中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Estimates of late Early Cretaceous atmospheric CO2 from Mongolia based on stomatal and isotopic analysis of Pseudotorellia

文献类型:期刊论文

作者Zhang, Xiaoqing6,7; Royer, Dana L.7; Shi, Gongle6; Ichinnorov, Niiden5; Herendeen, Patrick S.4; Crane, Peter R.2,3; Herrera, Fabiany1
刊名AMERICAN JOURNAL OF BOTANY
出版日期2024-07-01
卷号111期号:7页码:11
关键词Albian Aptian fossil leaf cuticle Ginkgoales leaf-gas exchange model paleoclimate paleo-CO2 proxy
ISSN号0002-9122
DOI10.1002/ajb2.16376
通讯作者Zhang, Xiaoqing(xzhang04@wesleyan.edu)
英文摘要Premise: The Aptian-Albian (121.4-100.5 Ma) was a greenhouse period with global temperatures estimated as 10-15 degrees C warmer than pre-industrial conditions, so it is surprising that the most reliable CO2 estimates from this time are <1400 ppm. This low CO2 during a warm period implies a very high Earth-system sensitivity in the range of 6 to 9 degrees C per CO2 doubling between the Aptian-Albian and today. Methods: We applied a well-vetted paleo-CO2 proxy based on leaf gas-exchange principles (Franks model) to two Pseudotorellia species from three stratigraphically similar samples at the Tevshiin Govi lignite mine in central Mongolia (similar to 119.7-100.5 Ma). Results: Our median estimated CO2 concentration from the three respective samples was 2132, 2405, and 2770 ppm. The primary reason for the high estimated CO2 but with relatively large uncertainties is the very low stomatal density in both species, where small variations propagate to large changes in estimated CO2. Indeed, we found that at least 15 leaves are required before the aggregate estimated CO2 approaches that of the full data set. Conclusions: Our three CO2 estimates all exceeded 2000 ppm, translating to an Earth-system sensitivity (similar to 3-5 degrees C/CO2 doubling) that is more in keeping with the current understanding of the long-term climate system. Because of our large sample size, the directly measured inputs did not contribute much to the overall uncertainty in estimated CO2; instead, the inferred inputs were responsible for most of the overall uncertainty and thus should be scrutinized for their value choices.
WOS关键词SP-NOV ; EVOLUTION ; CUPRESSACEAE ; TEMPERATURE ; SENSITIVITY ; PINACEAE ; CLIMATE ; RECORD ; LEAVES ; EARTH
资助项目National Science Foundation of USA[NSF 20-509] ; National Natural Science Foundation of China[NSFC 42202024] ; Natural Science Foundation of Jiangsu Province, China[BK20221160] ; National Geographic Society[EC-96755R-22]
WOS研究方向Plant Sciences
语种英语
WOS记录号WOS:001274859500003
出版者WILEY
资助机构National Science Foundation of USA ; National Natural Science Foundation of China ; Natural Science Foundation of Jiangsu Province, China ; National Geographic Society
源URL[http://ir.nigpas.ac.cn/handle/332004/44094]  
专题中国科学院南京地质古生物研究所
通讯作者Zhang, Xiaoqing
作者单位1.Field Museum, Negaunee Integrat Res Ctr, Sci & Educ, Chicago, IL 60605 USA
2.Yale Univ, Yale Sch Environm, New Haven, CT 06511 USA
3.Oak Spring Garden Fdn, Upperville, VA 20184 USA
4.Chicago Bot Garden, Chicago, IL 60022 USA
5.Mongolian Acad Sci, Inst Paleontol, Ulaanbaatar 15160, Mongolia
6.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, State Key Lab Palaeobiol & Stratig, Nanjing 210008, Peoples R China
7.Wesleyan Univ, Dept Earth & Environm Sci, 265 Church St, Middletown, CT 06459 USA
推荐引用方式
GB/T 7714
Zhang, Xiaoqing,Royer, Dana L.,Shi, Gongle,et al. Estimates of late Early Cretaceous atmospheric CO2 from Mongolia based on stomatal and isotopic analysis of Pseudotorellia[J]. AMERICAN JOURNAL OF BOTANY,2024,111(7):11.
APA Zhang, Xiaoqing.,Royer, Dana L..,Shi, Gongle.,Ichinnorov, Niiden.,Herendeen, Patrick S..,...&Herrera, Fabiany.(2024).Estimates of late Early Cretaceous atmospheric CO2 from Mongolia based on stomatal and isotopic analysis of Pseudotorellia.AMERICAN JOURNAL OF BOTANY,111(7),11.
MLA Zhang, Xiaoqing,et al."Estimates of late Early Cretaceous atmospheric CO2 from Mongolia based on stomatal and isotopic analysis of Pseudotorellia".AMERICAN JOURNAL OF BOTANY 111.7(2024):11.

入库方式: OAI收割

来源:南京地质古生物研究所

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