|
|
|
| Precipitation Changes during the Early Holocene and Middle Holocene Implicated by Exogenetic Detrital Mineral Changes in Huahai Lake, Hexi Corridor of NW China |
| Li Zhuolun, Wang Naiang, Li Yu, Cheng Hongyi, Chen Qing |
| College of Earth and Environmental Sciences/Center for Climatic Change and Hydrologic Cycle in Arid Region, Lanzhou University, Lanzhou 730000, China |
|
|
|
|
Abstract Huahai Lake, located in the western part of Hexi Corridor, NW China, is a key research area for Holocene environmental changes on millennial timescales in a monsoon-westerly transition area. Based on exogenetic detrital mineral, we reconstructed precipitation changes in Huahai Lake area, Hexi Corridor of NW China during the early Holocene (10.47-8.87 cal ka BP) and the middle Holocene (8.87-5.5 cal ka BP). Results show that during early Holocene the amount of exogenetic detrital mineral was higher than that in the middle Holocene, and then it indicated that precipitation during the early Holocene was higher than that in the middle Holocene. Moreover, higher precipitation in the early Holocene was mainly controlled by strong Indian Monsoon, precipitation changes could have been affected by westerly winds that could have contributed to the water vapor supply to this region during the middle Holocene. The most humid conditions that occurred in the study area during the middle Holocene may have been caused by strong westerlies and low levels of evaporation.
|
|
Received: 30 October 2013
Published: 20 November 2014
|
|
|
| [1] Li Y,Wang N A,Cheng H Y,et al.Holocene environmental change in the marginal area of the Asian monsoon:a record from Zhuye Lake,NW China[J].Boreas,2009,38:349-361.[2] Long H,Lai Z P,Wang N A,et al.Holocene climate variations from Zhuyeze terminal lake records in East Asian monsoon margin in arid northern China[J].Quaternary Research,2010,74:46-56.[3] Zhang H C,Ma Y Z,Wünnemann B,et al.A Holocene climatic record from arid northwestern China[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2000,162:389-401.[4] 王乃昂,李卓仑,李育,等.河西走廊花海剖面晚冰期以来年代学及沉积特征研究[J].沉积学报,2011,29(3):552-560.[5] Fleitmann D,Burns S J,Mudelsee M,et al.Holocene forcing of the Indian Monsoon recorded in a stalagmite from Southern Oman[J].Science,2003,300:1737-1739.[6] Morrill C,Overpeck J T,Cole J E,et al.Holocene variations in the Asian monsoon inferred from the geochemistry of lake sediments in central Tibet[J].Quaternary Research,2006,65:232-243.[7] Opitz S,Wünnemann B,Aichner B,et al.Late Glacial and Holocene development of Lake Donggi Cona,north-eastern Tibetan Plateau,inferred from sedimentological analysis[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2012,337/338:159-176.[8] Wang Y J,Cheng H,Edwards R L,et al.The Holocene Asian monsoon:links to solar changes and North Atlantic climate[J].Science,2005,308:854-857.[9] Chen F H,Yu Z C,Yang M L,et al.Holocene moisture evolution in arid central Asia and its out-of-phase relationship with Asian monsoon history[J].Quaternary Science Reviews,2008,27:351-364.[10] 蒋庆丰,沈吉,刘兴起,等.西风区全新世以来湖泊沉积记录的高分辨率古气候演化[J].科学通报,2007,52(9):1042-1049.[11] 陶士臣,安成邦,陈发虎,等.孢粉记录的新疆巴里坤湖16.7 cal ka BP以来的植被与环境[J].科学通报,2010,55(11):1026-1035.[12] Wang N A,Li Z L,Li Y,et al.Younger Dryas event recorded by the mirabilite deposition in Huahai lake,Hexi Corridor,NW China[J].Quaternary International,2012,250:93-99.[13] 王可丽,江灏,赵红岩.中国西北地区水汽的平流输送和辐合输送[J].水科学进展,2006,17(2):164-169.[14] 胡刚,王乃昂,高顺尉,等.花海湖泊全新世古风成砂的发现及其古环境解释[J].中国沙漠,2002,22(2):63-69.[15] 胡刚,王乃昂,罗建育,等.花海湖泊古风成砂的粒度特征及其环境意义[J].沉积学报,2001,19(4):642-647.[16] 李卓仑,陈晴,王乃昂,等.河西走廊花海古湖泊全新世白云石的发现及其环境意义[J].湖泊科学,2013,25(4):330-334.[17] 陈曦.中国干旱区自然地理[M].北京:科学出版社,2010:93-105.[18] 姚波,刘兴起,王永波,等.可可西里库赛湖KS-2006孔矿物组成揭示的青藏高原北部晚全新世气候变迁[J].湖泊科学,2011,23(6):903-909.[19] 张世涛,宋学良,张子雄,等.星云湖表层沉积物矿物组成及其环境意义[J].地球科学进展,2003,18(6):928-932.[20] 金章东.湖泊沉积物的矿物组成、成因、环境指示及研究进展[J].地球科学与环境学报,2011,33(1):34-44.[21] 侯新花,吴艳宏,杨丽原.全新世镜泊湖粒度特征记录的该地区古降水变化历史[J].湖泊科学,2006,18(6):605-614.[22] Chen C T,Lan H C,Lou J Y,et al.The dry Holocene megathermal in Inner Mongolia[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2003,193:181-200.[23] Sun D,Bloemenda J,Rea D K,et al.Grain-size distribution function of polymodal sediments in hydraulic and aeolian environments,and numerical partitioning of the sedimentary components[J].Sedimentary Geology,2002,152:263-277.[24] 宁凯,李卓仑,王乃昂,等.巴丹吉林沙漠地表风积砂粒度空间分布及其环境意义[J].中国沙漠,2013,33(3):642-648.[25] 靳建辉,曹相东,李志忠,等.艾比湖周边灌丛沙堆风沙沉积记录的气候环境演化[J].中国沙漠,2013,33(5):1314-1323.[26] 黄银洲,王乃昂,程弘毅,等.毛乌素沙地历史时期沙漠化——基于北大池湖泊周边沉积剖面粒度的研究[J].中国沙漠,2013,33(2):426-432.[27] Wang N A,Li Z L,Li Y,et al.Millennial-scale environmental changes in the Asian monsoon margin during the Holocene,implicated by the lake evolution of Huahai Lake in the Hexi Corridor of northwest China[J].Quaternary International,2013,313-314:100-109.[28] Deckker P D,Corrège T,Head J.Late Pleistocene record of cyclic eolian activity from tropical Australia suggesting the Younger Dryas is not an unusual climatic event[J].Geology,1991,19:602-605.[29] 李卓仑,王乃昂,李育,等.近50年来黑河出山径流对气候变化的响应[J].水土保持通报,2012,32(2):7-11,16.[30] 马宏伟,王乃昂,李卓仑.近50年石羊河流域气候变化的R/S分析[J].兰州大学学报(自然科学版),2010,46(4):42-45,57.[31] 李卓仑,张乃梦,王乃昂,等.晚冰期以来河西走廊花海古湖泊演化过程及其对气候变化的响应[J].中国沙漠,2014,34(2):342-348.[32] Zhang J W,Chen F H,Holmes J A,et al.Holocene monsoon climate documented by oxygen and carbon isotopes from lake sediments and peat bogs in China:a review and synthesis[J].Quaternary Science Reviews,2011,30:1973-1987.[33] Dykoski C A,Edwardsa R L,Cheng H.A high-resolution,abso-lute-dated Holocene and deglacial Asian monsoon record from Dongge Cave,China[J].Earth Planet Science Letter,2005,233:71-86.[34] 董进国,孔兴功,汪永进.神农架全新世东亚季风演化及其热带辐合带控制[J].第四纪研究,2006,26(5):827-834.[35] 刘兴起,沈吉,王苏民,等.晚冰期以来青海湖地区气候变迁受西南季风控制的介形类壳体氧同位素证据[J].科学通报,2006,51(22):2690-2694.[36] Gupta A K,Anderson D M,Overpeck J T.Abrupt changes in the Asian southwest monsoon during the Holocene and their links to the North Atlantic Ocean[J].Nature,2003,421:354-357.[37] Vandenberghe J,Renssen H,Huissteden K,et al.Penetration of Atlantic westerly winds into central and East Asia[J].Quaternary Science Reviews,2006,25:2380-2389.[38] 李卓仑,王乃昂,李育等.河西走廊花海古湖泊早、中全新世湖水盐度变化及其环境意义[J].冰川冻土,2013,35(6):1481-1489.[39] Zhang H C,Peng J L,Ma Y Z,et al.Late Quaternary palaeolake levels in Tengger Desert,NW China[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2004,211:45-58.[40] 王乃昂,李卓仑,程弘毅,等.阿拉善高原晚第四纪高湖面与大湖期的再探讨[J].科学通报,2011,56(17):1367-1377.[41] Li Y,Morrill C.Multiple factors causing Holocene lake-level change in monsoonal and arid central Asia as identified by model experiments[J].Climate Dynamics,2010,35:1119-1132.[42] 李育,李卓仑,王乃昂.蒸发和环流因素对湖泊演化的影响——河西走廊猪野泽不同位置全新世沉积物古环境意义探讨[J].湖泊科学,2012,24(3):474-479. |
| No Suggested Reading articles found! |
|
|
Viewed |
|
|
|
Full text
|
|
|
|
|
Abstract
|
|
|
|
|
Cited |
|
|
|
|
| |
Shared |
|
|
|
|
| |
Discussed |
|
|
|
|
2014, Vol. 34 
