过去 1900 年间亚马逊河流域内格罗河阿纳维勒哈纳斯群岛一个湖泊的碳储量、碳积累率和颗粒分布情况

Vanessa Cunha Silva, Keila Aniceto, Caroline Rocha Maia, Renato Campello Cordeiro, P. Moreira-Turcq, Luciane Silva Moreira, Christian J. Sanders, Humberto Marotta, B. Turcq
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引用次数: 0

摘要

最近的研究表明,尽管变化很大,但亚马逊流域的湖泊系统在积累和储存有机碳(TOC)方面取得了重大成果。然而,该地区的示范作用仍然有限,缺乏更多数据来更好地估算该地区的非碳成分。本文旨在估算位于下内格罗河地区 Anavilhanas 群岛的一个亚马逊湖的碳储量、碳积累率和颗粒分布特征。数据采集采用了 14C 方法,并对 1 米深的沉积物岩芯样本的密度、颗粒度和总有机碳速率进行了分析。结果表明,在公元前 1900 年期间,博托湖出现了两次孤立的沙粒沉积高峰,可能与重大水动力事件有关。总体而言,湖泊环境的特征非常明显,主要是细粉砂和粘土颗粒的沉积。在大约公元前 1900 年至公元前 850 年期间,沉积速率为 0.03 厘米/年-¹,公元前 850 年后为 0.07 厘米/年-¹。据估计,波托湖在整个时期积累的 TOC 储量约为 231,000 吨。据估计,亚马逊河流域土壤的总有机碳存量并不多。这些结果是阿纳维勒哈纳斯群岛作为总有机碳汇发挥作用的重要标志。
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CARBON STOCK, RATES OF CARBON ACCUMULATION AND DISTRIBUTION OF PARTICLES IN A LAKE OF THE ANAVILHANAS ARCHIPELAGO, NEGRO RIVER - AMAZON DURING THE LAST 1900 YEARS
Recent studies show that, despite great variability, the lake systems of the Amazon Basin have presented significant results in the accumulation and storage of organic carbon (TOC). However, the demonstration in the region is still limited and lacks more data to better estimate this non-carbon component of the region. The objective of this article was to estimate the carbon stock, the carbon accumulation rates and characterize the granulometric distribution of an Amazonian lake located in the Anavilhanas Archipelago, in the Lower Negro River region. Data were carried out using the 14C method and analyses of density, granulometry and TOC rate sof samples of a sediment core 1 meter deep. The results have shown that, during the period of 1900 cal years BP, Lake Boto presented two isolated peaks of sand particle sedimentation possibly related to major hydrodynamic events. Generally, well-defined characteristics of a lacustrine environment with sedimentation of fine silt and clay particles predominate. The sedimentation rate was 0.03 cm.year-¹ between approximately 1900 to 850 cal years BP and 0.07 cm.year-¹ in the last 850 cal years BP. It is estimated that Lake Boto has a stock of approximately 231,000 tons of TOC accumulated during the entire period. The stock of TOC is not significant as it is estimated for the soils of the Amazon. The results are an important indication of the role of the Anavilhanas Archipelago as a TOC sink.
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