[1] 常梦瑶. 2017. 金沙江缝合带巴塘竹巴笼地区基性岩系岩石地球化学特征及意义[D]. 成都：成都理工大学：6-11.

Chang Mengyao. 2017. Geochemical characteristics and significance of mafic rocks from Batang Zhubalong area along Jinshajiang suture zone[D]. Chengdu: Chengdu University of Technology: 6-11.
[2] 陈红汉，吴悠，肖秋苟，等. 2010. 昌都盆地古油藏的流体包裹体证据[J]. 地质学报，84（10）：1457-1469.

Chen Honghan, Wu You, Xiao Qiugou, et al. 2010. Fluid inclusion evidence of paleo-oil reservoirs in Changdu Basin, Tibet[J]. Acta Geologica Sinica, 84(10): 1457-1469.
[3] 杜德勋，罗建宁，李兴振. 1997. 昌都地块沉积演化与古地理[J]. 岩相古地理，17（4）：1-17.

Du Dexun, Luo Jianning, Li Xingzhen. 1997. Sedimentary characteristics of the Wuxue Formation in the Susong Fanchang region, Anhui[J]. Lithofacies Palaeogeography, 17(4): 1-17.
[4] 关绍曾. 1978. 南雄盆地的介形类化石及其地层意义[J]. 地层古生物论文集（1）：152-179.

Guang Shaozeng. 1978. On fossil ostracodas from the Nanxiong Basin and their stratigraphic significance[J]. Essays on Stratigraphic Paleontology (1): 152-179.
[5] 李余亮. 2018. 广东省韶关市丹霞盆地长坝组沉积特征与古气候研究[D]. 南昌：东华理工大学：26-31.

Li Yuliang. 2018. Sedimentary characteristics and paleoclimate of the Changba Formation in the Danxia Basin, Shaoguan city, Guangdong province, South China[D]. Nanchang: East China University of Technology: 26-31.
[6] 潘桂棠，李兴振，王立全，等. 2002. 青藏高原及邻区大地构造单元初步划分[J]. 地质通报，21（11）：701-707.

Pan Guitang, Li Xingzhen, Wang Liquan, et al. 2002. Preliminary division of tectonic units of the Qinghai-Tibet Plateau and its adjacent regions[J]. Geological Bulletin of China, 21(11): 701-707.
[7] 谭富文，王剑，付修根，等. 2009. 藏北羌塘盆地基底变质岩的锆石SHRIMP年龄及其地质意义[J]. 岩石学报，25（1）：139-146.

Tan Fuwen, Wang Jian, Fu Xiugen, et al. 2009. U-Pb zircon SHRIMP age of metamorphic rocks from the basement of the Qiangtang Basin, northern Tibet, and its geological significance[J]. Acta Petrologica Sinica, 25(1): 139-146.
[8] 王凤之，陈留勤，郭福生，等. 2018. 江西信江盆地晚白垩世塘边组成壤碳酸盐岩碳、氧同位素特征[J]. 岩石矿物学杂志，37（1）：143-151.

Wang Fengzhi, Chen Liuqin, Guo Fusheng, et al. 2018. Carbon and oxygen isotopic compositions of pedogenic carbonates from the Late Cretaceous Tangbian Formation in the Xinjiang Basin, Jiangxi province[J]. Acta Petrologica et Mineralogica, 37(1): 143-151.
[9] 王辉. 2005. 青藏高原羌塘—三江地区残留微陆块[J]. 云南地质，25（1）：1-10.

Wang Hui. 2005. The relict microcontinent in Qiangtang-Sanjiang area of Qing-Zang Plateau[J]. Yunnan Geology, 25(1): 1-10.
[10] 王永栋，孙柏年，黄成敏，等. 2015. 地史时期古大气二氧化碳变化趋势与温室气候：以中生代白垩纪为例[J]. 自然杂志，37（2）：108-114.

Wang Yongdong, Sun Bonian, Huang Chengmin, et al. 2015. Variation of paleo-CO2 and greenhouse climate in the geological history: A case study from the Cretaceous of the Mesozoic[J]. Chinese Journal of Nature, 37(2): 108-114.
[11] 王宇佳. 2019. 江西广丰晚白垩世周田组沉积特征与古气候分析[D]. 南昌：东华理工大学：33-36.

Wang Yujia. 2019. Sedimentary characteristics and paleoclimate of the Zhoutian Formation in the Guangfeng Basin of Jiangxi province[D]. Nanchang: East China University of Technology: 33-36.
[12] 吴喆. 2022. 江达—维西陆缘弧贡觉段三叠纪火山岩地球化学特征、岩石成因及其大地构造意义[D]. 北京：中国地质科学院：10-15.

Wu Zhe. 2022. Geochemical characteristics, petrogenesis and tectonic significance of Triassic volcanic rocks in Gongjue of Jiangda-Weixi continental margin arc[D]. Beijing: Chinese Academy of Geological Sciences: 10-15.
[13] 席党鹏，万晓樵，李国彪，等. 2019. 中国白垩纪综合地层和时间框架[J]. 中国科学：地球科学，49（1）：257-288.

Xi Dangpeng, Wan Xiaoqiao, Li Guobiao, et al. 2019. Cretaceous comprehensive strata and time frame in China[J]. Science China Earth Science, 49(1): 257-288.
[14] 西藏地质调查局. 2007. 巴苏、贡吉、然乌和芒康县1/25万区域地质调查报告[R].

Geological Survey of Xizang. 2007. 1/250, 000 regional geological survey report of Basu, Gongji, Ranwu and Mangkang counties[R].
[15] 徐颖. 2020. 西藏昌都盆地古近纪沉积特征分析[D]. 南昌：东华理工大学：7-14.

Xu Ying. 2020. Analysis of Paleogene sedimentary characteristics in Changdu Basin, Tibet[D]. Nanchang: East China University of Technology: 7-14.
[16] 占王忠，谭富文，陈明. 2018. 藏东昌都盆地沉积构造演化及油气远景分析[J]. 沉积与特提斯地质，38（4）：85-96.

Zhan Wangzhong, Tan Fuwen, Chen Ming. 2018. Sedimentary-tectonic evolution and hydrocarbon potential in the Qamdo Basin, eastern Xizang[J]. Sedimentary Geology and Tethyan Geology, 38(4): 85-96.
[17] 张治波，徐颖，苗艳菊，等. 2022. 昌都盆地古近系贡觉组物源及其沉积环境[J]. 沉积学报，40（6）：1561-1581.

Zhang Zhibo, Xu Ying, Miao Yanju, et al. 2022. Provenance and sedimentary environment of Paleogene Gongjue Formation in Qamdo Basin[J]. Acta Sedimentologica Sinica, 40(6): 1561-1581.
[18] 周天军，陈晓龙，左萌，等. 2023. 地球气候敏感度研究的现状和未来[J]. 第四纪研究，43（2）：604-624.

Zhou Tianjun, Chen Xiaolong, Zuo Meng, et al. 2023. Earth's climate sensitivity: Methods, climate feedback processes, progresses and prospects[J]. Quaternary Sciences, 43(2): 604-624.
[19] Ando A, Nakano T, Kaiho K, et al. 2009. Onset of seawater 87Sr/86Sr excursion prior to Cenomanian-Turonian oceanic anoxic event 2? New Late Cretaceous strontium isotope curve from the central Pacific Ocean[J]. The Journal of Foraminiferal Research, 39(4): 322-334.
[20] Arens N C, Jahren A H, Amundson R. 2000. Can C3 plants faithfully record the carbon isotopic composition of atmospheric carbon dioxide?[J]. Paleobiology, 26(1): 137-164.
[21] Barclay R S, Mcelwain J C, Sageman B B. 2010. Carbon sequestration activated by a volcanic CO2 pulse during ocean anoxic event 2[J]. Nature Geoscience, 3(3): 205-208.
[22] Barral A, Gomez B, Fourel F, et al. 2017a. CO2 and temperature decoupling at the million-year scale during the Cretaceous greenhouse[J]. Scientific Reports, 7(1): 8310.
[23] Barral A, Gomez B, Legendre S, et al. 2017b. Evolution of the carbon isotope composition of atmospheric CO2 throughout the Cretaceous[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 471: 40-47.
[24] Bergman N M, Lenton T M, Watson A J. 2004. COPSE: A new model of biogeochemical cycling over Phanerozoic time[J]. American Journal of Science, 304(5): 397-437.
[25] Berner R A. 2006. Inclusion of the weathering of volcanic rocks in the GEOCARBSULF model[J]. American Journal of Science, 306(5): 295-302.
[26] Berner R A, Kothavala Z. 2001. Geocarb III: A revised model of atmospheric CO2 over Phanerozoic time[J]. American Journal of Science, 301(2): 182-204.
[27] Bice K L, Birgel D, Meyers P A, et al. 2006. A multiple proxy and model study of Cretaceous upper ocean temperatures and atmospheric CO2 concentrations[J]. Paleoceanography, 21(2): PA2002.
[28] Boudinot F G, Kopf S, Dildar N, et al. 2021. Carbon cycling during oceanic anoxic event 2: Compound-specific carbon isotope evidence from the western interior seaway[J]. Paleoceanography and Paleoclimatology, 36(9): e2021PA004287.
[29] Bralower T J, Fullagar P D, Paull C K, et al. 1997. Mid-Cretaceous strontium-isotope stratigraphy of deep-sea sections[J]. GSA Bulletin, 109(11): 1421-1442.
[30] Breecker D O, Sharp Z D, McFadden L D. 2009. Seasonal bias in the formation and stable isotopic composition of pedogenic carbonate in modern soils from central New Mexico[J]. GSA Bulletin, 121(3/4): 630-640.
[31] Breecker D O, Sharp Z D, McFadden L D. 2010. Atmospheric CO2 concentrations during ancient greenhouse climates were similar to those predicted for A.D. 2100[J]. Proceedings of the National Academy of Sciences of the United States of America, 107(2): 576-580.
[32] Cerling T E. 1992. Use of carbon isotopes in paleosols as an indicator of the P(CO2) of the paleoatmosphere[J]. Global Biogeochemical Cycles, 6(3): 307-314.
[33] Choquette P W, Pray L C. 1970. Geologic nomenclature and classification of porosity in sedimentary carbonates[J]. AAPG Bulletin, 54(2): 207-250.
[34] Corentin P, Pucéat E, Pellenard P, et al. 2022. Hafnium-neodymium isotope evidence for enhanced weathering and uplift-climate interactions during the Late Cretaceous[J]. Chemical Geology, 591: 120724.
[35] Cotton J M, Sheldon N D. 2012. New constraints on using paleosols to reconstruct atmospheric pCO2 [J]. Geological Society of America Bulletin, 124(9/10): 1411-1423.
[36] Damsté J S S, Kuypers M M M, Pancost R D, et al. 2008. The carbon isotopic response of algae, (cyano) bacteria, archaea and higher plants to the Late Cenomanian perturbation of the global carbon cycle: Insights from biomarkers in black shales from the Cape Verde Basin (DSDP Site 367)[J]. Organic Geochemistry, 39(12): 1703-1718.
[37] Diefendorf A F, Freeman K H, Wing S L, et al. 2015. Paleogene plants fractionated carbon isotopes similar to modern plants[J]. Earth and Planetary Science Letters, 429: 33-44.
[38] Du B X, Lei X T, Zhang M Z, et al. 2018. Late Early Cretaceous climate and pCO2 estimates in the Liupanshan Basin, Northwest China[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 503: 26-39.
[39] Ekart D D, Cerling T E, Montanez I P, et al. 1999. A 400 million year carbon isotope record of pedogenic carbonate: Implications for paleoatmospheric carbon dioxide[J]. American Journal of Science, 299(10): 805-827.
[40] Farquhar G D, O'Leary M H, Berry J A. 1982. On the relationship between carbon isotope discrimination and the intercellular carbon dioxide concentration in leaves[J]. Functional Plant Biology, 9(2): 121-137.
[41] Fletcher T L, Greenwood D R, Moss P T, et al. 2014. Paleoclimate of the Late Cretaceous (Cenomanian-Turonian) portion of the Winton Formation, central-western Queensland, Australia: New observations based on clamp and bioclimatic analysis[J]. Palaios, 29(3): 121-128.
[42] Forster A, Schouten S, Moriya K, et al. 2007. Tropical warming and intermittent cooling during the Cenomanian/Turonian oceanic anoxic event 2: Sea surface temperature records from the equatorial Atlantic[J]. Paleoceanography, 22(1): PA1219.
[43] Foster G L, Royer D L, Lunt D J. 2017. Future climate forcing potentially without precedent in the last 420 million years[J]. Nature Communications, 8: 14845.
[44] Franks P J, Royer D L, Beerling D J, et al. 2014. New constraints on atmospheric CO2 concentration for the Phanerozoic[J]. Geophysical Research Letters, 41(13): 4685-4694.
[45] Freeman K H, Hayes J M. 1992. Fractionation of carbon isotopes by phytoplankton and estimates of ancient CO2 levels[J]. Global Biogeochemical Cycles, 6(2): 185-198.
[46] Friedrich O, Norris R D, Erbacher J. 2012. Evolution of Middle to Late Cretaceous oceans-A 55 m.y. record of earth's temperature and carbon cycle[J]. Geology, 40(2): 107-110.
[47] Hasegawa T. 2003. Cretaceous terrestrial paleoenvironments of northeastern Asia suggested from carbon isotope stratigraphy: Increased atmospheric pCO2-induced climate[J]. Journal of Asian Earth Sciences, 21(8): 849-859.
[48] Hong S K, Lee Y I. 2012. Evaluation of atmospheric carbon dioxide concentrations during the Cretaceous[J]. Earth and Planetary Science Letters, 327/328: 23-28.
[49] Huang C M, Retallack G J, Wang C S, et al. 2013. Paleoatmospheric pCO2 fluctuations across the Cretaceous-Tertiary boundary recorded from paleosol carbonates in NE China[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 385: 95-105.
[50] Huang K N, Opdyke N D, Li J G, et al. 1992. Paleomagnetism of Cretaceous rocks from eastern Qiangtang Terrane of Tibet[J]. Journal of Geophysical Research: Solid Earth, 97(B2): 1789-1799.
[51] Huber B T, Macleod K G, Watkins D K, et al. 2018. The rise and fall of the Cretaceous hot greenhouse climate[J]. Global and Planetary Change, 167: 1-23.
[52] Hyland E G, Sheldon N D. 2013. Coupled CO2-climate response during the Early Eocene climatic optimum[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 369: 125-135.
[53] Jones C E, Jenkyns H C. 2001. Seawater strontium isotopes, oceanic anoxic events, and seafloor hydrothermal activity in the Jurassic and Cretaceous[J]. American Journal of Science, 301(2): 112-149.
[54] Joo Y J, Sageman B B, Hurtgen M T. 2020. Data-model comparison reveals key environmental changes leading to Cenomanian-Turonian oceanic anoxic event 2[J]. Earth-Science Reviews, 203: 103123.
[55] Kohn M J. 2010. Carbon isotope compositions of terrestrial C3 plants as indicators of (paleo)ecology and (paleo)climate[J]. Proceedings of the National Academy of Sciences of the United States of America, 107(46): 19691-19695.
[56] Kohn M J. 2016. Carbon isotope discrimination in C3 land plants is independent of natural variations in pCO2 [J]. Geochemical Perspectives Letters, 2(1): 35-43.
[57] Laugié M, Donnadieu Y, Ladant J B, et al. 2020. Stripping back the modern to reveal the Cenomanian-Turonian climate and temperature gradient underneath[J]. Climate of the Past, 16(3): 953-971.
[58] Leier A, Quade J, DeCelles C P, et al. 2009. Stable isotopic results from paleosol carbonate in South Asia: Paleoenvironmental reconstructions and selective alteration[J]. Earth and Planetary Science Letters, 279(3/4): 242-254.
[59] Li H, Yu J X, Mcelwain J C, et al. 2019. Reconstruction of atmospheric CO2 concentration during the Late Changhsingian based on fossil conifers from the Dalong Formation in South China[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 519: 37-48.
[60] Li J, Wen X Y, Huang C M. 2016. Lower Cretaceous paleosols and paleoclimate in Sichuan Basin, China[J]. Cretaceous Research, 62: 154-171.
[61] Li L, DeCelles P, Kapp P, et al. 2024. Constraining carbonate diagenesis using clumped isotope temperatures and U-Pb dating: A case study and implications for paleoelevation interpretations in western central Tibet[J]. Geochimica et Cosmochimica Acta, 374: 1-14.
[62] Li X H, Jenkyns H C, Zhang C K, et al. 2014. Carbon isotope signatures of pedogenic carbonates from SE China: Rapid atmospheric pCO2 changes during middle-late Early Cretaceous time[J]. Geological Magazine, 151(5): 830-849.
[63] Ludvigson G A, Joeckel R M, Murphy L R, et al. 2015. The emerging terrestrial record of Aptian-Albian global change[J]. Cretaceous Research, 56: 1-24.
[64] Matsumoto H, Coccioni R, Frontalini F, et al. 2022. Mid-Cretaceous marine Os isotope evidence for heterogeneous cause of oceanic anoxic events[J]. Nature Communications, 13(1): 239.
[65] Mays C, Steinthorsdottir M, Stilwell J D. 2015. Climatic implications of Ginkgoites waarrensis Douglas emend. From the south polar Tupuangi flora, Late Cretaceous (Cenomanian), Chatham Islands[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 438: 308-326.
[66] Mckenzie N R, Horton B K, Loomis S E, et al. 2016. Continental arc volcanism as the principal driver of icehouse-greenhouse variability[J]. Science, 352(6284): 444-447.
[67] Montañez I P. 2013. Modern soil system constraints on reconstructing deep-time atmospheric CO2 [J]. Geochimica et Cosmochimica Acta, 101: 57-75.
[68] Nemoto T, Hasegawa T. 2011. Submillennial resolution carbon isotope stratigraphy across the oceanic anoxic event 2 horizon in the Tappu section, Hokkaido, Japan[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 309(3/4): 271-280.
[69] Orr T J, Wurster C M, Roberts E M, et al. 2022. Paleoatmospheric CO2 oscillations through a cool Middle/Late Cretaceous recorded from pedogenic carbonates in Africa[J]. Cretaceous Research, 135: 105191.
[70] Passalia M G. 2009. Cretaceous pCO2 estimation from stomatal frequency analysis of gymnosperm leaves of Patagonia, Argentina[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 273(1/2): 17-24.
[71] Qi Z L, Li Y L, Wang C S. 2021. Hydrocarbon potential of the Late Permian and the Late Triassic source rocks from the Qamdo (Changdu) Basin, eastern Tibet and its linkage with the sea level change[J]. Frontiers in Earth Science, 9: 778025.
[72] Rao Z G, Chen F H, Cheng H, et al. 2013. High-resolution summer precipitation variations in the western Chinese Loess Plateau during the last glacial[J]. Scientific Reports, 3: 2785.
[73] Rao Z G, Guo W K, Cao J T, et al. 2017. Relationship between the stable carbon isotopic composition of modern plants and surface soils and climate: A global review[J]. Earth-Science Reviews, 165: 110-119.
[74] Retallack G J. 2009. Greenhouse crises of the past 300 million years[J]. Geological Society of America Bulletin, 121(9/10): 1441-1455.
[75] Retallack G J, Conde G D. 2020. Deep time perspective on rising atmospheric CO2 [J]. Global and Planetary Change, 189: 103177.
[76] Retallack G J, Dilcher D L. 2012. Outcrop versus core and geophysical log interpretation of mid-Cretaceous paleosols from the Dakota Formation of Kansas[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 329/330: 47-63.
[77] Romanek C S, Grossman E L, Morse J W. 1992. Carbon isotopic fractionation in synthetic aragonite and calcite: Effects of temperature and precipitation rate[J]. Geochimica et Cosmochimica Acta, 56(1): 419-430.
[78] Roy S, Sanyal P, Ghosh P, et al. 2021. Atmospheric CO2 estimates based on Gondwanan (Indian) pedogenic carbonates reveal positive linkage with Mesozoic temperature variations[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 582: 110638.
[79] Sandler A. 2006. Estimates of atmospheric CO2 levels during the mid-Turonian derived from stable isotope composition of paleosol calcite from Israel[M]//Alonso-Zarza A M, Tanner L H. Paleo-environmental record and applications of calcretes and palustrine carbonates. Boulder: Geological Society of America: 75-88.
[80] Scaife J D, Ruhl M, Dickson A J, et al. 2017. Sedimentary mercury enrichments as a marker for submarine large igneous province volcanism? Evidence from the mid-Cenomanian event and oceanic anoxic event 2 (Late Cretaceous)[J]. Geochemistry, Geophysics, Geosystems, 18(12): 4253-4275.
[81] Schlanser K, Diefendorf A F, Greenwood D R, et al. 2020. On geologic timescales, plant carbon isotope fractionation responds to precipitation similarly to modern plants and has a small negative correlation with pCO2 [J]. Geochimica et Cosmochimica Acta, 270: 264-281.
[82] Shang F. 2016. Mesozoic history of the southeastern Tibetan Plateau: Sediment provenance, paleoclimate, and surface elevation history[D]. Morgantown: West Virginia University: 1-77.
[83] Sheldon N D, Tabor N J. 2009. Quantitative paleoenvironmental and paleoclimatic reconstruction using paleosols[J]. Earth-Science Reviews, 95(1/2): 1-52.
[84] Stubbs T L, Benton M J, Elsler A, et al. 2019. Morphological innovation and the evolution of hadrosaurid dinosaurs[J]. Paleobiology, 45(2): 347-362.
[85] Tajika E. 1999. Carbon cycle and climate change during the Cretaceous inferred from a biogeochemical carbon cycle model[J]. Island Arc, 8(2): 293-303.
[86] van Bentum E C, Reichart G J, Forster A, et al. 2012. Latitudinal differences in the amplitude of the OAE-2 carbon isotopic excursion: pCO2 and paleo productivity[J]. Biogeosciences, 9(2): 717-731.
[87] Varela A N, Raigemborn M S, Richiano S, et al. 2018. Late Cretaceous paleosols as paleoclimate proxies of high-latitude southern Hemisphere: Mata Amarilla Formation, Patagonia, Argentina[J]. Sedimentary Geology, 363: 83-95.
[88] Wan C B, Wang D H, Zhu Z P, et al. 2011. Trend of Santonian (Late Cretaceous) atmospheric CO2 and global mean land surface temperature: Evidence from plant fossils[J]. Science China Earth Sciences, 54(9): 1338-1345.
[89] Wang Q, Wang X, Wei H T, et al. 2019. Climatic significance of the stable carbon isotopic composition of surface soils in northern Iran and its application to an Early Pleistocene loess section[J]. Organic Geochemistry, 127: 104-114.
[90] Wang Y D, Huang C M, Sun B N, et al. 2014. Paleo-CO2 variation trends and the Cretaceous greenhouse climate[J]. Earth-Science Reviews, 129: 136-147.
[91] Zhao X J. 1983. Phylogeny and evolutionary stages of Dinosauria[J]. Acta Palaeontologica Polonica, 28(1/2): 295-306.