查表明,P. gr. onkodes呈对数正态分布,中位深度小于5 m,厚壳(> 0.2 mm)的出现概率为95%,厚度小于8.8 m。关于蚓类昆虫现代分布的资料很少。在OBIS数据库中,vermetid物种被报道的深度范围相对较宽。然而,珊瑚和珊瑚藻表面的相对高密度(每平方米约10只)只出现在平均低潮以上至约6米深度的地方。在西大西洋-加勒比省,Acropora palmata是最精确的RSL标志,没有其他化石组合成分可以改善其古深度信息。将珊瑚和蛭体组合作为RSL指标的可靠使用,依赖于在物种或物种群水平上对珊瑚化石和珊瑚藻的鉴定。现有数据的缺乏突出表明需要进一步研究来自各种海洋和珊瑚礁环境的现代珊瑚礁中的珊瑚藻和蛭体物种的分布。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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