[1] 陈鸿明，侯光良，文德卓玛，等. 2023. 末次冰盛期与全新世青藏高原松属植被分布及其演变[J]. 第四纪研究， 43（5）：1211-1224.

Chen Hongming, Hou Guangliang, Zhuoma Wende, et al. 2023. Distribution and evolution of Pinus spp. vegetation in the Tibetan Plateau during the Last Glacial Maximum and Holocene[J]. Quaternary Sciences, 43(5): 1211-1224.
[2] 陈玉美，舒强，张茂恒，等. 2014. 南京下蜀黄土记录的 250~100 ka期间的环境演化信息[J]. 地质科技情报，33（6）：55-59，77.

Chen Yumei, Shu Qiang, Zhang Maoheng, et al. 2014. Environmental evolution information recorded in the Xiashu loess (250-100 ka) in Nanjing, China[J]. Geological Science and Technology Information, 33(6): 55-59, 77.
[3] 方晶，胡克，杨永强，等. 2009. 辽东半岛长兴岛八岔沟古泻湖型泥炭的形成及全新世最高海平面[J]. 吉林大学学报（地球科学版），39（3）：461-469.

Fang Jing, Hu Ke, Yang Yongqiang, et al. 2009. Paleoenvironments of Holocene lagoon peat and the highest sea-level in Bachagou, Changxing Island, Liaodong Peninsula[J]. Journal of Jilin University (Earth Science Edition), 39(3): 461-469.
[4] 方晶，杨永强，马宏伟，等. 2012. 辽东半岛大孤山古溺谷平原沉积环境的复原：基于岩心黏土混浊水电导率和pH值以及硅藻组合[J]. 海洋学报，34（6）：133-141.

Fang Jing, Yang Yongqiang, Ma Hongwei, et al. 2012. Edimentary environmental analysis based on the electric conductivity and pH of stirred clayed drilling cores in water and diatom recovered from the old drowned valley plain in the Dagu Mountain, Liaodong Peninsula in China[J]. Acta Oceanologica Sinica, 34(6): 133-141.
[5] 符文侠，何宝林，孙试斌，等. 1987. 晚更新世末期以来辽东半岛东部滨海沉积相与沉积环境的探讨[J]. 地理科学，7（1）：29-34.

Fu Wenxia, He Baolin, Sun Shibin, et al. 1987. An approach to the facies and environment of the littoral deposits in the east Liaodong Peninsula since the late stage of the Late Pleistocene[J]. Scientia Geographica Sinica, 7(1): 29-34.
[6] 符文侠，焦亚宁，魏成凯. 1985. 从海积地貌和沉积特征看辽东半岛南部沿岸全新世海水入侵趋势[J]. 海洋湖沼通报，（3）：37-41.

Fu Wenxia, Jiao Yaning, Wei Chengkai. 1985. Understanding the trend of the Holocene transgression through the characteristic of the marine dipositional configuration and sedimentation on the southwest coast in the Liaodong Peninsula[J]. Transactions of Oceanology and Limnology, (3): 37-41.
[7] 符文侠，王玉广，刘国海. 1995. 辽宁沿海泥炭堆积与全新世海面变化[J]. 黄渤海海洋，13（2）：23-32.

Fu Wenxia, Wang Yuguang, Liu Guohai. 1995. Peat accumulation and sea level changes in Holocene along the coast of Liaoning[J]. Journal of Oceanography of Huanghai & Bohai Seas, 13(2): 23-32.
[8] 付晓芬. 2018. 太原盆地20ka以来孢粉组合与古环境研究[D]. 成都: 成都理工大学.

Fu Xiaofen. 2018. Sporollen assemblages and palaeoenvironmental evolution since 20ka BP in Taiyuan Basin[D]. Chengdu: Chengdu University of Technology.
[9] 胡梦珺，庄静，孙文丽，等. 2023. 青藏高原东北部全新世常量元素地球化学特征及环境演变[J]. 中国沙漠，43（2）：11-20.

Hu Mengjun, Zhuang Jing, Sun Wenli, et al. 2023. Geochemical characteristics of major elements and environmental evolution in the Holocene in the northeastern Tibetan Plateau[J]. Journal of Desert Research, 43(2): 11-20.
[10] 李雪铭. 1997. 辽南大莲泡积物的沉积特征及古环境变化[J]. 沉积学报，15（1）：80-84.

Li Xueming. 1997. Sedimentary characteristics of the Dalianpao sediment in southern Liaoning and its paleo-environment changes[J]. Acta Sedimentologica Sinica, 15(1): 80-84.
[11] 马瑞丰，张威，金培红，等. 2021. 辽宁南部金州地区距今13.5 ka以来古植被古气候变化[J]. 第四纪研究，41（1）：43-50.

Ma Ruifeng, Zhang Wei, Jin Peihong, et al. 2021. Palaeo-vegetation and palaeo-climate changes since 13.5 cal. ka B.P. in Jinzhou, southern of Liaoning province[J]. Quaternary Sciences, 41(1): 43-50.
[12] 毛沛妮，庞奖励，黄春长，等. 2017. 汉江上游黄土常量元素地球化学特征及区域对比[J]. 地理学报，72（2）: 279-291.

Mao Peini, Pang Jiangli, Huang Chunchang, et al. 2017. Chemical weathering characteristics and regional comparative study of the loess deposits in the upper Hanjiang River[J]. Acta Geographica Sinica, 72(2): 279-291.
[13] 史本恒. 2006. 辽东半岛全新世最大海侵的考古学观察[J]. 四川文物（6）：37-41.

Shi Benheng. 2006. Archaeological discovery of the largest palaeogeographical transgression in Liaodong Peninsula[J]. Sichuan Cultural Relics, (6): 37-41.
[14] 王明达，梁洁，侯居峙，等. 2016. 青藏高原湖泊表层沉积物GDGTs分布特征及其影响因素[J]. 中国科学：地球科学，46（2）：167-183.

Wang Mingda, Liang Jie, Hou Juzhi, et al. 2016. Distribution of GDGTs in lake surface sediments on the Tibetan Plateau and its influencing factors[J]. Science China Earth Sciences, 46(2): 167-183.
[15] 张威，马瑞丰，刘亮，等. 2022. 辽东半岛全新世沉积物记录的古气候变化研究进展[J]. 沉积学报，40（5）：1355-1366.

Zhang Wei, Ma Ruifeng, Liu Liang, et al. 2022. Research progress on Paleo-climate change from Holocene sediment records in Liaodong Peninsula[J]. Acta Sedimentologica Sinica, 40(5): 1355-1366.
[16] 中国科学院贵阳地球化学研究所第四纪孢粉组，C14组. 1977. 辽宁省南部一万年来自然环境的演变[J]. 中国科学：地球科学，（6）：603-614.

Quaternary Sporopollen Formation, Guiyang Institute of Geochemistry, Chinese Academy of Sciences, Group C 14. 1977. Evolution of the natural environment in the southern Liaoning province during 10,000 years[J]. Science China Earth Sciences, (6): 603-614.
[17] 钟以章，高常波. 1988. 辽东半岛全新世海平面变化及近5000年来的地壳运动[J]. 海洋科学，12（1）：4-8.

Zhong Yizhang, Gao Changbo. 1988. Sea level changes in the Holocene and crustal movement in the past 5000 years in the Liaodong Peninsula[J]. Marine Sciences, 12(1): 4-8.
[18] 周家兴，吴利杰，于娟，等. 2019. 铜川地区11.4~1.5 ka B.P.期间黄土地球化学风化特征及其古气候意义[J]. 地球与环境，47（1）：64-73.

Zhou Jiaxing, Wu Lijie, Yu Juan, et al. 2019. Characteristics of geochemical weathering of loess in the Tongchuan area during 11.4-1.5 ka B.P. and its paleoclimatic implications[J]. Earth and Environment, 47(1): 64-73.
[19] Antonioli F, Ferranti L, Fontana A, et al. 2009. Holocene relative sea-level changes and vertical movements along the Italian and Istrian coastlines[J]. Quaternary International, 206(1/2): 102-133.
[20] Borges J, Huh Y. 2007. Petrography and chemistry of the bed sediments of the Red River in China and Vietnam: Provenance and chemical weathering[J]. Sedimentary Geology, 194(3/4): 155-168.
[21] Deng C L, Shaw J, Liu Q S, et al. 2006. Mineral magnetic variation of the Jingbian loess/paleosol sequence in the northern Loess Plateau of China: Implications for Quaternary development of Asian aridification and cooling[J]. Earth and Planetary Science Letters, 241(1/2): 248-259.
[22] Dykoski C A, Edwards R L, Cheng H, et al. 2005. A high-resolution, absolute-dated Holocene and deglacial Asian monsoon record from Dongge cave, China[J]. Earth and Planetary Science Letters, 233(1/2): 71-86.
[23] Emiliani C. 1970. Pleistocene paleotemperatures[J]. Science, 168(3933): 822-825.
[24] Giaime M, Salem A, Wang Y N, et al. 2022. Holocene evolution and signature of environmental change of the Burullus lagoon (Nile Delta) deciphered from a long sediment record[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 590: 110861.
[25] Hatté C, Morvan J, Noury C, et al. 2001. Is classical acid-alkali-acid treatment responsible for contamination? An alternative proposition[J]. Radiocarbon, 43(2A): 177-182.
[26] Jouzel J, Hoffmann G, Parrenin F, et al. 2002. Atmospheric oxygen 18 and sea-level changes[J]. Quaternary Science Reviews, 21(1/2/3): 307-314.
[27] Küçükuysal C, Yavuz N. 2017. Multi-proxy records of Quaternary fluvio-lacustrine sediments around Lakes Eymir and Mogan, Ankara (central Anatolia, Turkey)[J]. Environmental Earth Sciences, 76(16): 587.
[28] Liu J B, Chen J H, Zhang X J, et al. 2015. Holocene East Asian summer monsoon records in northern China and their inconsistency with Chinese stalagmite δ18O records[J]. Earth-Science Reviews, 148: 194-208.
[29] Liu X X, Vandenberghe J, An Z S, et al. 2016. Grain size of Lake Qinghai sediments: Implications for riverine input and Holocene monsoon variability[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 449: 41-51.
[30] Ma L S, Gao C Y, Kattel G R, et al. 2018. Evidence of Holocene water level changes inferred from diatoms and the evolution of the Honghe peatland on the Sanjiang Plain of Northeast China[J]. Quaternary International, 476: 82-94.
[31] O’brien S R, Mayewski P A, Meeker L D, et al. 1995. Complexity of Holocene climate as reconstructed from a Greenland ice core[J]. Science, 270(5244): 1962-1964.
[32] Reimer P J, Bard E, Bayliss A, et al. 2013. IntCal13 and Marine13 radiocarbon age calibration curves 0-50,000 years cal BP[J]. Radiocarbon, 55(4): 1869-1887.
[33] Roddaz M, Viers J, Brusset S, et al. 2006. Controls on weathering and provenance in the Amazonian Foreland Basin: Insights from major and trace element geochemistry of Neogene Amazonian sediments[J]. Chemical Geology, 226(1/2): 31-65.
[34] Sheldon N D, Tabor J N. 2009. Quantitative paleoenvironmental and paleoclimatic reconstruction using paleosols[J]. Earth-Science Reviews, 95(1/2): 1-52.
[35] Stuiver M, Braziunas T F, Grootes P M, et al. 1997. Is there evidence for solar forcing of climate in the GISP2 oxygen isotope record?[J]. Quaternary Research, 48(3): 259-266.
[36] Sun Q L, Zhou J, Shen J, et al. 2006. Environmental characteristics of Mid-Holocene recorded by lacustrine sediments from Lake Daihai, north environment sensitive zone, China[J]. Science China Earth Sciences, 49(9): 968-981.
[37] Syromyatnikov K V, Levitan M A, Kuzmina T G, et al. 2017. Geochemistry of sediments of the Holocene transgressive sequences of the Kara Sea[J]. Geochemistry International, 55(6): 503-520.
[38] Thompson L G, Yao T, Davis M E, et al. 1997. Tropical climate instability: The last glacial cycle from a Qinghai-Tibetan ice core[J]. Science, 276(5320): 1821-1825.
[39] Wang G, Wang Y L, Wei Z F, et al. 2020. Geochemical records of Qionghai Lake sediments in southwestern China linked to Late Quaternary climate changes[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 560: 109902.
[40] Wang Y J, Cheng H, Edwards R L, et al. 2008. Millennial- and orbital-scale changes in the East Asian monsoon over the past 224, 000 years[J]. Nature, 451(7182): 1090-1093.
[41] Yang M X, Yao T D, Wang H J, et al. 2006. Climatic oscillations over the past 120 kyr recorded in the Guliya ice core, China[J]. Quaternary International, 154/155: 11-18.
[42] Yi L, Yu H J, Ortiz J D, et al. 2012. A reconstruction of Late Pleistocene relative sea level in the South Bohai Sea, China, based on sediment grain-size analysis[J]. Sedimentary Geology: 281: 88-100.