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首页> 外文期刊>Palaeontology >Establishing temperate crustose early Holocene coralline algae as archives for palaeoenvironmental reconstructions of the shallow water habitats of the Mediterranean Sea
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Establishing temperate crustose early Holocene coralline algae as archives for palaeoenvironmental reconstructions of the shallow water habitats of the Mediterranean Sea

机译:建立温带蛋黄早期全茂珊瑚藻类作为地中海浅水栖息地的古环境重建档案

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摘要

Over the past decades, coralline algae have increasingly been used as archives of palaeoclimate information due to their seasonal growth bands and their vast distribution from high latitudes to the tropics. Traditionally, these reconstructions have been performed mainly on high latitude species, limiting the geographical area of their potential use. Here we assess the use of temperate crustose fossil coralline algae from shallow water habitats for palaeoenvironmental reconstruction to generate records of past climate change. We determine the potential of three different species of coralline algae, Lithothamnion minervae, Lithophyllum stictaeforme and Mesophyllum philippii, with different growth patterns, as archives for pH (delta B-11) and temperature (Mg/Ca) reconstruction in the Mediterranean Sea. Mg concentration is driven by temperature but modulated by growth rate, which is controlled by species-specific and intraspecific growth patterns. L. minervae is a good temperature recorder, showing a moderate warming trend in specimens from 11.37 cal ka BP (from 14.2 +/- 0.4 degrees C to 14.9 +/- 0.15 degrees C) to today. In contrast to Mg, all genera showed consistent values of boron isotopes (delta B-11) suggesting a common control on boron incorporation. The recorded delta B-11 in modern and fossil coralline specimens is in agreement with literature data about early Holocene pH, opening new perspectives of coralline-based, high-resolution pH reconstructions in deep time.
机译:在过去的几十年中,由于他们的季节性增长乐队以及从高纬度到热带地区的广泛分布,珊瑚藻类越来越多地被用作古藏信息的档案。传统上,这些重建主要是在高纬度物种上进行的,限制了它们潜在使用的地理区域。在这里,我们评估使用温带瘢痕疙瘩从浅水栖息地进行古环境重建的浅水栖息地,以产生过去的气候变化的记录。我们确定三种不同种类的珊瑚藻类,锂疗法Minervae,Lithothyllum Stictaeforme和培养的菲利普利的潜力,具有不同的生长模式,作为地中海的pH(delta b-11)和温度(mg / ca)重建的档案。 Mg浓度由温度驱动,但通过生长速率调节,该生长速率由物种特异性和内部增长模式控制。 L. Minervae是一种良好的温度记录仪,显示出今天的11.37只Cal Ka BP的标本温暖趋势(从14.2 +/- 0.4摄氏度为14.9 +/- 0.15摄氏度)。与Mg相比,所有属均显示硼同位素(Delta B-11)的一致值,表明硼掺入的常见控制。现代和化石珊瑚标本中的记录ΔB-11与关于早期全茂性pH的文献数据一致,在深度时间内开启基于珊瑚的高分辨率的pH重建的新观点。

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