山西临汾盆地末次间冰期以来古气候变化研究
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摘要
临汾盆地位于鄂尔多斯台地的南部和东部边缘,该区域是我国新构造运动非常强烈的地区之一。以山西临汾盆地为着眼点进行研究,有利于从更广泛的、具有成因联系的区域整体上来认识青藏高原隆升及其环境效应这一重大科学问题,并且临汾盆地千伏村剖面记录了末次间冰期以来的气候变化,对揭示晋西南地区古气候变化的规律具有重要的意义。
自中更新世以来盆地中经历了多次的湖侵、湖退,沉积地层连续,形成了黄土-古土壤层与河湖相沉积层互层分布的现象,蕴藏了丰富的古气候变化的信息。本文通过对临汾盆地湖泊沉积物的磁化率、粒度、地球化学元素、有机质等多气候环境代用指标的数据处理与综合分析,对能够准确反映该区域古气候变化的代用指标进行了遴选。在此基础上,剖析了临汾盆地对全球气候变化信号的响应,揭示了临汾盆地末次冰期高时间分辨率的气候波动,初步建立了临汾盆地末次间冰期以来的古气候环境的演变过程与特征,为进一步讨论该时段中国中东部地区气候环境演变提供了类比材料。
根据对千伏东(QFD)湖相沉积剖面沉积特征描述以及对该剖面进行的磁化率、粒度、有机质含量、化学元素含量及比值等气候代用指标的数据处理与分析,确定将磁化率、<4μm粘土组分含量、4～63μm粉砂组分含量、中值粒径、有机质含量、Rb、Sr含量及其比值作为研究千伏村剖面的气候代用指标,并确定了其古气候指示意义。
根据多气候环境代用指标的对比分析与年代的内插推算,结合剖面的沉积特征,建立了临汾盆地末次间冰期以来沉积地层年代序列,并将千伏村剖面末次间冰期以来的沉积环境划分为五个阶段:即末次冰期早期阶段(L1L3)、末次冰期间冰段早期(L1S2)、末次冰期间冰段中期(L1L2)、末次冰期间冰段晚期(L1S1)、末次冰期晚期阶段(L1L1),同时得出临汾盆地千伏村剖面的气候经历了以下几个演化阶段:深度760-620cm(73～51.9kaB.P.)相对干冷的气候期;深度620～530cm(51.9～46.1kaB.P.)相对湿润的气候回暖期;深度530～300cm(46.1～28.9kaB.P)相对干冷气候期;深度300～220cm(28.9～22kaB.P)相对湿润的气候回暖期;深度220～0cm(22～10.3kaB.P.)经历了末次冰期最为干冷的冰盛期和后期逐渐回暖的冰消期。
受全球气候变化影响,千伏村剖面记录了末次冰期的一些千年尺度的全球性气候事件,包括16次暖事件和7次冷事件,初步推测16个暖事件为D-O事件在东亚季风区的体现,而7个冷事件为Heinrich事件H1～H6以及冰消期的YD事件的表现。
Linfen Basin is located in the southern and eastern edge of Ordos Massif; this region is one of the areas where neotectonic movement of our country is very strong. It is in favor of recognizing the major scientific issue that the regional uplift of the Tibetan Plateau and its environmental effects to focus research on Shanxi Linfen Basin from a more extensive contact with the causes of a whole region, and there is also of great significance to reveal the paleoclimate changes of southwest of Shanxi from the record since last Interglacial at Qianfu section of Linfen Basin.
Since Middle Pleistocene basin has experienced a number of lakes invaded the lake retreated, continuous sedimentary strata formed of loess-paleosol layers and layers of lake sediment distribution in each situation, and there has been abundant paleoclimate change information. Based on data processing and integrated analysis of Linfen Basin lake sediments in magnetic susceptibility, grain-size, geochemistry element, and organic matter, we picked out the paleoclimate proxies those be able to accurately reflect the region's paleoclimate change, and then analyzed the response to signal of global climate change in Linfen Basin, revealed the climate fluctuations of high temporal resolution in the last glacial, set up characters and process of the paleoclimatic evolvement in Linfen Basin since the last interglacial, and more provided a analogical material for further discussion of the evolution of climate and environment in the central and eastern region of China.
Based on sedimentological analysis of Qinfudong (QFD) section, data processing and integrated analysis of Linfen Basin lake sediments in magnetic susceptibility, grain-size, chemical element composition, and organic matter, we confirmed magnetic susceptibility, <4μm content of clay, 4～63μm content of silty sand, median grain-size, content of organic matter, Rb and Sr concentrations along with Rb/Sr ratio as climate proxies to study Qianfu section, and also determined its paleoclimatic significance.
According to the comparative analysis among climate Multi-proxy and interpolation during ages, combining with the sedimentological characteristics of section, time sequence since the last interglacial of Linfen Basin was established and divided into five stages: L1L3, L1S2, L1L2, L1S1 and L1L1. They are respectively corresponding to depth of 760～620cm (73～51.9kaB.P.), relatively arid and cold; 62～530cm (51.9～46.1kaB.P.), relatively worm and humid; 530～300cm(46.1～28.9kaB.P), relatively arid and cold;300～220cm(28.9～22kaB.P), relatively worm and humid; 220～0cm(22～10.3kaB.P.), worm and humid arid and cold by turns.
By the impact of global climate change, Qianfu section also recorded a number of millennium-scale climate events during the last glacial which performance of the global characteristics, including sixteen warm events and seven cold events which we inferred as sixteen Dansgaard-Oescheger events, six Heinrich events (H1～H6) and the Younger Dryas during the last deglacial.
自中更新世以来盆地中经历了多次的湖侵、湖退,沉积地层连续,形成了黄土-古土壤层与河湖相沉积层互层分布的现象,蕴藏了丰富的古气候变化的信息。本文通过对临汾盆地湖泊沉积物的磁化率、粒度、地球化学元素、有机质等多气候环境代用指标的数据处理与综合分析,对能够准确反映该区域古气候变化的代用指标进行了遴选。在此基础上,剖析了临汾盆地对全球气候变化信号的响应,揭示了临汾盆地末次冰期高时间分辨率的气候波动,初步建立了临汾盆地末次间冰期以来的古气候环境的演变过程与特征,为进一步讨论该时段中国中东部地区气候环境演变提供了类比材料。
根据对千伏东(QFD)湖相沉积剖面沉积特征描述以及对该剖面进行的磁化率、粒度、有机质含量、化学元素含量及比值等气候代用指标的数据处理与分析,确定将磁化率、<4μm粘土组分含量、4～63μm粉砂组分含量、中值粒径、有机质含量、Rb、Sr含量及其比值作为研究千伏村剖面的气候代用指标,并确定了其古气候指示意义。
根据多气候环境代用指标的对比分析与年代的内插推算,结合剖面的沉积特征,建立了临汾盆地末次间冰期以来沉积地层年代序列,并将千伏村剖面末次间冰期以来的沉积环境划分为五个阶段:即末次冰期早期阶段(L1L3)、末次冰期间冰段早期(L1S2)、末次冰期间冰段中期(L1L2)、末次冰期间冰段晚期(L1S1)、末次冰期晚期阶段(L1L1),同时得出临汾盆地千伏村剖面的气候经历了以下几个演化阶段:深度760-620cm(73～51.9kaB.P.)相对干冷的气候期;深度620～530cm(51.9～46.1kaB.P.)相对湿润的气候回暖期;深度530～300cm(46.1～28.9kaB.P)相对干冷气候期;深度300～220cm(28.9～22kaB.P)相对湿润的气候回暖期;深度220～0cm(22～10.3kaB.P.)经历了末次冰期最为干冷的冰盛期和后期逐渐回暖的冰消期。
受全球气候变化影响,千伏村剖面记录了末次冰期的一些千年尺度的全球性气候事件,包括16次暖事件和7次冷事件,初步推测16个暖事件为D-O事件在东亚季风区的体现,而7个冷事件为Heinrich事件H1～H6以及冰消期的YD事件的表现。
Linfen Basin is located in the southern and eastern edge of Ordos Massif; this region is one of the areas where neotectonic movement of our country is very strong. It is in favor of recognizing the major scientific issue that the regional uplift of the Tibetan Plateau and its environmental effects to focus research on Shanxi Linfen Basin from a more extensive contact with the causes of a whole region, and there is also of great significance to reveal the paleoclimate changes of southwest of Shanxi from the record since last Interglacial at Qianfu section of Linfen Basin.
Since Middle Pleistocene basin has experienced a number of lakes invaded the lake retreated, continuous sedimentary strata formed of loess-paleosol layers and layers of lake sediment distribution in each situation, and there has been abundant paleoclimate change information. Based on data processing and integrated analysis of Linfen Basin lake sediments in magnetic susceptibility, grain-size, geochemistry element, and organic matter, we picked out the paleoclimate proxies those be able to accurately reflect the region's paleoclimate change, and then analyzed the response to signal of global climate change in Linfen Basin, revealed the climate fluctuations of high temporal resolution in the last glacial, set up characters and process of the paleoclimatic evolvement in Linfen Basin since the last interglacial, and more provided a analogical material for further discussion of the evolution of climate and environment in the central and eastern region of China.
Based on sedimentological analysis of Qinfudong (QFD) section, data processing and integrated analysis of Linfen Basin lake sediments in magnetic susceptibility, grain-size, chemical element composition, and organic matter, we confirmed magnetic susceptibility, <4μm content of clay, 4～63μm content of silty sand, median grain-size, content of organic matter, Rb and Sr concentrations along with Rb/Sr ratio as climate proxies to study Qianfu section, and also determined its paleoclimatic significance.
According to the comparative analysis among climate Multi-proxy and interpolation during ages, combining with the sedimentological characteristics of section, time sequence since the last interglacial of Linfen Basin was established and divided into five stages: L1L3, L1S2, L1L2, L1S1 and L1L1. They are respectively corresponding to depth of 760～620cm (73～51.9kaB.P.), relatively arid and cold; 62～530cm (51.9～46.1kaB.P.), relatively worm and humid; 530～300cm(46.1～28.9kaB.P), relatively arid and cold;300～220cm(28.9～22kaB.P), relatively worm and humid; 220～0cm(22～10.3kaB.P.), worm and humid arid and cold by turns.
By the impact of global climate change, Qianfu section also recorded a number of millennium-scale climate events during the last glacial which performance of the global characteristics, including sixteen warm events and seven cold events which we inferred as sixteen Dansgaard-Oescheger events, six Heinrich events (H1～H6) and the Younger Dryas during the last deglacial.
引文
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