稳定碳同位素在评价南大西洋罗卡斯环礁珊瑚Porites astreoides (Lamarck, 1816)生长速率中的应用

A. Santos, N. S. Pereira, A. N. Sial
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引用次数: 0

摘要

珊瑚礁经常被用作气候研究的自然档案。这些生物有能力将地球化学数据整合到外骨骼中,外骨骼可以用作不同环境变量的代理。在这项工作中,在南大西洋Rocas环礁收集的一个蛇床虫(PTM-1)珊瑚群落的不同部分使用了多种碳稳定同位素谱(δC)。该方法旨在验证该方法作为评估硬骨珊瑚群珊瑚生长率的替代方法的有效性。这种方法是基于珊瑚δC根据光度(即云量)而变化的想法,光度呈现季节性变化,并在珊瑚中记录年度周期。因此,每个同位素循环的长度与珊瑚的生长速度相对应。在这项工作中,进行了4个采样分辨率为0.5mm的同位素剖面。δC循环用于评估PTM-1集落的生长速率。δC周期的长度沿剖面从3到12毫米不等,该菌落的总体平均生长速率估计为6.69±2.39毫米/年,与该物种在其他物种中的生长速率接近。区域,表明该方法在评估珊瑚生长率方面的有效性。
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Aplicação de isótopos estáveis de carbono na avaliação da taxa de crescimento do coral Porites astreoides (Lamarck, 1816) do Atol das Rocas - Atlântico Sul
Corals are often used as natural archives for climate research. These organisms have the ability to incorporate geochemical data into their exoskeletons, which can be used as proxies for different environmental variables. In this work, multiple carbon stable isotope profiles (δC) were used in different sections of a Porites astreoides (PTM-1) coral colony, collected at Rocas Atoll South Atlantic. This approach aims to verify the effectiveness of this method as an alternative for the evaluation of coral growth rate of the Scleractinia group. Such method is based on the idea that the coral δC varies according to the luminosity (i.e. cloud cover), which presents seasonal variability and leave the annual cycles recorded in the corals. Thus, the length of each isotopic cycle corresponds to the growth rate of a coral. In this work, 4 isotopic profiles with 0.5 mm sampling resolution were carried out. The δC cycles were used to evaluate the growth rate of the PTM-1 colony. The length of the δC cycles varied from 3 to 12 mm along the profiles and the overall average growth rate estimated for this colony was 6.69 ± 2.39 mm/year, close to those reported for this species in other species. regions, indicating the effectiveness of this method in assessing coral growth rate.
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