Vegetation response to climate change during an Early Jurassic hyperthermal event (Jenkyns Event) from Northern China (Ordos Basin)

被引:5
|
作者
Baranyi, Viktoria [1 ]
Jin, Xin [2 ,3 ]
Dal Corso, Jacopo [4 ]
Li, Binbing [2 ,3 ]
Kemp, David B. [4 ,5 ]
机构
[1] Croatian Geol Survey, Dept Geol, Sachsova 2, Zagreb 10000, Croatia
[2] Chengdu Univ Technol, State Key Lab Oil & Gas Reservoir Geol & Exploitat, Chengdu 610059, Peoples R China
[3] Chengdu Univ Technol, Inst Sedimentary Geol, Chengdu 610059, Peoples R China
[4] China Univ Geosci, State Key Lab Biogeol & Environm Geol, Wuhan 430074, Peoples R China
[5] China Univ Geosci, Sch Earth Sci, Hubei Key Lab Crit Zone Evolut, Wuhan 430074, Peoples R China
关键词
Jenkyns Event; Hyperthermal; Palynology; Climate; Vegetation change; Ordos Basin; OCEANIC ANOXIC EVENT; TRIASSIC/JURASSIC BOUNDARY; JUNGGAR BASIN; CRETACEOUS STRATA; LUSITANIAN BASIN; ATMOSPHERIC CO2; CARBON-DIOXIDE; FLORAL CHANGES; T-OAE; TOARCIAN;
D O I
10.1016/j.palaeo.2024.112180
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
The Early Jurassic Jenkyns Event (or Toarcian Oceanic Anoxic Event T-OAE) was an episode of global warming and C-cycle perturbation that affected both marine and terrestrial ecosystems, but the interplay between climate change and vegetation is not established in detail from sections outside of Europe. Here, abundance changes in spore-pollen assemblages from the lacustrine Anya succession in the Ordos Basin (North China) reveal a unique record of vegetation dynamics during the Jenkyns Event. Plant communities responded to the event with biodiversity losses and the reorganization of gymnosperm-dominated forests. Community-level shifts are observed from the Pliensbachian-Toarcian boundary, but the onset of the negative carbon excursion (NCIE) that marks the event is coeval with the most significant turnover: a switch from a high-diversity vegetation with conifers, seed ferns, cycads, bennettites and ferns to drought-adapted low-diversity flora with Cheirolepidiaceae. The demise of forests and lowland mire biomes resulted in deforestation with increased weathering and soil erosion that exacerbated the terrestrial ecosystem crisis already under stress from rising temperatures. Terrestrial recovery was initiated before the end of the Jenkyns Event with the resurgence of pioneer ferns and lycopsids that colonized disturbed habitats. Plant assemblages signal aridification at the onset of the event with frequent climatic oscillations and extreme weather patterns during the event itself. The main NCIE phase was preceded by a short-lived cooling phase in the earliest Toarcian. In the aftermath of the NCIE, Cheirolepidiaceae forests declined and a more stable biome developed with seed ferns and various conifers. This was contemporaneous with delta development and shallowing of the lake surrounded by lowland mires with ferns, clubmosses and horsetails. Comparison of floral patterns across the Jenkyns Event show that, although Cheirolepidiaceae dominated the event globally, there were differences in vegetation response between coastal and inland areas, and recovery patterns might differ regionally.
引用
收藏
页数:17
相关论文
共 50 条
  • [31] Response of vegetation variation to climate change and human activities in the Shiyang River Basin of China during 2001-2022
    Sun, Chao
    Bai, Xuelian
    Wang, Xinping
    Zhao, Wenzhi
    Wei, Lemin
    JOURNAL OF ARID LAND, 2024, 16 (08) : 1044 - 1061
  • [32] Climate forcing of terrestrial carbon sink during the Middle Jurassic greenhouse climate: Chronostratigraphic analysis of the Yan′an Formation, Ordos Basin, North China
    Zhang, Zhihui
    Wang, Tiantian
    Ramezani, Jahandar
    Lv, Dawei
    Wang, Chengshan
    GEOLOGICAL SOCIETY OF AMERICA BULLETIN, 2021, 133 (7-8) : 1723 - 1733
  • [33] Chemo-and Biostratigraphy of the Jurassic Oil Shales from the Qiangtang Basin,Northern Tibet,China:A Case Study of the Toarcian Oceanic Anoxic Event
    CHEN Lan
    XU Guiwen
    DA Xuejuan
    YI Haisheng
    ZHU Zhangxiong
    HUANG Zhaohui
    LI Xiaogang
    ActaGeologicaSinica(EnglishEdition), 2017, 91 (02) : 630 - 643
  • [34] Chemo- and Biostratigraphy of the Jurassic Oil Shales from the Qiangtang Basin, Northern Tibet, China: A Case Study of the Toarcian Oceanic Anoxic Event
    Chen, Lan
    Xu, Guiwen
    Da, Xuejuan
    Yi, Haisheng
    Zhu, Zhangxiong
    Huang, Zhaohui
    Li, Xiaogang
    ACTA GEOLOGICA SINICA-ENGLISH EDITION, 2017, 91 (02) : 630 - 643
  • [35] The Artinskian Warming Event: an Euramerican change in climate and the terrestrial biota during the early Permian
    Marchetti, Lorenzo
    Forte, Giuseppa
    Kustatscher, Evelyn
    DiMichele, William A.
    Lucas, Spencer G.
    Roghi, Guido
    Juncal, Manuel A.
    Hartkopf-Froder, Christoph
    Krainer, Karl
    Morelli, Corrado
    Ronchi, Ausonio
    EARTH-SCIENCE REVIEWS, 2022, 226
  • [36] Dynamic change of vegetation and its response to climate and topographic factors in the Xijiang River basin, China
    Lu Jia
    Zhan-bin Li
    Guo-ce Xu
    Zong-ping Ren
    Peng Li
    Yu-ting Cheng
    Yi-xin Zhang
    Bin Wang
    Jia-xin Zhang
    Shu Yu
    Environmental Science and Pollution Research, 2020, 27 : 11637 - 11648
  • [37] Trends of vegetation dynamics and its response to climate change in Pearl River Basin of southwestern China
    Zhenfeng Wei
    Yunyun Zheng
    Rui Zhang
    Lei Du
    Qunying Huang
    Shixin Yang
    Arabian Journal of Geosciences, 2022, 15 (5)
  • [38] Dynamic change of vegetation and its response to climate and topographic factors in the Xijiang River basin, China
    Jia, Lu
    Li, Zhan-bin
    Xu, Guo-ce
    Ren, Zong-ping
    Li, Peng
    Cheng, Yu-ting
    Zhang, Yi-xin
    Wang, Bin
    Zhang, Jia-xin
    Yu, Shu
    ENVIRONMENTAL SCIENCE AND POLLUTION RESEARCH, 2020, 27 (11) : 11637 - 11648
  • [39] The early-Eocene climate optimum (EECO) event in the Qaidam basin, northwest China: clay evidence
    Wang, C. W.
    Hong, H. L.
    Song, B. W.
    Yin, K.
    Li, Z. H.
    Zhang, K. X.
    Ji, J. L.
    CLAY MINERALS, 2011, 46 (04) : 649 - 661
  • [40] Late Pliocene and early pleistocene vegetation and climate change revealed by a pollen record from Nihewan Basin, North China
    Li, Yuecong
    Zhang, Zhen
    Ding, Guoqiang
    Xu, Qinghai
    Wang, Yong
    Chi, Zhenqing
    Dong, Jin
    Zhang, Lei
    QUATERNARY SCIENCE REVIEWS, 2019, 222