The Holocene temperature conundrum answered by mollusk records from East Asia

被引：88
作者：
Dong, Yajie [1 ,2 ,3 ]
Wu, Naiqin [1 ]
Li, Fengjiang [1 ,2 ,3 ]
Zhang, Dan [1 ,4 ]
Zhang, Yueting [1 ,4 ]
Shen, Caiming [5 ]
Lu, Houyuan [1 ,4 ]
机构：
[1] Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing 100029, Peoples R China
[2] Chinese Acad Sci, Innovat Acad Earth Sci, Beijing 100029, Peoples R China
[3] Chinese Acad Sci, Ctr Excellence Life & Paleoenvironm, Beijing 100044, Peoples R China
[4] Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China
[5] Yunnan Normal Univ, Fac Geog, Yunnan Key Lab Plateau Geog Proc & Environm Chang, Kunming 650500, Yunnan, Peoples R China
来源：
NATURE COMMUNICATIONS | 2022年 / 13卷 / 01期
基金：
中国国家自然科学基金;
关键词：
SYNERGISTIC FEEDBACKS; SPECIES-DIVERSITY; LOESS SEQUENCE; CLIMATE; RECONSTRUCTION; VEGETATION; CHINA; DYNAMICS; PLATEAU; EUROPE;
D O I：
10.1038/s41467-022-32506-7
中图分类号：
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号：
07 ; 0710 ; 09 ;
摘要：
Seasonal biases (the warm-season contribution) of Holocene mean annual temperature (MAT) reconstructions from geological records were proposed as a possible cause of the mismatch with climate simulated temperature. Here we analyze terrestrial mollusk assemblages that best reflect seasonal signals and provide quantitative MAT and four-season temperature records for northern China during the past 20,000 years. The MAT estimated from the seasonal temperatures of a four-season-mean based on mollusks shows a peak during -9000-4000 years ago, followed by a cooling trend. In general, the contribution of summer and winter temperature to MAT is significantly greater than that of spring and autumn temperatures. The relative contribution of each season varies over time and corresponds roughly with the seasonal insolation in each season. This independent evidence from mollusk records from the mid-latitudes of East Asia does not support the Holocene long-term warming trend observed in climate simulations and the seasonal bias explanation.
引用
收藏
页数：9
相关论文
共 76 条
[1]   Central Europe temperature constrained by speleothem fluid inclusion water isotopes over the past 14,000 years [J].
Affolter, Stephane ;
Hauselmann, Anamaria ;
Fleitmann, Dominik ;
Edwards, R. Lawrence ;
Cheng, Hai ;
Leuenberger, Markus .
SCIENCE ADVANCES, 2019, 5 (06)
[2]   Rapid environmental changes in southern Europe during the last glacial period [J].
Allen, JRM ;
Brandt, U ;
Brauer, A ;
Hubberten, HW ;
Huntley, B ;
Keller, J ;
Kraml, M ;
Mackensen, A ;
Mingram, J ;
Negendank, JFW ;
Nowaczyk, NR ;
Oberhänsli, H ;
Watts, WA ;
Wulf, S ;
Zolitschka, B .
NATURE, 1999, 400 (6746) :740-743
[3]  
[Anonymous], 1999, Geochimica, DOI DOI 10.19700/J.0379-1726.1999.03.008
[4]   Global temperature modes shed light on the Holocene temperature conundrum [J].
Bader, Juergen ;
Jungclaus, Johann ;
Krivova, Natalie ;
Lorenz, Stephan ;
Maycock, Amanda ;
Raddatz, Thomas ;
Schmidt, Hauke ;
Toohey, Matthew ;
Wu, Chi-Ju ;
Claussen, Martin .
NATURE COMMUNICATIONS, 2020, 11 (01)
[5]  
Baker JL, 2017, NAT GEOSCI, V10, P430, DOI [10.1038/ngeo2953, 10.1038/NGEO2953]
[6]  
Birks H., 2012, Tracking Environmental Change Using Lake Sediments, vol. 5. Data Handling and Numerical Techniques, DOI [DOI 10.1007/978-94-007-2745-8, 10.1007/978-94-007-2745-8]
[7]   Seasonal origin of the thermal maxima at the Holocene and the last interglacial [J].
Bova, Samantha ;
Rosenthal, Yair ;
Liu, Zhengyu ;
Godad, Shital P. ;
Yan, Mi .
NATURE, 2021, 589 (7843) :548-+
[8]  
Braak C. J. F., 2012, CANOCO Reference Manual and User's Guide: Software Ordination (Version 5.0)
[9]   Synergistic feedbacks from ocean and vegetation on the African monsoon response to mid-Holocene insolation [J].
Braconnot, P ;
Joussaume, S ;
Marti, O ;
de Noblet, N .
GEOPHYSICAL RESEARCH LETTERS, 1999, 26 (16) :2481-2484
[10]   Evaluation of climate models using palaeoclimatic data [J].
Braconnot, Pascale ;
Harrison, Sandy P. ;
Kageyama, Masa ;
Bartlein, Patrick J. ;
Masson-Delmotte, Valerie ;
Abe-Ouchi, Ayako ;
Otto-Bliesner, Bette ;
Zhao, Yan .
NATURE CLIMATE CHANGE, 2012, 2 (06) :417-424
12345678