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首页> 外文期刊>Radiocarbon >LATE PLEISTOCENE AND HOLOCENE VEGETATION, CLIMATE DYNAMICS, AND AMAZONIAN TAXA IN THE ATLANTIC FOREST, LINHARES, SE BRAZIL
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LATE PLEISTOCENE AND HOLOCENE VEGETATION, CLIMATE DYNAMICS, AND AMAZONIAN TAXA IN THE ATLANTIC FOREST, LINHARES, SE BRAZIL

机译:巴西林哈雷斯大西洋森林晚更新世和全新世植被,气候动力学和氨氮塔克萨

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摘要

Analysis of biological proxies in lake sediment and geochemical analysis of soil profiles reveal natural vegetation dynamics, with climate inferences, since the late Pleistocene in a fragment of the pristine lowland Atlantic Forest of southeastern Brazil. Carbon isotopes from soil organic matter and ~(14)C ages from the humin fraction indicate the dominance of C_3 plants since -17,000 cal BP. Palynological analysis of a sediment core indicates the presence of Atlantic Forest vegetation since 7700 cal BP. Changes in the relative abundance of tree ferns and palms suggest the predominance of a humid period from -7000-4000 cal BP and establishment of the modern seasonal climate at -4000 cal BP. Data indicate maintenance of the regional forest coverage since the late Pleistocene, corroborating previous suggestions that this region was a forest refuge during less humid periods of the late Pleistocene and Holocene. Some plant taxa with currently divided distributions between Amazonia and the Atlantic Forest colonized the region since at least 7500 cal BP, indicating an earlier connection between Amazonia and Atlantic Forest.
机译:自巴西东南部原始低地大西洋森林的一个更新世晚期以来,对湖泊沉积物中生物代理的分析和对土壤剖面的地球化学分析揭示了自然植被动态,并带有气候推断。土壤有机质的碳同位素和腐殖质部分的〜(14)C年龄表明自-17,000 cal BP以来C_3植物的优势。对沉积物芯的孢粉学分析表明,自7700 cal BP以来就有大西洋森林植被存在。树蕨和棕榈树相对丰度的变化表明-7000-4000 cal BP处于湿润时期,而-4000 cal BP则建立了现代季节性气候。数据表明,自晚更新世以来该地区的森林覆盖率得以维持,这证实了先前的建议,即该地区是晚更新世和全新世较不湿润时期的森林避难所。自至少7500 cal BP以来,亚马逊地区和大西洋森林之间的一些植物类目目前分布分散,这是该地区的殖民地,表明亚马逊地区和大西洋森林之间的联系较早。

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