托阿尔期大洋缺氧事件在中国陆相地层的碳循环扰动响应<sup>&#x0002A;</sup>

doi:10.7605/gdlxb.2025.02.006

古地理学报 ›› 2025, Vol. 27 ›› Issue (2): 528-540. doi: 10.7605/gdlxb.2025.02.006

• 综述 • 上一篇

托阿尔期大洋缺氧事件在中国陆相地层的碳循环扰动响应^*

陈兰(), 达雪娟, 朱章雄, 徐桂文, 毛伟丞, 黄文科, 夏芳, 杨佩琳, 骆宇晗, 廖显娇

重庆科技大学地球科学系, 重庆 401331

收稿日期:2024-03-06 修回日期:2024-05-31 出版日期:2025-04-01 发布日期:2025-04-01
作者简介:
陈兰,女,1975年生,教授,主要从事黑色页岩与大洋缺氧事件研究。E-mail: cllc-10@163.com。
基金资助:
*国家自然科学基金(编号: 42272125,42241203,41572095)以及中国科学院地球化学研究所矿床地球化学国家重点实验室开放基金(编号: 202215)共同资助

Response to carbon cycle perturbation during the Toarcian oceanic anoxic event in terrestrial strata of China

CHEN Lan(), DA Xuejuan, ZHU Zhangxiong, XU Guiwen, MAO Weicheng, HUANG Wenke, XIA Fang, YANG Peilin, LUO Yuhan, LIAO Xianjiao

Department of Earth Sciences,Chongqing University of Science and Technology,Chongqing 401331,China

Received:2024-03-06 Revised:2024-05-31 Online:2025-04-01 Published:2025-04-01
About author:
CHEN Lan,born in 1975,professor,is mainly engaged in research on black shales and Oceanic Anoxic Events. E-mail: cllc-10@163.com.
Supported by:
Co-funded by the National Natural Science Foundation of China(Nos. 42272125,42241203,41572095)and Opening Foundations of the State Key Laboratories of Ore Deposit Geochemistry,Institute of Geochemistry,Chinese Academy of Sciences(No.202215)

摘要/Abstract

摘要：

早侏罗世托阿尔期早期的大洋缺氧事件(Toarcian Oceanic Anoxic Event,T-OAE)是中生代发生的一次剧烈的环境扰动事件,伴随着全球碳同位素负偏、快速升温、金属中毒等。然而,对这一事件的研究主要集中在特提斯洋等海相地层,陆相地层研究比较薄弱。前人运用沉积学、古生物学、同位素地层学等多学科交叉,发现T-OAE在中国四川盆地、金羊盆地、柴达木盆地等陆相地层中有明显的响应,并且碳同位素发生了-1.3‰~-7‰负偏,最大负偏移量达到-12.5‰,其偏移可能为Karoo-Ferrar 大火成岩省喷发,导致大量的¹²C释放,引起了一系列气候—环境—生态变化。换言之,Karoo-Ferrar大火成岩省(KFLIP)引起温度升高,甲烷水合物分解,进一步加剧变暖,使得大量的甲烷或CO₂进入大气中; 温度升高也伴随着从湿地、永久冻土、冰盖、植被野火中释放出大量的甲烷或CO₂作为碳源,从而引起了碳同位素负偏移。虽然这些机制与温度升高以及正反馈气候作用有关,但不是引起T-OAE碳同位素偏移的必然控制因素。总之,KFLIP可能是T-OAE的导火线,造成了碳循环出现幕式扰动。研究结果可以与同时期海相地层进行综合对比,为精确厘定T-OAE层位提供可靠依据; 进一步探讨碳循环扰动的影响因素,也可能为更全面地了解早侏罗世托阿尔期大洋缺氧事件在陆相地层中的气候—环境响应提供新的思路。

关键词: 侏罗纪, 托阿尔期大洋缺氧事件, 碳循环扰动, 陆相地层, 中国

Abstract:

The Early Jurassic Toarcian Oceanic Anoxic Event(T-OAE,ca.~183Ma)represents a significantly environmental perturbation in the Mesozoic and was associated with pronounced negative carbon isotope excursion(NCIE),increasing sea-surface temperatures,heavy metal poising,and so on. This event recording in the Marine strata such as the Tethys ocean,has been researched in detail,but it was paid little attention in the terrestrial strata. This review synthesizes data from the Sichuan,Jingyuan,and Qaidam basins,which preserve terrestrial responses to the T-OAE based on sedimentological,paleontological,and isotopic evidence. Terrestrial strata exhibit a carbon isotope excursion(CIE)of -1.3‰ to -7‰,whereas the Ordos Basin records an extreme CIE of -12.5‰. These anomalies suggest carbon-cycle perturbations linked to major environmental changes,likely triggered by massive volcanism from the Karoo-Ferrar Large Igneous Province(KFLIP). An alternatively hypothesis is that KFLIP-triggered climatic warming released unusually high fluxes of methane and /or carbon dioxide to the atmosphere. Rising temperatures during the early Toarcian would also have increased emission of large amounts of methane and /or carbon dioxide from wetlands,permafrost,ice caps,and vegetation wildfire. Although these mechanisms would have contributed to rising global temperatures via positive climate feedbacks,they may not represent the primary driver of the Toarcian CIE. By correlating terrestrial and marine records(e.g.,European Shelf and North China), this study refines the stratigraphic framework of the T-OAE. Furthermore, evaluating paleotemperature proxies, carbon-cycle dynamics, and their environmental couplings during the T-OAE offers insights into modern climate responses to light carbon emissions.

Key words: Jurassic, T-OAE, carbon cycle perturbation, terrestrial strata, China

陈兰, 达雪娟, 朱章雄, 徐桂文, 毛伟丞, 黄文科, 夏芳, 杨佩琳, 骆宇晗, 廖显娇. 托阿尔期大洋缺氧事件在中国陆相地层的碳循环扰动响应^*[J]. 古地理学报, 2025, 27(2): 528-540.

CHEN Lan, DA Xuejuan, ZHU Zhangxiong, XU Guiwen, MAO Weicheng, HUANG Wenke, XIA Fang, YANG Peilin, LUO Yuhan, LIAO Xianjiao. Response to carbon cycle perturbation during the Toarcian oceanic anoxic event in terrestrial strata of China[J]. Journal of Palaeogeography（Chinese Edition）, 2025, 27(2): 528-540.

http://www.gdlxb.cn/CN/Y2025/V27/I2/528

图/表 5

表2 中国陆相盆地Toarcian期TOC含量、有机碳同位素值以及偏移(CIE)

Table2 Full listing of sections studied in this work,along with key data on TOC and organic carbon isotopes values and excursions(CIE),and references

研究剖面	四川盆地				塔里木盆地		柴达木盆地大煤沟	鄂尔多斯盆地安崖	辽宁
研究剖面	Core A	Core B	LQ104X井	阆中地区	西剖面	东剖面	柴达木盆地大煤沟	鄂尔多斯盆地安崖	金羊盆地 ZK01井	田师傅盆地长梁子
TOC /%	$0.1 ~ 3.3 1.2$	$0.1 ~ 1.3 0.6$	$0.23 ~ 1.97 0.94$	$0.10 ~ 3.63 1.56$	$0 ~ 4.5 0.47$	$0.1 ~ 17.1 3.38$	$0.7 ~ 4.16 1.63$	$0.04 ~ 22.13 1.49$	$0.61 ~ 4.33 1.32$	$0.18 ~ 0.95 0.56$
δ¹³C_org /‰	$- 30.1 ~ - 22.8 - 27.6$	$- 27.9 ~ - 21.3 - 24.8$	$- 28.6 ~ - 23.4 - 26.4$	$- 29.8 ~ - 23.1 -$	$- 20.9 ~ - 28.4 -$	$- 21.7 ~ - 26.5 -$	$- 29.1 ~ - 21 - 24.8$	$- 32.85 ~ - 18.04 - 25.44$	$- 23.3 ~ 25.3 - 24.1$	$- 25.5 ~ - 22.1 - 23.8$
CIE/‰	-4	-4	-3.8	-3.9	-7	-4.5	-3.5	-12.5	-2	+1.3
参考文献	Xu et al., 2017a	Xu et al., 2017a	Liu et al.,2020a	Wang et al., 2023a,2023b	Qiu et al., 2023b	Qiu et al., 2023b	Lu et al., 2020	Jin et al.,2020	Liu et al., 2020b	Zhang et al., 2021

表2 中国陆相盆地Toarcian期TOC含量、有机碳同位素值以及偏移(CIE)

Table2 Full listing of sections studied in this work,along with key data on TOC and organic carbon isotopes values and excursions(CIE),and references

研究剖面	四川盆地				塔里木盆地		柴达木盆地大煤沟	鄂尔多斯盆地安崖	辽宁
研究剖面	Core A	Core B	LQ104X井	阆中地区	西剖面	东剖面	柴达木盆地大煤沟	鄂尔多斯盆地安崖	金羊盆地 ZK01井	田师傅盆地长梁子
TOC /%	$0.1 ~ 3.3 1.2$	$0.1 ~ 1.3 0.6$	$0.23 ~ 1.97 0.94$	$0.10 ~ 3.63 1.56$	$0 ~ 4.5 0.47$	$0.1 ~ 17.1 3.38$	$0.7 ~ 4.16 1.63$	$0.04 ~ 22.13 1.49$	$0.61 ~ 4.33 1.32$	$0.18 ~ 0.95 0.56$
δ¹³C_org /‰	$- 30.1 ~ - 22.8 - 27.6$	$- 27.9 ~ - 21.3 - 24.8$	$- 28.6 ~ - 23.4 - 26.4$	$- 29.8 ~ - 23.1 -$	$- 20.9 ~ - 28.4 -$	$- 21.7 ~ - 26.5 -$	$- 29.1 ~ - 21 - 24.8$	$- 32.85 ~ - 18.04 - 25.44$	$- 23.3 ~ 25.3 - 24.1$	$- 25.5 ~ - 22.1 - 23.8$
CIE/‰	-4	-4	-3.8	-3.9	-7	-4.5	-3.5	-12.5	-2	+1.3
参考文献	Xu et al., 2017a	Xu et al., 2017a	Liu et al.,2020a	Wang et al., 2023a,2023b	Qiu et al., 2023b	Qiu et al., 2023b	Lu et al., 2020	Jin et al.,2020	Liu et al., 2020b	Zhang et al., 2021

图1 四川盆地大安寨段碳同位素和TOC曲线对比(数据来源于: Xu et al., 2017a;Liu et al., 2020a;Wang et al., 2023a,2023b)

Fig.1 δ¹³C_org and TOC during T-OAE in the Da’anzai Member of Sichuan Basin(Data sources from Xu et al., 2017a;Liu et al., 2020a;Wang et al., 2023a,2023b)

图2 中国其他盆地侏罗系有机碳同位素和TOC曲线对比(数据来源于: Jin et al., 2020;Liu et al., 2020b;Lu et al., 2020;Zhang et al., 2021;邱若原等,2023)

Fig.2

δ 13 C org

and TOC during T-OAE in the Jurassic in other basins of China(Data sources from Jin et al., 2020;Liu et al., 2020b;Lu et al., 2020;Zhang et al., 2021;Qiu et al., 2023)

图2 中国其他盆地侏罗系有机碳同位素和TOC曲线对比(数据来源于: Jin et al., 2020;Liu et al., 2020b;Lu et al., 2020;Zhang et al., 2021;邱若原等,2023)

Fig.2

δ 13 C org

and TOC during T-OAE in the Jurassic in other basins of China(Data sources from Jin et al., 2020;Liu et al., 2020b;Lu et al., 2020;Zhang et al., 2021;Qiu et al., 2023)

图3 T-OAE期间Karoo-Ferrar 大火成岩省引起的气候、环境变化

Fig.3 Climate and environmental effects of Karoo-Ferrar Large Igneous Province(KFLIP)during T-OAE

参考文献 98

[1]	陈小浪. 2015. 辽宁本溪田师傅盆地侏罗纪植物群以及沉积环境研究. 东北大学硕士学位论文.
	[Chen X L. 2015. Researches on the Jurassic plants and sedimentary environment of the Tianshifu Basin,Benxi,Liaoning Province. Masteral dissertation of Northeastern University]
[2]	陈杨,金鑫,郎咸国,李滨兵. 2023. 鄂尔多斯盆地T-OAE时期湖泊硫循环及其地质意义. 沉积学报: 1-22. DOI: 10.14027/j.issn.1000-0550.2023.112.
	[Chen Y,Jin X,Lang X G,Li B B. 2023. Sulfur Cycle Change and Its Geological Significance During the Toarcian Oceanic Anoxic Event(T-OAE)in the Ordos Basin. Acta Sedimentologica Sinica: 1-22. DOI: 10.14027/j.issn.1000-0550.2023.112]
[3]	邓胜徽,卢远征,樊茹,方林浩,李鑫,刘璐. 2012. 早侏罗世Toarcian期大洋缺氧事件及其在陆地生态系统中的响应. 地球科学,37(增刊2): 23-38.
	[Deng S H,Lu Y Z,Fan R,Fang L H,Li X,Liu L. 2012. Toarcian(Early Jurassic)Oceanic Anoxic Event and the responses in terrestrial ecological system. Earth Science, 37(Supplement 2): 23-38]
[4]	冯宝华. 1988. 彬县延长群古风化壳、富县组“花斑泥岩”和华池等地富县组粘土岩的特征及相变关系. 煤田地质与勘探,(3): 12-14.
	[Feng B H. 1988. Characteristics and phase transformation relationship of ancient weathering crust of Yanchang Group in Binxian County,“spotted mudstone”of Fuxian Formation and clay rock of Fuxian Formation in Huachi. Coal Geology & Exploration,(3): 12-14]
[5]	高瑞珍. 2019. 柴北缘早侏罗世古气候演化及对Toarcian大洋缺氧事件的响应. 河南科技大学硕士学位论文.
	[Gao R Z. 2019. Paleoclimatic evolution of the Early Jurassic in the northern Qaidam Basin and its response to the Toarcian Ocean Anoxic Events. Masteral dissertation of Henan Polytechnic University]
[6]	胡俊杰,马寅生,吴祎,李宗星,彭博,魏小洁,刘大鹏. 2019. 柴达木盆地侏罗纪古气候演变过程: 来自化学风化特征的证据. 高校地质学报,25(4): 548-557.
	[Hu J J,Ma Y S,Wu Y,Li Z X,Peng B,Wei X J,Liu D P. 2019. Jurassic palaeoclimate evolution of the Qaidam Basin: evidence from chemical weathering analyses. Geological Journal of China Universities,25(4): 548-557]
[7]	黄迪颖. 2019. 中国侏罗纪综合地层和时间框架. 中国科学: 地球科学,49: 227-256.
	[Huang D Y. 2019. Jurassic integrative stratigraphy and timescale of China. Science China: Earth Sciences,49: 227-256]
[8]	刘犟,李凤杰,侯景涛,方朝刚,孟立娜. 2012. 鄂尔多斯盆地吴起地区下侏罗统富县组沉积相特征. 岩性油气藏,24( 3) : 74-78.
	[Liu J,Li F J,Hou J T,Fang C G,Meng L N. 2012. Sedimentary facies of the Lower Jurasic Formation in Wuqi area,Ordos Basin. Lithologic Reservoirs,24( 3) : 74-78]
[9]	刘淼,张渝金,孙守亮,陈井胜,李斌,杨帆,张涛,汪岩,吴振. 2019. 辽西金羊盆地北票组孢粉组合及其时代和古气候意义. 地球科学,44(10): 3393-3408.
	[Liu M,Zhang Y J,Sun S L,Chen J S,Li B,Yang F,Zhang T, Wang Y,Wu Z. 2019. Palynological assemblages of Beipiao Formation in Jinyang Basin of West Liaoning,and Their Age and Paleoclimatic Significances. Earth Science,44(10): 3393-3408]
[10]	刘兆生. 1998. 塔里木盆地北缘侏罗纪孢粉组合. 微体古生物学报,15(2): 144-165.
	[Liu Z S. 1998. Jurassic palynological assemblages from the northern Margin in the Tarim Basin of Xinjiang,NW China. Acta Micropalaeontologica Sinica,15(2): 144-165]
[11]	鲁静,邵龙义,王占刚,李永红,王帅. 2014. 柴北缘侏罗纪煤层有机碳同位素组成与古气候. 中国矿业大学学报,43(4): 612-618.
	[Lu J,Shao L Y,Wang Z G,Li Y H,Wang S. 2014. Organic carbon isotope composition and paleoclimatic evolution of Jurassic coal seam in the northern Qaidam basin. Journal of China University of Mining & Technology. 43(4): 612-618]
[12]	鲁静,杨敏芳,孙晓禹,邵龙义,张凤海. 2018. 柴北缘侏罗纪煤显微组分与泥炭沉积速率. 矿业科学学报,3(1): 1-8.
	[Lu J,Yang M F,Sun X Y,Shao L Y,Zhang F H. 2018. Jurassic coal maceral and deposition rate of peat in the northern Qaidam Basin. Journal of Mining Science and Technology,3(1): 1-8]
[13]	钱涛,王宗秀,柳永清,刘少峰,高万里,李王鹏,胡俊杰,李磊磊. 2018. 柴达木盆地北缘侏罗纪沉积物源分析: 地层序列及LA-ICP-MS年代学信息. 中国科学: 地球科学,48: 224-242.
	[Qian T,Wang Z X,Liu Y Q,Liu S F,Gao W L,Li W P,Hu J J,Li L L. 2018. Provenance analysis of the Jurassic northern Qaidam Basin: stratigraphic succession and LA-ICP-MS geochronology. Scientia Sinica Terrae,48: 224-242]
[14]	秦健铭,陈积权,高远,席党鹏,王成善. 2020. 松辽盆地晚白垩世陆表古温度定量重建: 以LD6-7井嫩江组一、二段为例. 沉积学报,38(4): 759-770.
	[Qin J M,Chen J Q,Gao Y,Xi D P,Wang C S. 2020. Quantitative paleotemperature reconstruction of Late Cretaceous Nenjiang Formation in Songliao Basin: a case study of the LD6-7 Core. Acta Sedimentologica Sinica,38(4): 759-770]
[15]	邱若原,方琳浩,卢远征,邓胜徽,张新智,吕沛宗,任嘉豪,黄汝婷,房亚男,张小宇,李宏佳,鲜本忠,师生宝. 2023. 早侏罗世大洋缺氧事件在塔里木盆地的响应. 沉积学报,41(2): 425-434.
	[Qiu R Y,Fang L H,Lu Y Z,Deng S H,Zhang X Z,Lü P Z,Ren J H,Huang R T,Fang Y N,Zhang X Y,Li H J,Xian B Z,Shi S B. 2023. Responses to the Early Jurassic Oceanic Anoxic Events in the Tarim Basin. Acta Sedimentologica Sinica,41(2): 425-434]
[16]	陕西省地质矿产局. 1998. 陕西省岩石地层. 武汉: 中国地质大学出版社,1-291.
	[Shaanxi Bureau of Geology and Mineral Resources. 1998. The Rock Stratigraphy of Shaanxi Province. Wuhan: China University of Geosciences Press, 1-291]
[17]	王招明,钟端,赵培荣,夏维书,张师本,严剑洲. 2004. 库车前陆盆地露头区油气地质. 北京: 石油工业出版社.
	[Wang Z M,Zhong D,Zhao P R,Xia W S,Zhang S B,Yan J Z. 2004. Petroleum Geology of Outcrops Areas in Kuche Foreland Basin. Beijing: Petroleum Industry Press]
[18]	许坤,杨建国,陶明华,梁鸿德,赵传本,李荣辉,孔慧,李瑜,万传彪,彭维松. 2003. 中国北方侏罗系(Ⅶ): 东北地层区. 北京: 石油工业出版社.
	[Xu K.,Yang J G,Tao M H,Liang H D,Zhao C B,Li R H,Kong H,Li Y,Wan C B,Peng W S. 2003. Jurassic System in the North of China(Ⅶ): Northeast Stratigraphic Region. Beijing: Petroleum Industry Press]
[19]	杨若飞. 2019. 四川盆地大安寨段黑色岩系沉积环境、成烃特征及对早侏罗世大洋缺氧事件的陆相响应研究. 南京大学博士学位论文.
	[Yang R F. 2019. Sedimentary environment and hydrocarbon generation of the black shales series in the Da’anzhai Member and its terrestrial response to the EarlyJurassic Oceanic Anoxic Event in the Sichuan Basin,China. Doctoral dissertation of Nanjing University]
[20]	袁效奇,傅智雁,王喜富. 2003. 中国北方侏罗系(V): 鄂尔多斯地层区. 北京: 石油工业出版社,54-94.
	[Yuan X Q,Fu Z Y,Wang X F. 2003. Jurassic System in the North of China(V)Odros stratigraphic Region. Beijing: Petroleum Industry Press,54-94]
[21]	张虎权,王廷栋,阎存凤,袁剑英. 2007. 民和盆地侏罗系地层划分与对比. 地层学杂志,(1): 62-67.
	[Zhang H Q,Wang T D,Yan C F,Yuan J Y. 2007. The subdivision and correlation of the Jurassic system of the Minhe Basin. Journal of Stratigraphy,(1): 62-67]
[22]	张艳,裴昌蓉,孙守亮,万传彪,孙跃武. 2022. 辽西金羊盆地SZK01井北票组孢粉组合及其地质意义. 大庆石油地质与开发,41(6): 13-22.
	[Zhang Y,Pei C R,Sun S L,Wan C B,Sun Y W. 2022. Palynological assemblage of Beipiao Formation in Well SZK01 in Jinyang Basin and its geological significances. Petroleum Geology and Development in Daqing,41(6): 13-22]
[23]	张云望,金鑫,乔培军,李滨兵,洪彦哲,陈俞超,芦刚,杜怡星,时志强. 2023. 鄂尔多斯盆地东北部下侏罗统富县组沉积物源分析: 来自榆林安崖剖面砂岩的岩石学及元素地球化学证据. 沉积学报,41(5): 1414-1429.
	[Zhang Y W,Jin X,Qiao P J,Li B B,Hong Y Z,Chen Y C,Lu G,Du Y X,Shi Z Q. 2023. Petrological and geochemical constraints on sedimentary provenance of the Fuxian Formation(Lower Jurassic)Sandstones in the Northeastern Ordos Basin. Acta Sedimentologica Sinica,41(5): 1414-1429]
[24]	赵俊兴,陈洪德,张锦泉. 1999. 鄂尔多斯盆地下侏罗统富县组沉积体系及古地理. 岩相古地理,19( 5) : 40-46.
	[Zhao J X,Chen H D,Zhang J Q. 1999. The depositiona systems and palaeogeography of the Lower Jurassic Fuxian Formaion in the Ordos Basin. Sedimentary Facies and Palaeogeography,19( 5) : 40-46]
[25]	甄甄,李永飞,郜晓勇,孙守亮,周铁锁. 2016. 金羊盆地SZK01井下侏罗统北票组沉积相及其有机质特征. 世界地质,35(1): 207-215.
	[Zhen Z,Li Y F,Gao X Y,Sun S L,Zhou T S. 2016. Characteristics of sedimentary facies and organic Matter of Lower Jurassic Beipiao Formation of Well SZK01 in Jinyang Basin. Global Geology,35(1): 207-215]
[26]	Baker S J,Hesselbo S P,Lenton T M,Duarte L V,Belcher C M. 2017. Charcoal evidence that rising atmospheric oxygen terminated Early Jurassic Ocean anoxia. Nature Communications,8: 15018.
[27]	Baranyi V,Jin X,Dal Corso J,Shi Z Q,Grasby S E,Kemp D B. 2023. Collapse of terrestrial ecosystems linked to heavy metal poisoning during the Toarcian oceanic anoxic event. Geology,51(7): 652-656.
[28]	Burgess S D, Bowring S A. 2015. High-precision geochronology confirms voluminous magmatism before, during, and after Earth’s most severe extinction. Science Advances, 1(7): e1500470.
[29]	Came R E,Brand U,Affek H P. 2014. Clumped isotope signatures in modern brachiopod carbonate. Chemical Geology,377: 20-30.
[30]	Caruthers A H,Smith P L,Gröcke D R. 2013. The Pliensbachian-Toarcian(Early Jurassic)extinction,a global multi-phased event. Palaeogeography,Palaeoclimatology,Palaeoecology,386: 104-118.
[31]	Chen W H,Kemp D B,He T C,Huang C J,Jin S M,Xiong Y J,Newton R J. 2021. First record of the early Toarcian Oceanic Anoxic Event in the Hebrides Basin(UK)and implications for redox and weathering changes. Global and Planetary Change,207: 103685.
[32]	Cohen A S,Coe A L,Harding S M,Schwark L. 2004. Osmium isotope evidence for the regulation of atmospheric CO₂ by continental weathering. Geology,32: 157-160.
[33]	Cui H,Zhu S F,Liang C,Ma W Z,Tong H,Shi Z S. 2023. Facies association analysis of a Toarcian siliciclastic-carbonate lacustrine system,Sichuan Basin,China. Palaeogeography,Palaeoclimatology,Palaeoecology,631: 111841.
[34]	Dennis K J,Cochran J K,Land Man N H,Schrag D P. 2013. The climate of the Late Cretaceous: new insights from the application of the carbonate clumped isotope thermometer to Western Interior Seaway Macrofossil. Earth and Planetary Science Letters,362: 51-65.
[35]	Erba E. 2004. Calcareous nannofossils and Mesozoic oceanic anoxic events . Marine Micropaleontology, 52(1): 85-106.
[36]	Ettinger N P,Larson T E,Kerans C,Thibodeau A M,Hattori K E,Kacur S M,Martindale R C. 2021. Ocean acidification and photic-zone anoxia at the Toarcian Oceanic Anoxic Event: insights from the Adriatic Carbonate Platform. Sedimentology,68: 63-107.
[37]	Fantasia A,Föllmi K B,Adatte T,Spangenberg J E,Montero-Serrano J C. 2018. The Early Toarcian oceanic anoxic event: paleoenvironmental and paleoclimatic change across the Alpine Tethys(Switzerland). Global and Planetary Change,162: 53-68.
[38]	Fernandez A,Korte C,Ull Mann C V,Looser N,Wohlwend S,Bernasconi S M. 2021. Reconstructing the Magnitude of Early Toarcian(Jurassic)warming using the reordered clumped isotope compositions of belemnites. Geochimica et Cosmochimica Acta,293: 308-327.
[39]	Gambacorta G,Cavalheiro L,Brumsack H J,Dickson A J,Jenkyns H C,Schnetger B,Wagner T,Erba E. 2023. Suboxic conditions prevailed during the Toarcian Oceanic Anoxic Event in the Alpine-Mediterranean Tethys: the Sogno Core pelagic record(Lombardy Basin,northern Italy). Global and Planetary Change,223: 104089.
[40]	Gambacorta G,Brumsack H J,Jenkyns H C,Erba E. 2024. The early Toarcian Oceanic Anoxic Event(Jenkyns Event)in the Alpine-Mediterranean Tethys,north African Margin,and north European epicontinental seaway. Earth-Science Reviews,248: 104636.
[41]	Ghosh P,Adkins J,Affek H,Balta B,Guo W,Schauble E A,Schrag D,Eiler J M. 2006. ¹³C-¹⁸O bonds in carbonate minerals: a new kind of paleothermometer. Geochimica et Cosmochimica Acta,70(6): 1439-1456.
[42]	Hesselbo S P,Jenkyns H C. 1998. British lower Jurassic Sequence Stratigraphy. Mesozoic and Cenozoic Sequence Stratigraphy of European Basins,60: 561-581.
[43]	Hesselbo S P,Jenkyns H C,Duarte L V,Oliveira L C V. 2007. Carbon-isotope record of the Early Jurassic(Toarcian)Oceanic Anoxic Event from fossil wood and Marine carbonate(Lusitanian Basin,Portugal). Earth and Planetary Science Letters,253: 455-470.
[44]	Hollaar T P,Baker S J,Hesselbo S P,Deconinck J F,Mander L,Ruhl M,Belcher C M. 2021. Wildfire activity enhanced during phases of Maximum orbital eccentricity and precessional forcing in the early Jurassic. Communications Earth & Environment,2(1): 247.
[45]	Huang C J,Hesselbo S P. 2014. Pacing of the Toarcian Oceanic Anoxic Event(Early Jurassic)from astronomical correlation of Marine sections. Gondwana Research,25(4): 1348-1356.
[46]	Ikeda M,Hori R S,Ikehara M,Miyashita R,Chino M,Ya Mada K. 2018. Carbon cycle dynamics linked with Karoo-Ferrar volcanism and astronomical cycles during Pliensbachian-Toarcian(Early Jurassic). Global and Planetary Change,170: 163-171.
[47]	Jenkyns H C. 1985. The early Toarcian and Ceno Manian-Turonian anoxic events in Europe: comparisons and contrasts. Geologische Rundschau,74: 505-518.
[48]	Jenkyns H C. 1988. The early Toarcian(Jurassic)anoxic event: stratigraphic,sedimentary,and geochemical evidence. American Journal of Science,288: 101-151.
[49]	Jenkyns H C. 2010. Geochemistry of oceanic anoxic events. Geochemistry,Geophysics,Geosystems,11: Q03004.
[50]	Jenkyns H C,Clayton C J. 1986. Black shales and carbon isotopes in pelagic sediments from the Tethyan Lower Jurassic. Sedimentology,33: 87-106.
[51]	Jenkyns H C,Sophie M. 2021. The chemostratigraphy and environmental significance of the Marlstone and Junction Bed(Beacon Limestone,Toarcian,Lower Jurassic,Dorset,UK). Geological Magazine,159: 357-371.
[52]	Jenkyns H C, Macfarlane S. 2022. The chemostratigraphy and environmental significance of the Marlstone and Junction Bed (Beacon Limestone, Toarcian, Lower Jurassic, Dorset, UK). Geological Magazine, 159: 357-371.
[53]	Jin X,Shi Z Q,Baranyi V,Kemp D B,Han Z,Luo G M,Hu J F,He F,Chen L,Preto N. 2020. The Jenkyns Event(early Toarcian OAE)in the Ordos Basin,North China. Global and Planetary Change,193: 103273.
[54]	Jin X,Zhang F,Baranyi V,Kemp D B,Feng X B,Grasby S E,Sun G Y,Shi Z Q,Chen W H,Dal Corso J. 2022. Early Jurassic Massive release of terrestrial mercury linked to floral crisis. Earth and Planetary Science Letters,598: 117842.
[55]	Jones M W,Abatzoglou J T,Veraverbeke S,Andela N,Lasslop G,Forkel M,Smith A J P,Burton C,Betts R A,Vander,Werf G R,Sitch S,Canadell J G,Santín C,Kolden C,Doerr S H,Le Qu’er’e,Corinne.2022. Global and regional trends and drivers of fire under climate change. Rev. Geophys,60: e2020RG000726.
[56]	Kemp D B,Coe A L,Cohen A S,Schwark L. 2005. Astronomical pacing of methane release in the Early Jurassic period. Nature,437: 396-399.
[57]	Kemp D B, Selby D, Izumi K. 2020. Direct coupling between carbon release and weathering during the Toarcian oceanic anoxic event. Geology, 48(10): 976-980.
[58]	Kemp D B,Suan G,Fantasia A,Jin S M,Chen W H. 2022. Global organic carbon burial during the Toarcian oceanic anoxic event: patterns and controls. Earth-Science Reviews,231: 104086.
[59]	Krencker F N, Fantasia A, El Ouali M, Kabiri L, Bodin S. 2022. The effects of strong sediment-supply variability on the sequence stratigraphic architecture: Insights from early Toarcian carbonate factory collapses. Marine and Petroleum Geology, 136: 105469.
[60]	Küspert W. 1982. Environmental changes during oil shale deposition as deduced from stable isotope ratios. In: Einsele G, Seilacher A(eds). Cyclic and Event Stratification. Berlin, Heidelberg: Springer, 482-501.
[61]	Kunert A,Kendall B. 2023. Global ocean redox changes before and during the Toarcian Oceanic Anoxic Event. Nature Eommunications,14: 815.
[62]	Li B B,Jin X,Corso J D,Ogg J G,Lang X G,Baranyi V,Preto N,Franceschi M,Qiao P J,Shi Z Q. 2023. Complex pattern of environmental changes and organic Matter preservation in the NE Ordos lacustrine depositional system(China)during the T-OAE(Early Jurassic). Global and Planetary Change,221: 104045.
[63]	Li D H,Li J Z,Zhang B,Yang J J,Wang S Y. 2017. Formation characteristics and resource potential of Jurassic tight oil in Sichuan Basin. Petroleum Research,2(4): 301-314.
[64]	Li Q,McArthur J M,Thirlwall M F,Turchyn A V,Page K,Bradbury H J,Weis R,Lowry D. 2021. Testing for ocean acidification during the Early Toarcian using δ44/40Ca and δ88/86Sr. Chemical Geology,574: 120228.
[65]	Liu J C,Cao J,Hu G,Wang Y,Yang R F,Liao Z W. 2020a. Water-level and redox fluctuations in a Sichuan Basin lacustrine system coincident with the Toarcian OAE. Palaeogeography,Palaeoclimatology,Palaeoecology,558: 109942.
[66]	Liu M,Sun P,Them II T R,Li Y F,Sun S L,Gao X Y,Huang X,Tang Y J. 2020b. Organic geochemistry of a lacustrine shale across the Toarcian Oceanic Anoxic Event(Early Jurassic)from NE China. Global and Planetary Change,191: 103214.
[67]	Liu R P,Hu G,Cao J,Yang R F,Liao Z W,Hu C W,Pang Q,Pang P. 2022. Enhanced hydrological cycling and continental weathering during the Jenkyns Event in a lake system in the Sichuan Basin,China. Global and Planetary Change,216: 103915.
[68]	Lu J,Zhou K,Yang M F,Eley Y,Shao L Y,Hilton J. 2020. Terrestrial organic carbon isotopic composition(δ¹³C_org)and environmental perturbations linked to Early Jurassic volcanism: evidence from the Qinghai-Tibet Plateau of China. Global and Planetary Change,195: 103331.
[69]	Mattioli E,Pittet B,Suan G,Mailliot S. 2008. Calcareous nannoplankton changes across the early Toarcian oceanic anoxic event in the western Tethys. Paleoceanography,23: PA3208.
[70]	McArthur J M,Donovan D T,Thirlwall M F,Fouke B W,Mattey D. 2000. Strontium isotope profile of the early Toarcian(Jurassic)oceanic anoxic event,the duration of ammonite biozones,and belemnite palaeotemperatures. Earth and Planetary Science Letters,179(2): 269-285.
[71]	Müller T,Price G,Bajnai D,Nyerges A,Kesjár D,Raucsik B,Varga A,Judik K,Fekete J,May Z,Pálfy J. 2017. New multiproxy record of the Jenkyns Event(also known as the Toarcian Oceanic Anoxic Event)from the Mecsek Mountains(Hungary): differences,duration and drivers. Sedimentology,64(1): 66-86.
[72]	Ogg J G,Ogg G M,Gradstein F M. 2016. Jurassic: A Concise Geologic Time Scale. Amsterdam: Elsevier: 151-166.
[73]	Pieńkowski G,Hodbod M,Ull Mann C V. 2016. Fungal decomposition of terrestrial organic Matter accelerated Early Jurassic climate warming. Scientific Reports,6: 31930.
[74]	Pieńkowski G,Hesselbo S P,Barbacka M,Leng M J. 2020. Non-Marine carbon-isotope stratigraphy of the Triassic-Jurassic transition in the Polish Basin and its relationships to organic carbon preservation,ρCO₂ and palaeotemperature. Earth-Science Reviews,210: 103383.
[75]	Qiu R Y,Fang L H,Lu Y Z,Chen Y X,Huang R D,Lei W Z,Zhang P Y,Li M S. 2023a. Cyclostratigraphy of the Lower Jurassic(Toarcian)terrestrial successions in the Sichuan Basin,southwestern China. Journal of Asian Earth Sciences,250: 105617.
[76]	Qiu R Y,Fang L H,Lü P Z,Jiang F J,Zhang X Z,Zhang X Y,Zhang P Y,Zhu L,Shi S B. 2023b. Long eccentricity forcing of the Late Pliensbachian to Early Toarcian(Jurassic)terrestrial wildfire activities in the Tarim Basin,northwestern China. Palaeogeography,Palaeoclimatology,Palaeoecology,613: 111408.
[77]	Qiu Z,He J L. 2022. Depositional environment changes and organic Matter accumulation of Pliensbachian-Toarcian lacustrine shales in the Sichuan basin,SW China. Journal of Asian Earth Sciences,232: 105035.
[78]	Reolid M,Iwańczuk J,Mattioli E,Abad I. 2020. Integration of gam Ma ray spectrometry,magnetic susceptibility and calcareous nannofossils for interpreting environmental perturbations: an example from the Jenkyns Event(lower Toarcian)from South Iberian Palaeo Margin(Median Subbetic,SE Spain). Palaeogeography,Palaeoclimatology,Palaeoecology,560: 110031.
[79]	Robinson S A,Ruhl M,Astley D L,Naafs B D A,Farnsworth J A,Bown P R,Jenkyns H C,Lunt D J,O’Brien C,Pancost R D,Markwick P. 2017. Early Jurassic North Atlantic sea-surface temperatures from TEX86 palaeothermometry. Sedimentology,64(1): 215-230.
[80]	Ruebsam W,Al-Husseini M. 2020. Calibrating the Early Toarcian(Early Jurassic)with stratigraphic black holes(SBH). Gondwana Research,82: 317-336.
[81]	Ruebsam W,Reolid M,Mattioli E,Schwark L. 2022. Organic carbon accumulation at the northern Gondwana paleo Margin(Tunisia)during the Toarcian Oceanic Anoxic Event: sedimentological and geochemical evidence. Palaeogeography,Palaeoclimatology,Palaeoecology,586: 110781.
[82]	Ruhl M,Hesselbo S P,Jenkyns H C,Xu W M,Silva R L,Matthews K J,Mather T A,Mac Niocaill C,Riding J B. 2022. Reduced plate motion controlled timing of Early Jurassic Karoo-Ferrar large igneous province volcanism. Science Advances,8: eabo0866.
[83]	Schouten S,Hop Mans E C,Schefuß E,Sinninghe Damsté J S. 2002. Distributional variations in Marine crenarchaeotal membrane lipids: a new tool for reconstructing ancient sea water temperatures?Earth and Planetary Science Letters,204(1-2): 265-274.
[84]	Su K M,Lu J G,Zhang G W,Chen S J,Li Y,Xiao Z L,Wang P,Qiu W. 2018. Origin of natural gas in Jurassic Da’anzhai Member in the western part of central Sichuan Basin,China. Journal of Petroleum Science and Engineering,167: 890-899.
[85]	Thibault N,Ruhl M,Ull Mann C V,Korte C,Kemp D B,Gröcke D R,Hesselbo S P. 2018. The wider context of the Lower Jurassic Toarcian oceanic anoxic event in Yorkshire coastal outcrops,UK. Proceedings of the Geologists’ Association,129: 372-391.
[86]	Ull Mann C V,Boyle R,Duarte L V,Hesselbo S P,Kase Mann S A,Klein T,Lenton T M,Piazza V,Aberhan M. 2020. Warm afterglow from the Toarcian Oceanic Anoxic Event drives the success of deep-adapted brachiopods. Scientific Reports,10: 6549.
[87]	Wang E Z,Feng Y,Guo T L,Li M W,Xiong L,Lash G G,Dong X X,Wang T,Ouyang J S. 2023a. Sedimentary differentiation triggered by the Toarcian Oceanic Anoxic Event and formation of lacustrine shale oil reservoirs: organic matter accumulation and pore system evolution of the Early Jurassic sedimentary succession,Sichuan Basin,China. Journal of Asian Earth Sciences,256: 105825.
[88]	Wang E Z,Guo T L,Li M W,Xiong L,Dong X X,Wang T,Ouyang J S. 2023b. Reservoir characteristics and oil properties of a lacustrine shale system: Early Jurassic black shale from the Sichuan Basin,SW China. Journal of Asian Earth Sciences,242: 105491.
[89]	Wang Y D,Mosbrugger V,Zhang H. 2005. Early to Middle Jurassic vegetation and climatic events in the Qaidam Basin,Northwest China. Palaeogeography,Palaeoclimatology,Palaeoecology,224: 200-216.
[90]	Xu W M,Ruhl M,Jenkyns H,Hesselbo S,Riding J,Selby D,Naafs B,Weijers J,Pancost R,Tegelaar E,Idiz E. 2017a. Carbon sequestration in an expanded lake system during the Toarcian oceanic anoxic event. Nature Geoscience,10: 129-134.
[91]	Xu Q L,Liu B,Ma Y S,Song X M,Wang Y J,Xin X K,Chen Z X. 2017b. Controlling factors and dynamical Formation models of lacustrine organic matter accumulation for the Jurassic Da’anzhai Member in the central Sichuan Basin,southwestern China. Marine and Petroleum Geology,86: 1391-1405.
[92]	Xu W,Ruhl M,Jenkyns H C,Leng M J,Huggett J M,Minisini D,Ull Mann C V,Riding J B,Weijers J W,Storm M S,Percival L M. 2018. Evolution of the Toarcian(Early Jurassic)carbon-cycle and global climatic controls on local sedimentary processes(Cardigan Bay Basin,UK). Earth and Planetary Science Letters,484: 396-411.
[93]	Yang J H,Cawood P A,Du Y S,Li W Q,Yan J X. 2016. Reconstructing Early Permian tropical climates from chemical weathering indices. Geological Society of America Bulletin,128(5-6): 739-751.
[94]	Zhang P X,Yang M F,Lu J,Jiang Z F,Zhou K,Liu H Q,He Z,Wang Y,Bian X,Shao L Y,Hilton J,Bond D P G. 2023. Middle Jurassic terrestrial environmental and floral changes linked to volcanism: evidence from the Qinghai-Tibet Plateau,China. Global and Planetary Change,223: 104094.
[95]	Zhang Q,Gong E,Zhang Y,Guan C. 2021. Early Jurassic(Toarcian)warming identified from lacustrine sediments of eastern Liaoning,China. Geological Magazine,158: 1194-1208.
[96]	Zhang Q,Gong E P,Zhang Y L,Guan C Q. 2022. Palynoflora and palaeoclimate of the late Early Jurassic(Toarcian)in eastern Liaoning,China. Palaeobiodiversity and Palaeoenvironments,102: 73-88.
[97]	Zhang Z H,Wang C S,Lü D W,Hay W W,Wang T T,Cao S. 2020. Precession-scale climate forcing of peatland wildfires during the early middle Jurassic greenhouse period. Global and Planetary Change,184: 103051.
[98]	Zhou K,Lu J,Zhang S,Yang M F,Gao R,Shao L Y,Hilton J. 2022. Volcanism driven Pliensbachian(Early Jurassic)terrestrial climate and environment perturbations. Global and Planetary Change,216: 103919.

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