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Water, plants, and early human habitats in eastern Africa

机译:东非的水,植物和早期人类栖息地

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Water and its influence on plants likely exerted strong adaptive pressures in human evolution. Understanding relationships among water, plants, and early humans is limited both by incomplete terrestrial records of environmental change and by indirect proxy data for water availability. Here we present a continuous record of stable hydrogen-isotope compositions (expressed as SD values) for lipid biomarkers preserved in lake sediments from an early Pleistocene archaeological site in eastern Africa-Olduvai Gorge. We convert sedimentary leaf- and algal-lipid 6D values into estimates for ancient source-water 8D values by accounting for biochemical, physiological, and environmental influences on isotopic fraction-ation via published water-lipid enrichment factors for living plants, algae, and recent sediments. Reconstructed precipitation and lake-water 8D values, respectively, are consistent with modern isotopic hydrology and reveal that dramatic fluctuations in water availability accompanied ecosystem changes. Drier, conditions, indicated by less negative 8D values, occur in association with stable carbon-isotopic evidence for open, C_4-dominated grassland ecosystems. Wetter conditions, indicated by lower δD values, are associated with expanded woody cover across the ancient landscape. Estimates for ancient precipitation amounts, based on reconstructed precipitation SD values, range between approximately 250 and 700 mm-y~(-1) and are consistent with modern precipitation data for eastern Africa. We conclude that freshwater availability exerted a substantial influence on eastern African ecosystems and, by extension, was central to early human proliferation during periods of rapid climate change.
机译:水及其对植物的影响可能会在人类进化中施加强大的适应压力。陆地,环境变化的不完整记录以及水资源的间接替代数据,都限制了对水,植物和早期人类之间关系的理解。在这里,我们呈现了非洲东部-奥德维盖峡谷早期更新世考古遗址湖泊沉积物中保存的脂质生物标记物的稳定氢同位素组成(以SD值表示)的连续记录。通过考虑生物化学,生理和环境对同位素分馏作用的影响,我们通过已发表的活植物,藻类和最近的水脂富集因子,将沉积的叶和藻类脂类6D值转换为古代水源8D值的估计值沉积物。重建后的降水量和湖泊水的8D值分别与现代同位素水文学相一致,并揭示了水的可利用量的剧烈波动伴随着生态系统的变化。较少的8D负值表示较干燥的状况,并伴随着稳定的碳同位素证据表明开放的C_4为主的草地生态系统。较低的δD值表示的潮湿条件与整个古代景观中木质覆盖物的扩展有关。根据重建的降水SD值估算的古代降水量约为250至700 mm-y〜(-1),与东部非洲的现代降水数据一致。我们得出的结论是,淡水的可利用量对东部非洲的生态系统产生了重大影响,因此,在快速的气候变化时期,淡水的供应对于人类早期扩散至关重要。

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