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首页> 外文期刊>Quaternary International >Rainfall variability and vegetation recovery in rocky desertification areas recorded in recently-deposited stalagmites from Guilin, South China
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Rainfall variability and vegetation recovery in rocky desertification areas recorded in recently-deposited stalagmites from Guilin, South China

机译:中国南方桂林最近沉积的石笋中石漠化地区的降雨变化和植被恢复

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摘要

An actively growing stalagmite (sample DY-2) from Maomaotou Big Cave in Guilin, south China was dated using a combined approach of Th-230/U, Pb-210 and AMS C-14 dating techniques. The post-bomb C-14 curve shows that the DY-2 was deposited during 1964-2009 CE and a fast growth rate of similar to 2.25 mm/a was determined for this 9.3 cm-long stalagmite. The Pb-210 dating of the top 7 mm part of another stalagmite sample PL4 from Panlong Cave located in the same area as the Maomaotou Big Cave constrained a depositional interval during 1830-2009 CE with a much slower growth rate of similar to 0.04 mm/a. The delta O-18 variations of DY-2 and PL4 are highly comparable on decadal time-scales within age uncertainties, and both reveal a good coherence with local instrumental rainfall and historic dry-wet index records. These two delta O-18 records suggest that rainfall variability in the region of Guilin is modulated by Pacific Decadal Oscillation (PDO) and El Nino-Southern Oscillation (ENSO), as the latter can affect the East Asian Summer Monsoon (EASM) and Western Pacific Subtropical High (WPSH). On annual-to-decadal scales, the increase of EASM intensity and WPSH as well as the shift of negative (cold) PDO and La Nina phases would enhance the summer rainfall in the Guilin region, as revealed by the lower stalagmite delta O-18 values. While weakening EASM and WPSH with positive (warm) PDO and El Nino phases tend to lead to a dry climate in this region of south China. In addition, the stalagmite delta C-13 and Dead Carbon Proportion (DCP) records show gradually decreasing trends over the last several decades. According to the findings of synchronous increase in both soil pCO(2) and dissolved inorganic carbon (DIC) concentrations in seepage waters from the area of Guilin, the variation of stalagmite delta C-13 and DCP may reflect a history of vegetation recovery in such a rocky desertification area like Guilin, where the area of rocky desertification has been reducing since the 1990s due to afforestation policies and measures.
机译:使用Th-230 / U,Pb-210和AMS C-14测年技术相结合的方法,对华南桂林毛茂头大洞中活跃的石笋(DY-2样品)进行了测年。炸弹爆炸后的C-14曲线表明,DY-2沉积于1964-2009年CE期间,对于这种9.3 cm长的石笋,其快速生长速率约为2.25 mm / a。铅龙石岩样品PL4顶部7毫米部分的Pb-210测年与茂茂头大洞位于同一区域,盘龙洞中的石笋样品限制了沉积间隔,在公元1830-2009年间,其生长速度慢得多,接近0.04毫米/一个。 DY-2和PL4的δO-18变化在年龄不确定性的年代际尺度上具有高度可比性,并且都显示出与当地仪器降雨和历史干湿指数记录的良好一致性。这两个O-18记录表明,桂林地区的降雨变化受太平洋年代际涛动(PDO)和厄尔尼诺-南方涛动(ENSO)的影响,因为后者会影响东亚夏季风(EASM)和西部太平洋副热带高压(WPSH)。从年际到十年的尺度上,EASM强度和WPSH的增加以及负(冷)PDO和La Nina相的移动将增加桂林地区的夏季降雨,这由较低的石笋三角洲O-18揭示。价值观。在PDO和El Nino正(暖)相减弱EASM和WPSH的同时,往往会导致该华南地区出现干旱气候。此外,石笋δC-13和死碳比例(DCP)记录显示,在过去的几十年中,这种趋势呈逐渐下降的趋势。根据桂林地区渗水中土壤pCO(2)和溶解性无机碳(DIC)浓度同步增加的发现,石笋δC-13和DCP的变化可能反映了植被恢复的历史。像桂林这样的石漠化地区,由于造林政策和措施,自1990年代以来石漠化面积一直在减少。

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