首页> 外文期刊>Journal of Human Evolution >Subdecadal phytolith and charcoal records from Lake Malawi, East Africa imply minimal effects on human evolution from the similar to 74 ka Toba supereruption
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Subdecadal phytolith and charcoal records from Lake Malawi, East Africa imply minimal effects on human evolution from the similar to 74 ka Toba supereruption

机译:来自马拉维湖的Subdecadal Phytolith和木炭记录,East Africa从类似于74 Ka Toba超硬化的人类演变的影响最小

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The temporal proximity of the similar to 74 ka Toba supereruption to a putative 100-50 ka human population bottleneck is the basis for the volcanic winter/weak Garden of Eden hypothesis, which states that the eruption caused a 6-year-long global volcanic winter and reduced the effective population of anatomically modern humans (AMH) to fewer than 10,000 individuals. To test this hypothesis, we sampled two cores collected from Lake Malawi with cryptotephra previously fingerprinted to the Toba supereruption. Phytolith and charcoal samples were continuously collected at similar to 3-4 mm (similar to 8-9 yr) intervals above and below the Toba cryptotephra position, with no stratigraphic breaks. For samples synchronous or proximal to the Toba interval, we found no change in low elevation tree cover, or in cool climate C-3 and warm season C-4 xerophytic and mesophytic grass abundance that is outside of normal variability. A spike in locally derived charcoal and xerophytic C-4 grasses immediately after the Toba eruption indicates reduced precipitation and die-off of at least some afromontane vegetation, but does not signal volcanic winter conditions. A review of Toba tuff petrological and melt inclusion studies suggest a Tambora-like 50 to 100 Mt SO2 atmospheric injection. However, most Toba climate models use SO2 values that are one to two orders of magnitude higher, thereby significantly overestimating the amount of cooling. A review of recent genetic studies finds no support for a genetic bottleneck at or near similar to 74 ka. Based on these previous studies and our new paleoenvironmental data, we find no support for the Toba catastrophe hypothesis and conclude that the Toba supereruption did not 1) produce a 6-year-long volcanic winter in eastern Africa, 2) cause a genetic bottleneck among African AMH populations, or 3) bring humanity to the brink of extinction. (C) 2017 Elsevier Ltd. All rights reserved.
机译:类似于74 kA Toba超硬于推定的100-50ka人口瓶颈的时间接近是伊甸假设的火山冬季/弱花园的基础,这导致爆发引起了一个6年长的全球火山冬季并降低了解剖学现代人类(AMH)的有效群体,以少于10,000人。为了测试这个假设,我们采样了从马拉维湖的两座核心,用Cryptotephra以前指纹对ToBA超级性。植物和木炭样品在托巴加密对象的位置和下方和下方类似于3-4毫米(类似于8-9毫升)间隔,没有地层突破。对于ToBA间隔同步或近端的样品,我们发现低升高树盖或凉爽的气候C-3和温暖的季节C-4异味和营养草本丰富的变化,超出正常变化。在ToBA喷发后立即在局部衍生的木炭和杂草型C-4草的刺激表明,至少一些Afromontane植被的降水和抑制减少,但不发挥火山冬季条件。对Toba Tuff型肉质和熔融包容性研究的综述表明Tambora样50至100 mt SO2大气注射。然而,大多数ToBA气候模型使用SO2值,这是一个到两个数量级的值,从而显着高估了冷却量。近期遗传研究的审查发现,对类似于74 ka的遗传瓶颈没有支持。基于这些先前的研究和我们的新的古环境数据,我们发现没有对ToBA灾难假设的支持,并得出结论,Toba Superultion没有1)在东非,2)产生一个6年长的火山冬季,2)导致遗传瓶颈非洲AMH人口或3)将人类带来了灭绝的边缘。 (c)2017 Elsevier Ltd.保留所有权利。

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