中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
A latitudinal gradient of plant-insect interactions during the late Permian in terrestrial ecosystems? New evidence from Southwest China

文献类型:期刊论文

作者Liu, Hang-Yu4; Wei, Hai-Bo4; Chen, Jianbo4; Guo, Yun4; Zhou, Yu4; Gou, Xu-Dong4; Yang, Shi-Ling5,6,7; Labandeira, Conrad2,3,8; Feng, Zhuo1,4
刊名GLOBAL AND PLANETARY CHANGE
出版日期2020-09-01
卷号192页码:12
ISSN号0921-8181
关键词Insect damage type Terrestrial ecosystem Cathaysia Flora Lopingian Kayitou Formation
DOI10.1016/j.gloplacha.2020.103248
英文摘要The Permian-Triassic transition is concerned with a critical time interval during the evolutionary history of terrestrial ecosystems. However, the ecological underpinnings of terrestrial ecosystems during this time interval are poorly understood due to an impoverished fossil record. One of the more understudied episodes in the history of life is the ecological state of terrestrial ecosystems immediately before the Permian-Triassic ecological crisis. We address this issue by a quantitative study of a floral assemblage and its herbivorous insect damage based on 1086 plant specimens from the uppermost Permian of Southwest China. This bulk flora comprises 25 genera and 36 species of plants representing a typical, tropical rainforest vegetation of the upper Permian. We record 171 insect damage occurrences belonging to 24 distinctive damage types (DTs) from six functional feeding groups that were recognised in the flora. Statistical analyses of the occurrence, richness, diversity and frequency of DTs reveal that gigantopterids are the principal host plants for insect herbivores in the flora. Compared with other late Permian floras, a significant distinction of the insect damage spectrum can be recognised palaeolatitudinally based on the global position of phytogeographic regions. Despite the different, major targeted plant hosts in these floras, the richness and diversity of insect DTs and their herbivory levels from mid- to high latitudinal floras are remarkably lower than those of low latitudinal to equatorial floras. Our study indicates that terrestrial ecosystems from lower latitudes have higher levels of ecological complexity, and a distinct latitudinal gradient that probably was well established in terrestrial ecosystems during the late Permian. This assessment provides the first comprehensive overview of the ecological relationships among plants and insects, as well as their representation in terrestrial ecosystems of the late Paleozoic Cathaysia Flora.
WOS关键词GLOSSOPTERIS FLORA ; INTEGRATIVE STRATIGRAPHY ; COMPONENT COMMUNITY ; PETRIFIED FOREST ; MASS EXTINCTION ; 1ST RECORD ; HERBIVORY ; DAMAGE ; TIMESCALE ; PATTERNS
资助项目National Natural Science Foundation of China[U1702242] ; National Natural Science Foundation of China[41672015] ; National Natural Science Foundation of China[41762002] ; National Natural Science Foundation of China[41603035] ; Strategic Priority Research Program of the Chinese Academy of Sciences[XDB26000000] ; Yunnan Provincial Science and Technology Department[2019FJ010] ; Yunnan Provincial Science and Technology Department[2018FD008] ; China Geological Survey[DD20190022] ; Key Research Program of the Institute of Geology and Geophysics, Chinese Academy of Sciences[IGGCAS-201905]
WOS研究方向Physical Geography ; Geology
语种英语
出版者ELSEVIER
WOS记录号WOS:000551998100011
资助机构National Natural Science Foundation of China ; National Natural Science Foundation of China ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Yunnan Provincial Science and Technology Department ; Yunnan Provincial Science and Technology Department ; China Geological Survey ; China Geological Survey ; Key Research Program of the Institute of Geology and Geophysics, Chinese Academy of Sciences ; Key Research Program of the Institute of Geology and Geophysics, Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Yunnan Provincial Science and Technology Department ; Yunnan Provincial Science and Technology Department ; China Geological Survey ; China Geological Survey ; Key Research Program of the Institute of Geology and Geophysics, Chinese Academy of Sciences ; Key Research Program of the Institute of Geology and Geophysics, Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Yunnan Provincial Science and Technology Department ; Yunnan Provincial Science and Technology Department ; China Geological Survey ; China Geological Survey ; Key Research Program of the Institute of Geology and Geophysics, Chinese Academy of Sciences ; Key Research Program of the Institute of Geology and Geophysics, Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Yunnan Provincial Science and Technology Department ; Yunnan Provincial Science and Technology Department ; China Geological Survey ; China Geological Survey ; Key Research Program of the Institute of Geology and Geophysics, Chinese Academy of Sciences ; Key Research Program of the Institute of Geology and Geophysics, Chinese Academy of Sciences
源URL[http://ir.iggcas.ac.cn/handle/132A11/97579]  
专题地质与地球物理研究所_中国科学院新生代地质与环境重点实验室
通讯作者Feng, Zhuo
作者单位1.Chinese Acad Geol Sci, Inst Karst Geol, Guilin 541004, Peoples R China
2.Capital Normal Univ, Coll Life Sci, Key Lab Insect Evolut & Environm Change, Beijing 100048, Peoples R China
3.Univ Maryland, Dept Entomol, College Pk, MD 20742 USA
4.Yunnan Univ, Inst Palaeontol, Yunnan Key Lab Palaeobiol, MEC Int Joint Lab Palaeobiol & Palaeoenvironm,Yun, Kunming 650500, Yunnan, Peoples R China
5.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing 100029, Peoples R China
6.CAS Ctr Excellence Life & Paleoenvironm, Beijing 100044, Peoples R China
7.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China
8.Smithsonian Inst, Dept Paleobiol, Natl Museum Nat Hist, Washington, DC 20013 USA
推荐引用方式
GB/T 7714
Liu, Hang-Yu,Wei, Hai-Bo,Chen, Jianbo,et al. A latitudinal gradient of plant-insect interactions during the late Permian in terrestrial ecosystems? New evidence from Southwest China[J]. GLOBAL AND PLANETARY CHANGE,2020,192:12.
APA Liu, Hang-Yu.,Wei, Hai-Bo.,Chen, Jianbo.,Guo, Yun.,Zhou, Yu.,...&Feng, Zhuo.(2020).A latitudinal gradient of plant-insect interactions during the late Permian in terrestrial ecosystems? New evidence from Southwest China.GLOBAL AND PLANETARY CHANGE,192,12.
MLA Liu, Hang-Yu,et al."A latitudinal gradient of plant-insect interactions during the late Permian in terrestrial ecosystems? New evidence from Southwest China".GLOBAL AND PLANETARY CHANGE 192(2020):12.

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来源:地质与地球物理研究所

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