Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1016/j.palaeo.2020.110016 |
Decline of soil respiration in northeastern Tibet through the transition into the Oligocene icehouse | |
Licht, A.; Dupont-Nivet, G.; Meijer, N.; Rugenstein, J. Caves; Schauer, A.; Fiebig, J.; Mulch, A.; Hoorn, C.; Barbolini, N.; Guo, Z. | |
通讯作者 | Licht, A (corresponding author), Univ Washington, Dept Earth & Space Sci, Seattle, WA 98195 USA. |
来源期刊 | PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
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ISSN | 0031-0182 |
EISSN | 1872-616X |
出版年 | 2020 |
卷号 | 560 |
英文摘要 | Soil respiration (R-s), the production of carbon dioxide in soils, increases dramatically from deserts to forested ecosystems. R-s values thus provide a potential tool to identify past ecosystems if recorded in sedimentary archives. Here, we propose a quantitative method to reconstruct past R-s values from paleosols. This method reverses the soil paleobarometer, a proxy that estimates past atmospheric CO2 concentration values (CO2atm) from paleosols while considering a narrow range of variation for Rs. We use past CO2atm values from marine proxies to reconstruct soil respiration from a 20 million year-long isotopic record from northeastern Tibet covering the transition from the Eocene greenhouse to the Oligocene icehouse. We show that Rs dropped at least 4-fold through the transition into the Oligocene icehouse, marking the spread of boreal desert-steppes of Central Asia. We show that increasing aridity and the decline of monsoonal rainfall, in parallel with global cooling, caused the fall of soil respiration. These highly dynamic R-s emphasize the need for a systematic screening of paleosol isotopic data before using the soil paleobarometer to reconstruct CO2atm |
英文关键词 | Paleosol Paleoclimate Desertification Paleogene Atmospheric CO2 Monsoons |
类型 | Article |
语种 | 英语 |
开放获取类型 | Green Published |
收录类别 | SCI-E |
WOS记录号 | WOS:000591245000027 |
WOS关键词 | CLUMPED ISOTOPE GEOTHERMOMETER ; STABLE-ISOTOPE ; PEDOGENIC CARBONATE ; ORGANIC-MATTER ; XINING BASIN ; CO2 FLUX ; PLATEAU ; PRECIPITATION ; DIOXIDE ; CLIMATE |
WOS类目 | Geography, Physical ; Geosciences, Multidisciplinary ; Paleontology |
WOS研究方向 | Physical Geography ; Geology ; Paleontology |
来源机构 | 北京大学 ; Colorado State University ; E17 |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/349099 |
作者单位 | [Licht, A.; Schauer, A.] Univ Washington, Dept Earth & Space Sci, Seattle, WA 98195 USA; [Dupont-Nivet, G.; Meijer, N.] Univ Potsdam, Inst Geosci, D-14476 Potsdam, Germany; [Dupont-Nivet, G.] Univ Rennes, Geosci Rennes, UMR CNRS 6118, F-74205 Rennes, France; [Dupont-Nivet, G.; Guo, Z.] Peking Univ, Key Lab Orogen Belts & Crustal Evolut, Beijing 100871, Peoples R China; [Rugenstein, J. Caves] Max Planck Inst Meteorol, Bundesstr 53, D-21460 Hamburg, Germany; [Rugenstein, J. Caves; Mulch, A.] Senckenberg Biodivers & Climate Res Ctr, D-60325 Frankfurt, Germany; [Rugenstein, J. Caves] Colorado State Univ, Dept Geosci, Ft Collins, CO 80523 USA; [Fiebig, J.; Mulch, A.] Goethe Univ, Inst Geosci, D-60438 Frankfurt, Germany; [Hoorn, C.; Barbolini, N.] Univ Amsterdam, Inst Biodivers & Ecosyst Dynam, Dept Ecosyst & Landscape Dynam, NL-1098 XH Amsterdam, Netherlands; [Barbolini, N.] Stockholm Univ, Dept Ecol Environm & Plant Sci, SE-10691 Stockholm, Sweden; [Barbolini, N.] Stockholm Univ, Bolin Ctr Climate Res, SE-106... |
推荐引用方式 GB/T 7714 | Licht, A.,Dupont-Nivet, G.,Meijer, N.,et al. Decline of soil respiration in northeastern Tibet through the transition into the Oligocene icehouse[J]. 北京大学, Colorado State University, E17,2020,560. |
APA | Licht, A..,Dupont-Nivet, G..,Meijer, N..,Rugenstein, J. Caves.,Schauer, A..,...&Guo, Z..(2020).Decline of soil respiration in northeastern Tibet through the transition into the Oligocene icehouse.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,560. |
MLA | Licht, A.,et al."Decline of soil respiration in northeastern Tibet through the transition into the Oligocene icehouse".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 560(2020). |
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