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支链GDGTs与黄土古温度重建:机遇与挑战
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作者 卢红选 王欢业 +2 位作者 刘旭 盛维娟 刘卫国 《第四纪研究》 CAS CSCD 北大核心 2024年第5期1296-1307,共12页
目前对全球古温度的理解主要基于海洋记录,由于缺乏可靠的陆地古温度指标,对陆地温度变化的认识较为有限,这限制了对全球变暖背景下,陆地温度变化规律和机制的深入理解。支链甘油二烷基甘油四醚类化合物(brGDGTs)是某些细菌微生物细胞... 目前对全球古温度的理解主要基于海洋记录,由于缺乏可靠的陆地古温度指标,对陆地温度变化的认识较为有限,这限制了对全球变暖背景下,陆地温度变化规律和机制的深入理解。支链甘油二烷基甘油四醚类化合物(brGDGTs)是某些细菌微生物细胞脂膜中的四醚化合物,近20年来已成为广泛关注的陆地古温度计。该温度计一经推出,便在黄土古温度,特别是长时间尺度的古温度重建中发挥了重要作用。本研究首先回顾了brGDGTs温度计的发展历史,总结了近年来该温度计在细菌培养实验、现代过程调研、仪器分析方法、数据处理技术等方面的创新和进展。然后介绍了支链GDGTs在黄土古土壤剖面中不同时间尺度的古温度重建研究进展。黄土高原brGDGTs记录的陆地温度呈现明显的冰期-间冰期波动特征,表明太阳辐射和全球冰量对陆地温度变化重要的驱动作用;但与海洋温度相比,冰盛期-冰消期时段增温超前于海洋记录,推测陆地下垫面(植被、土壤湿度等)动态演化可能会对陆地温度变化起着重要的调控作用。最后多角度分析了brGDGTs陆地古温度重建面临的机遇和挑战。作为稀缺的陆地古温度计,brGDGTs为认识陆地温度变化规律和机制提供了难得的工具,但其确切生物来源、形成机制尚不明确。另外,全球黄土brGDGTs温度在变化趋势、周期和幅度上存在较大差异,且造成这种差异的原因还不清楚。为了应对这些挑战,应继续加强brGDGTs温度计的基础理论研究,明确其来源和形成机制,优化分析方法和校正模型。同时,结合现代观测和模拟研究,探究不同时间尺度下陆地下垫面(植被、土壤湿度等)与温度变化之间的反馈机制,进一步丰富我们对全球温度变化规律和机制的认识。 展开更多
关键词 brGDGTs 古温度 黄土 气候指标
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Distribution of branched glycerol dialkyl glycerol tetraethers in soils on the Northeastern Qinghai-Tibetan Plateau and possible production by nitrite-reducing bacteria 被引量:3
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作者 SUN ChiJun ZHANG ChuanLun +2 位作者 LI Fu Yan wang huanye LIU WeiGuo 《Science China Earth Sciences》 SCIE EI CAS CSCD 2016年第9期1834-1846,共13页
Branched glycerol dialkyl glycerol tetraethers (bGDGTs) are ubiquitous and abundant in soils, but their sources remain elusive. Recent studies demonstrate that the distributions of bGDGTs are sensitive to various en... Branched glycerol dialkyl glycerol tetraethers (bGDGTs) are ubiquitous and abundant in soils, but their sources remain elusive. Recent studies demonstrate that the distributions of bGDGTs are sensitive to various environmental factors. In an effort to understand how and to what extent soil moisture (expressed as soil water content (SWC) or mean annual precipita- tion (MAP), pH and temperature may impact the distribution of bGDGTs, and to shed more light on the biological sources of bGDGTs in cold and arid regions, we investigated the distribution of bGDGTs as well as bacterial 16S rRNA gene and func- tional genes involved in the N cycle (including amoA, nirS and nirK) in 41 surface soil samples from around Lake Qinghai and east of Qaidam Basin on the Northeastern Qinghai-Tibetan Plateau. We found that lower soil moisture reduced the fractional concentrations of cyclic bGDGTs and thus the cyclisation ratio of branched tetraethers (CBT) index correlated negatively with SWC and MAP, suggesting that soil moisture is an important factor controlling bGDGT distributions in soils in this add and semi-add region. Two subgroups of bGDGTs were assigned on the basis of cluster analysis, and bGDGT indices behaved dif- ferently in the two groups, hinting at different biosynthetic mechanisms for bGDGTs under different environmental conditions. Real time PCR results showed that nirS and nirK genes correlated significantly with the concentration of bGDGTs, suggesting that the nirS- or nirK-encoding bacteria involved in denitrification might potentially be an additional biological source for soil bGDGTs (besides Acidobacteria). Moreover, our results also support the application of new indices based on 5-methyl bGDGTs and 6-methyl bGDGTs in reconstructing past temperature and pH variations in this region. 展开更多
关键词 bGDGTs Soil water content CBT nirS- or nirK-encoding bacteria Real time PCR Cluster analysis
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Solar influenced late Holocene temperature changes on the northern Tibetan Plateau 被引量:12
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作者 HE YuXin LIU WeiGuo +7 位作者 ZHAO Cheng wang Zheng wang huanye LIU Yi QIN XianYan HU QiHou AN ZhiSheng LIU ZhongHui 《Chinese Science Bulletin》 SCIE EI CAS 2013年第9期1053-1059,共7页
Considerable efforts have been made to extend temperature records beyond the instrumental period through proxy reconstructions,in order to further understand the mechanisms of past climate variability.Yet,the global c... Considerable efforts have been made to extend temperature records beyond the instrumental period through proxy reconstructions,in order to further understand the mechanisms of past climate variability.Yet,the global coverage of existing temperature records is still limited,especially for some key regions like the Tibetan Plateau and for earlier times including the Medieval Warm Period(MWP).Here we present decadally-resolved,alkenone-based,temperature records from two lakes on the northern Tibetan Plateau.Characterized by marked temperature variability,our records provide evidence that temperatures during the MWP were slightly higher than the modern period in this region.Further,our temperature reconstructions,within age uncertainty,can be well correlated with solar irradiance changes,suggesting a possible link between solar forcing and natural climate variability,at least on the northern Tibetan Plateau. 展开更多
关键词 青藏高原北部 温度变化 晚全新世 太阳能 中世纪暖期 温度记录 气候变化 太阳辐照度
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A 12-kyr record of microbial branched and isoprenoid tetraether index in Lake Qinghai,northeastern Qinghai-Tibet Plateau:Implications for paleoclimate reconstruction 被引量:6
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作者 wang huanye DONG HaiLiang +2 位作者 ZHANG ChuanLun JIANG HongChen LIU WeiGuo 《Science China Earth Sciences》 SCIE EI CAS CSCD 2016年第5期951-960,共10页
Branched and Isoprenoid Tetraether(BIT) index was considered as a proxy for terrestrial organic matter input in lake sediments, based on the assumption that branched glycerol dialkyl glycerol tetraethers(b GDGTs) are ... Branched and Isoprenoid Tetraether(BIT) index was considered as a proxy for terrestrial organic matter input in lake sediments, based on the assumption that branched glycerol dialkyl glycerol tetraethers(b GDGTs) are mainly derived from terrestrial soils. However, mounting evidences have showed that the in situ production of b GDGTs is widespread in lakes, challenging BIT as a reliable terrestrial input proxy. Recently, BIT has been proven to be a reliable proxy for paleohydrology in a small crater lake(Lake Challa) in accordance with a different mechanism. However, the response of BIT to paleohydrology variation may differ for different lakes. In this study, we investigate the variations in the BIT index and the concentrations of its related GDGTs in a 12-ka sediment core from Lake Qinghai, in combination with our previous results for surface sediments. We find that variations in BIT strongly depend on the concentration of crenarchaeol in both surface and ancient sediments of this lake, whereas b GDGT concentration varies much less remarkably. Considering that crenarchaeol production is positively correlated with water depth in Lake Qinghai, water depth may exert negative control on the BIT index in this lake. This case is inconsistent with the positive relationship between BIT and lake levels or rainfall intensity reported for Lake Challa, suggesting that the response of BIT to local paleohydrology is site specific in lacustrine systems. Hence, the application of sedimentary BIT as a paleohydrological proxy in a specific lake requires caution before confirming the environmental controls on BIT in that lake. 展开更多
关键词 Lake Qinghai BIT lake water depth precipitation paleohydrology
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