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Climate and human impact during the past 2000 years as recorded in the Lagunas de Yala, Jujuy, northwestern Argentina

机译:在阿根廷西北部胡胡伊的拉古纳斯·德·亚拉(Lagunas de Yala)记录的过去2000年中的气候和人类影响

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摘要

~(210)Pb, ~(137)Cs and ~(14)C dated sediments of two late Holocene landslide lakes in the Provincial Park Lagunas de Yala (Laguna Rodeo, Laguna Comedero, 24°06′S, 65°30′W, 2100m asl, northwestern Argentina) reveal a high-resolution multi-proxy data set of climate change and human impact for the past ca. 2000 years. Comparison of the lake sediment data set for the 20th century (sediment mass accumulation rates MARs, pollen spectra, nutrient and charcoal fluxes) with independent dendroecological data from the catchment (fire scars, tree growth) and long regional precipitation series (from 1934 onwards) show that (1) the lake sediment data set is internally highly consistent and compares well with independent data sets, (2) the chronology of the sediment is reliable, (3) large fires (1940s, 1983/ 1984-1989) as documented in the local fire scar frequency are recorded in the charcoal flux to the lake sediments and coincide with low wet-season precipitation rates (e.g., 1940s, 1983/1984) and/or high interannual precipitation variability (late 1940s), and (4) the regional increase in precipitation after 1970 is recorded in an increase in the MARs (L. Rodeo from 100 to 390 mg cm~(-2) yr~(-1)) and in an increase in fern spores reflecting wet vegetation. The most significant change in MARs and nutrient fluxes (C_(org) and P) of the past 2000 years is observed with the transition from the Inca Empire to the Spanish Conquest around 1600 AD. Compared with the pre-17th century conditions, MARs increased by a factor of ca. 5 to >8 (to 800_(+ 130, -280) mgcm~(-2)yr~(-1)), PO_4 fluxes increased by a factor of 7, and C_(org) fluxes by a factor of 10.5 for the time between 1640 and 1930 AD. 17th to 19th century MARs and nutrient fluxes also exceed 20th century values. Excess Pb deposition as indicated by a significant increase in Pb/Zr and Pb/Rb ratios in the sediments after the 1950s coincides with a rapid expansion of the regional mining industry. Excess Pb is interpreted as atmospheric deposition and direct human impact due to Pb smelting.
机译:〜Lagunas de Yala省公园(Laguna Rodeo,Laguna Comedero,南纬24°06′,西经65°30′′W)两个晚全新世滑坡湖的〜(210)Pb,〜(137)Cs和〜(14)C沉积物,位于阿根廷西北部2100m asl)揭示了过去约20年气候变化和人类影响的高分辨率多代理数据集。 2000年将20世纪的湖泊沉积物数据集(沉积物质量累积速率MARs,花粉光谱,养分和木炭通量)与来自集水区的独立树状生态学数据(火疤,树木生长)和较长的区域降水序列(从1934年开始)进行比较表明(1)湖泊沉积物数据集在内部具有高度一致性,并且与独立数据集具有很好的比较;(2)沉积物的时间顺序是可靠的;(3)大火(1940年代,1983 / 1984-1989),如当地的火疤频率记录在通向湖泊沉积物的木炭通量中,并且与湿季降水率较低(例如1940s,1983/1984)和/或年际降水变化较大(1940年代后期)相符,并且(4) 1970年后区域降水的增加记录为MARs(罗迪欧(L. Rodeo)从100 mg〜(-2)yr〜(-1)增加)和反映湿生植被的蕨类孢子的增加。在公元1600年左右从印加帝国到西班牙征服的过渡期间,观察到了过去2000年MAR和营养通量(C_(org)和P)的最大变化。与17世纪以前的情况相比,MAR的增加幅度约为ca。 5至> 8(至800 _(+ 130,-280)mgcm〜(-2)yr〜(-1)),PO_4通量增加7倍,C_(org)通量增加10.5 1640年至1930年之间的时间。 17至19世纪的MAR和营养通量也超过了20世纪的值。 1950年代后沉积物中Pb / Zr和Pb / Rb比值的显着增加表明了过量的Pb沉积,这与区域采矿业的迅速发展相吻合。过量的铅被解释为大气沉积,并且由于铅的熔炼而直接影响人类。

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