2023 Vol. 29, No. 4
Article Contents

XU Keke, BI Zhiwei, YANG Huifeng, YANG Zhenjing, NING Kai, DAI Huimin, LIU Kai, LIU Guodong. 2023. Reconstruction of climatic and environmental evolution in the Yinchuan Basin from MIS6 to MIS5 based on spore–pollen evidence. Journal of Geomechanics, 29(4): 522-542. doi: 10.12090/j.issn.1006-6616.2023091
Citation: XU Keke, BI Zhiwei, YANG Huifeng, YANG Zhenjing, NING Kai, DAI Huimin, LIU Kai, LIU Guodong. 2023. Reconstruction of climatic and environmental evolution in the Yinchuan Basin from MIS6 to MIS5 based on spore–pollen evidence. Journal of Geomechanics, 29(4): 522-542. doi: 10.12090/j.issn.1006-6616.2023091

Reconstruction of climatic and environmental evolution in the Yinchuan Basin from MIS6 to MIS5 based on spore–pollen evidence

    Fund Project: This research is financially supported by the Natural Science Foundation of Hebei Province (Grant D2021504016) and the Geological Survey Projects of the China Geological Survey (Grants DD20221779 and DD20230210-01).
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  • MIS6 to MIS5 is a typical transition period from glacial to interglacial periods. The climate elements of MIS5 are similar to that of the current warm period, and studying its evolution process can better understand the climate change process of the current warm period and the future climate change trend. Based on modern spore–pollen and meteorological data, as well as stratigraphic spore–pollen and particle size indicators from the Yinchuan Basin in the monsoon margin area, the locally weighted average partial least squares method (LWWA-PLS) reconstruction results are considered to be the most robust after the selection of the training set, screening of the master climate parameters, cross-validation of the five reconstruction models, regional comparison, significance testing, and ecological interpretation. The climatic evolution from MIS6 to MIS5 can be divided into six stages. 157 to 131 ka, the climate was cold and humid, where wet and cold-loving arborvitae vegetation developed, with the average annual precipitation (Pann) being 424.99 mm and the average temperature in July (TJuly) 22.58 ℃. 131 to 119 ka, the climate turned wet and warm, and warm-loving trees and herbs developed; the Pann was 410.95 mm, and the TJuly was 23.62 ℃. 119 to 111 ka, the Pann was 369.50 mm, and the TJuly was 22.53 ℃; cold-loving herbs and trees developed in a cold and dry climate. 111 to 98 ka, the Pann is 378.39 mm, and the TJuly is 22.86 ℃; warm-loving trees account for a higher proportion in the early stage, and the number of cold-loving trees increased in the late stage; the climate was overall dry and warm, and the temperature increased first and then decreased. 98 to 85 ka, the Pann was 278.24, and the TJuly was 22.01 ℃; the overall climate was the driest and coldest, and cold-loving trees developed well. 85 to 78 ka, the Pann was 364.21 mm, and TJuly was 23.45 ℃; the climate turned warm and humid, and trees and herbs developed in this period. The reconstructed climate parameters' ensemble empirical mode decomposition (EEMD) results respond well to the 23 ka precessional cycle. Comparison with the mid- and high-latitude geologic record of the Northern Hemisphere suggests that solar radiation-influenced climatic variability in the North Atlantic primarily drives changes in the East Asian monsoon through the westerly wind circulation as well as the oceanic transport zone, which in turn influences climatic change in the Yinchuan Basin.

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  • [1] BAUCH H A, KANDIANO E S, 2007. Evidence for early warming and cooling in North Atlantic surface waters during the last interglacial[J]. Paleoceanography, 22(1): PA1201.

    Google Scholar

    [2] BAUCH H A, ERLENKEUSER H, 2008. A “critical” climatic evaluation of last interglacial (MIS 5e) records from the Norwegian Sea[J]. Polar Research, 27(2): 135-151. doi: 10.1111/j.1751-8369.2008.00059.x

    CrossRef Google Scholar

    [3] BAUCH H A, KANDIANO E S, HELMKE J, et al. , 2011. Climatic bisection of the last interglacial warm period in the Polar North Atlantic[J]. Quaternary Science Reviews, 30(15-16): 1813-1818. doi: 10.1016/j.quascirev.2011.05.012

    CrossRef Google Scholar

    [4] BERGER A, LOUTRE M F, 1991. Insolation values for the climate of the last 10 million years[J]. Quaternary Science Reviews, 10(4): 297-317. doi: 10.1016/0277-3791(91)90033-Q

    CrossRef Google Scholar

    [5] BIRKS H J B, GORDON A D, 1985. Numerical methods in quaternary pollen analysis[M]. London: Academic Press.

    Google Scholar

    [6] BIRKS H J B, TER BRAAK C J F, LINE J M, et al. , 1990. Diatoms and pH reconstruction[J]. Philosophical Transactions of the Royal Society B: Biological Sciences, 327(1240): 263-278.

    Google Scholar

    [7] BIRKS H J B, LOTTER A F, JUGGINS S, et al. , 2012. Tracking environmental change using lake sediments volume 5: data handling and numerical techniques[M]. Dordrecht: Springer: 123-141. DOI: 10.1007/978-94-007-2745-8.

    Google Scholar

    [8] BLAAUW M, CHRISTEN J A, 2011. Flexible paleoclimate age-depth models using an autoregressive gamma process[J]. Bayesian Analysis, 6(3): 457-474. doi: 10.1214/ba/1339616472

    CrossRef Google Scholar

    [9] CAI M T, WEI M J, XU D N, et al. , 2013. Vegetation and climate changes during three interglacial periods represented in the Luochuan loess-paleosol section, on the Chinese Loess Plateau[J]. Quaternary International, 296: 131-140. doi: 10.1016/j.quaint.2012.06.041

    CrossRef Google Scholar

    [10] CAO X Y, HERZSCHUH U, TELFORD R J, et al. , 2014. A modern pollen–climate dataset from China and Mongolia: Assessing its potential for climate reconstruction[J]. Review of Palaeobotany and Palynology, 211: 87-96. doi: 10.1016/j.revpalbo.2014.08.007

    CrossRef Google Scholar

    [11] CAO X Y, TIAN F, TELFORD R J, et al. , 2017. Impacts of the spatial extent of pollen-climate calibration-set on the absolute values, range and trends of reconstructed Holocene precipitation[J]. Quaternary Science Reviews, 178: 37-53. doi: 10.1016/j.quascirev.2017.10.030

    CrossRef Google Scholar

    [12] CHEN H Y, XU D Y, LIAO M N, et al. , 2021. A modern pollen dataset of China[J]. Chinese Journal of Plant Ecology, 45(7): 799-808. (in Chinese with English abstract) doi: 10.17521/cjpe.2021.0024

    CrossRef Google Scholar

    [13] CHEN J H, LV F Y, HUANG X Z, et al. , 2018. A novel procedure for pollen-based quantitative paleoclimate reconstructions and its application in China. Science China Earth Sciences, 60(11): 2059-2066,doi: 10.1007/s11430-017-9095-1

    Google Scholar

    [14] CHENG H, EDWARDS R L, SINHA A, et al. , 2016. The Asian monsoon over the past 640, 000 years and Ice Age terminations[J]. Nature, 534(7609): 640-646. doi: 10.1038/nature18591

    CrossRef Google Scholar

    [15] CHI C T, TIAN Y Y, ZHOU Z, et al. , 2021. Palaeoclimate and palaeoenvironmental evolution during the late Pliocene (3.04-2.88 Ma) based on pollen records from the Yinchuan Basin, Northwest China[J]. Quaternary International, 598: 15-23. doi: 10.1016/j.quaint.2021.04.036

    CrossRef Google Scholar

    [16] DING Z L, LIU D S, LIU D S, et al. , 1989. The 37 climatic cycles in the past 250×104 years [J]. Chinese Science Bulletin, 34(19): 1494-1496. (in Chinese) doi: 10.1360/csb1989-34-19-1494

    CrossRef Google Scholar

    [17] DU S H, LI B S, NIU D F, et al. , 2011. Age of the MGS5 segment of the Milanggouwan stratigraphical section and evolution of the desert environment on a kiloyear scale during the Last Interglacial in China's Salawusu River Valley: Evidence from Rb and Sr contents and ratios[J]. Geochemistry, 71(1): 87-95. doi: 10.1016/j.chemer.2010.07.002

    CrossRef Google Scholar

    [18] DUAN W H, CHENG H, TAN M, et al. , 2016. Onset and duration of transitions into Greenland Interstadials 15.2 and 14 in northern China constrained by an annually laminated stalagmite[J]. Scientific Reports, 6(1): 20844,doi: 10.1038/srep20844.

    CrossRef Google Scholar

    [19] FAN S X, ZHENG H R, LIU P G, et al. , 2002. Late quaternary sporopollen records ad rapid climatic fluctuation events in the Yinchuan Basin[J]. Geology in China, 29(4): 431-434. (in Chinese with English abstract)

    Google Scholar

    [20] GE Y G, WEI M J, 2014. Comparison of climate and environment change of the Last Interglacial Period and Holocene in Beijing Area, China[J]. International Journal of Geosciences, 5(8): 852-862. doi: 10.4236/ijg.2014.58075

    CrossRef Google Scholar

    [21] GRIMM E C, 1987. CONISS: A FORTRAN 77 program for stratigraphically constrained cluster analysis by the method of incremental sum of squares[J]. Computers & Geosciences, 13(1): 13-35.

    Google Scholar

    [22] GUAN D H, XI X X, HAO Y P, et al. , 1996. Climate instability revealed in the Beiyuan CaCO3 record during the Last Interglacial Age[J]. Journal of Glaciology and Geocryology, 18(2): 119-124. (in Chinese with English abstract)

    Google Scholar

    [23] HERZSCHUH U, BIRKS H J B, MISCHKE S, et al. , 2010. A modern pollen-climate calibration set based on lake sediments from the Tibetan Plateau and its application to a Late Quaternary pollen record from the Qilian Mountains[J]. Journal of Biogeography, 37(4): 752-766. doi: 10.1111/j.1365-2699.2009.02245.x

    CrossRef Google Scholar

    [24] HEUSSER L, MORLEY J, 1997. Monsoon fluctuations over the past 350 kyr: High-resolution evidence from northeast asia/northwest Pacific climate proxies (marine pollen and radiolarians)[J]. Quaternary Science Reviews, 16(6): 565-581. doi: 10.1016/S0277-3791(96)00079-0

    CrossRef Google Scholar

    [25] HEUSSER L E, 1990. Northeast Asian pollen records for the last 150, 000 years from deep-sea cores V28-304 and RC14-99 taken off the Pacific coast of Japan[J]. Review of Palaeobotany and Palynology, 65(1-4): 1-8. doi: 10.1016/0034-6667(90)90050-S

    CrossRef Google Scholar

    [26] HUANG K Y, WEI J H, CHEN B S, 2013. Research progress of pollen-based quantitative paleoclimate reconstruction using modern analogue technique[J]. Quaternary Sciences, 33(6): 1069-1079. (in Chinese with English abstract)

    Google Scholar

    [27] HUANG X Z, XIANG L X, ZHANG E Y, et al. , 2019. Mid-holocene cold event at ca. 7 ka and its impact on vegetation ecology in Northern China[J]. Quaternary Sciences, 39(3): 687-700. (in Chinese with English abstract)

    Google Scholar

    [28] JANSEN F, OKSANEN J, 2013. How to model species responses along ecological gradients: Huisman-Olff-Fresco models revisited[J]. Journal of Vegetation Science, 24(6): 1108-1117. doi: 10.1111/jvs.12050

    CrossRef Google Scholar

    [29] JIANG X Y, KONG X G, WANG Y J, et al. , 2011. A high-resolution stalagmite δ13C record from Sanbao cave over the penultimate glaciation[J]. Quaternary Sciences, 31(1): 1-7. (in Chinese with English abstract)

    Google Scholar

    [30] JIANG X Y, WANG X Y, HE Y Q, et al. , 2016. Precisely dated multidecadally resolved Asian summer monsoon dynamics 113.5-86.6 thousand years ago[J]. Quaternary Science Reviews, 143: 1-12. doi: 10.1016/j.quascirev.2016.05.003

    CrossRef Google Scholar

    [31] JOUZEL J, LORIUS C, PETIT J R, et al. , 1987. Vostok ice core: a continuous isotope temperature record over the last climatic cycle (160, 000 years)[J]. Nature, 329(6138): 403-408. doi: 10.1038/329403a0

    CrossRef Google Scholar

    [32] JUGGINS S, 2001. The European diatom database[EB/OL]. [2001-10]https://www.researchgate.net/publication/228722952_The_European_diatom_database

    Google Scholar

    [33] JUGGINS S, BIRKS H J B, 2012. Quantitative environmental reconstructions from biological data[M]//BIRKS H J B, LOTTER A F, JUGGINS S, et al. Tracking environmental change using lake sediments: data handling and numerical techniques. Dordrecht: Springer: 431-494,doi: 10.1007/978-94-007-2745-8_14.

    Google Scholar

    [34] JUGGINS S, 2013. Quantitative reconstructions in palaeolimnology: new paradigm or sick science?[J]. Quaternary Science Reviews, 64: 20-32. doi: 10.1016/j.quascirev.2012.12.014

    CrossRef Google Scholar

    [35] JUGGINS S, 2022. Rioja: analysis of quaternary science data[EB/OL]. [2022-10-31].https://cran.r-project.org/package=rioja.

    Google Scholar

    [36] KELLY M J, EDWARDS R L, CHENG H, et al. , 2006. High resolution characterization of the Asian Monsoon between 146, 000 and 99, 000 years B. P. from Dongge Cave, China and global correlation of events surrounding Termination II[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 236(1-2): 20-38. doi: 10.1016/j.palaeo.2005.11.042

    CrossRef Google Scholar

    [37] KUKLA G J, 1977. Pleistocene land-sea correlations I. Europe[J]. Earth-Science Reviews, 13(4): 307-374. doi: 10.1016/0012-8252(77)90125-8

    CrossRef Google Scholar

    [38] LAI J S, ZOU Y, ZHANG J L, et al. , 2022. Generalizing hierarchical and variation partitioning in multiple regression and canonical analyses using the rdacca. hp R package[J]. Methods in Ecology and Evolution, 13(4): 782-788. doi: 10.1111/2041-210X.13800

    CrossRef Google Scholar

    [39] LEGENDRE P, GALLAGHER E D, 2001. Ecologically meaningful transformations for ordination of species data[J]. Oecologia, 129(2): 271-280. doi: 10.1007/s004420100716

    CrossRef Google Scholar

    [40] LI X L, HAO Q Z, WEI M J, et al. , 2017. Phased uplift of the northeastern Tibetan Plateau inferred from a pollen record from Yinchuan Basin, Northwestern China[J]. Scientific Reports, 7(1): 18023,doi: 10.1038/s41598-017-16915-z.

    CrossRef Google Scholar

    [41] LI Y C, XU Q H, LIU J S, et al. , 2007. A transfer-function model developed from an extensive surface-pollen data set in northern China and its potential for palaeoclimate reconstructions[J]. The Holocene, 17(7): 897-905. doi: 10.1177/0959683607082404

    CrossRef Google Scholar

    [42] LIANG C, ZHAO Y, QIN F, et al. , 2020. Pollen-based Holocene quantitative temperature reconstruction on the eastern Tibetan Plateau using a comprehensive method framework[J]. Science China: Earth Sciences, 63(8): 1144-1160. doi: 10.1007/s11430-019-9599-y

    CrossRef Google Scholar

    [43] LISIECKI L E, RAYMO M E, 2005. A pliocene-pleistocene stack of 57 globally distributed benthic δ18O records[J]. Paleoceanography, 20(1): PA1003,doi: 10.1029/2004PA001071.

    CrossRef Google Scholar

    [44] LIU P G, FAN S X, LI X J, 2000. The geochemical element characteristics and paleosedimentary environment of the quaternary deposits in Yinchuan Basin[J]. Journal of Geomechanics, 6(4): 43-50, 94. (in Chinese with English abstract)

    Google Scholar

    [45] LU H, JIA J, XIA D S, et al. , 2015. East asian summer monsoon evolution during MIS 6.5 record in Chinese Loess Plateau and its implications[J]. Quaternary Sciences, 35(6): 1402-1411. (in Chinese with English abstract)

    Google Scholar

    [46] LU H Y, WU N Q, LIU K B, et al. , 2011. Modern pollen distributions in Qinghai-Tibetan Plateau and the development of transfer functions for reconstructing Holocene environmental changes[J]. Quaternary Science Reviews, 30(7-8): 947-966. doi: 10.1016/j.quascirev.2011.01.008

    CrossRef Google Scholar

    [47] MANGERUD J, SØNSTEGAARD E, SEJRUP H P, 1978. Correlation of the Eemian (interglacial) stage and the deep-sea oxygen-isotope stratigraphy[J]. Nature, 277(5693): 189-192.

    Google Scholar

    [48] MCMANUS J F, OPPO D W, CULLEN J L, 1999. A 0.5-million-year record of millennial-scale climate variability in the North Atlantic[J]. Science, 283(5404): 971-975. doi: 10.1126/science.283.5404.971

    CrossRef Google Scholar

    [49] MING Y F, 2004. Preliminary study of MIS6 East Asian summer monsoon suborbital scale climate change[D] Nanjing: Nanjing Normal University. (in Chinese)

    Google Scholar

    [50] MUHS D R, SIMMONS K R, STEINKE B, 2002. Timing and warmth of the Last Interglacial period: new U-series evidence from Hawaii and Bermuda and a new fossil compilation for North America[J]. Quaternary Science Reviews, 21(12-13): 1355-1383. doi: 10.1016/S0277-3791(01)00114-7

    CrossRef Google Scholar

    [51] OKSANEN J, BLANCHET F G, FRIENDLY M, et al. , 2020. Vegan community ecology package version 2.5-7 November 2020[EB/OL]. [2020-11-28].https://cran.r-project.org/package=vegan

    Google Scholar

    [52] OVERPECK J T, WEBB T, PRENTICE I C, 1985. Quantitative interpretation of fossil pollen spectra: Dissimilarity coefficients and the method of modern analogs[J]. Quaternary Research, 23(1): 87-108. doi: 10.1016/0033-5894(85)90074-2

    CrossRef Google Scholar

    [53] PEI Q M, MA Y Z, HU C L, et al. , 2016. Climatic character of Marine Isotope Stage (MIS) 5e in the representative regions of the world: A review[J]. Advances in Earth Science, 31(11): 1182-1196. (in Chinese with English abstract)

    Google Scholar

    [54] PETIT J R, JOUZEL J, RAYNAUD D, et al. , 1999. Climate and atmospheric history of the past 420, ;000 years from the Vostok ice core, Antarctica[J]. Nature, 399(6735): 429-436. doi: 10.1038/20859

    CrossRef Google Scholar

    [55] QIN F, ZHAO Y, 2013. Methods of quantitative climate reconstruction based on palynological data and their applications in China[J]. Quaternary Sciences, 33(6): 1054-1068. (in Chinese with English abstract)

    Google Scholar

    [56] QIN F, 2021. Modern pollen assemblages of the surface lake sediments from the steppe and desert zones of the Tibetan Plateau[J]. Science China Earth Sciences, 64(3): 425-439. doi: 10.1007/s11430-020-9693-y

    CrossRef Google Scholar

    [57] REGATTIERI E, ISOLA I, ZANCHETTA G, et al. , 2012. Stratigraphy, petrography and chronology of speleothem deposition at Tana che Urla (Lucca, Italy): Paleoclimatic implications[J]. Geografia Fisica e Dinamica Quaternaria, 35(2): 141-152.

    Google Scholar

    [58] SIMPSON G L, OKSANEN J, 2021. Analogue: analogue matching and modern analogue technique transfer function models(R package version 0. 17-6)[EB/OL]. [2021-06-20].https://cran.r-project.org/package=analogue.

    Google Scholar

    [59] SUN J M, DING Z L, 1998. Deposits and soils of the past 130, 000 years at the desert–loess transition in Northern China[J]. Quaternary Research, 50(2): 148-156. doi: 10.1006/qres.1998.1989

    CrossRef Google Scholar

    [60] SUN X J, DU N Q, WONG C Y, et al. , 1994. Paleovegetation and paleoenvironment of Manasi Lake, Xinjiang, N. W. China during the last 14000 years[J]. Quaternary Sciences, 14(3): 239-248. (in Chinese with English abstract)

    Google Scholar

    [61] SUN X J, LUO Y L, 2001. Pollen record of the last 280 ka from deep sea sediments of the northern South China Sea[J]. Science in China Series D: Earth Sciences, 44(10): 879-888. doi: 10.1007/BF02907079

    CrossRef Google Scholar

    [62] TANG Z H, DU S S, LIU F L, 2017. Late Pleistocene changes in vegetation and the associated human activity at Beiyao Site, Central China[J]. Review of Palaeobotany and Palynology, 244: 107-112. doi: 10.1016/j.revpalbo.2017.04.002

    CrossRef Google Scholar

    [63] TER BRAAK C J F, BARENDREGT L G, 1986. Weighted averaging of species indicator values: Its efficiency in environmental calibration[J]. Mathematical Biosciences, 78(1): 57-72. doi: 10.1016/0025-5564(86)90031-3

    CrossRef Google Scholar

    [64] TER BRAAK C J F, LOOMAN C W N, 1986. Weighted averaging, logistic regression and the Gaussian response model[J]. Vegetatio, 65(1): 3-11. doi: 10.1007/BF00032121

    CrossRef Google Scholar

    [65] TER BRAAK C J F, JUGGINS S, 1993. Weighted averaging partial least squares regression (WA-PLS): an improved method for reconstructing environmental variables from species assemblages[J]. Hydrobiologia, 269(1): 485-502.

    Google Scholar

    [66] TIAN Y Y, ZHOU Z, CHI C T, et al. , 2020. The paleoclimate change period of the Late Pliocene-Early Pleistocene recorded by pollen from core PL02 in Yinchuan Basin[J]. Quaternary Sciences, 40(6): 1418-1430. (in Chinese with English abstract)

    Google Scholar

    [67] TONG G B, SHI Y, FAN S X, et al. , 1995a. Environment features of Yinchuan Basin in Late Quaternary period[J]. Earth Science, 4(4): 421-426. (in Chinese with English abstract)

    Google Scholar

    [68] TONG G B, ZHENG H R, YANG Z J, et al. , 1995b. Multicyclic model of palynoflora climate since 4 Ma in China[J]. Marine Geology & Quaternary Geology, 15(4): 81-96. (in Chinese with English abstract)

    Google Scholar

    [69] VERES D, BAZIN L, LANDAIS A, et al. , 2013. The Antarctic ice core chronology (AICC2012): an optimized multi-parameter and multi-site dating approach for the last 120 thousand years[J]. Climate of the Past, 9(4): 1733-1748. doi: 10.5194/cp-9-1733-2013

    CrossRef Google Scholar

    [70] WANG F X, QIAN N F, ZHANG Y L, et al. , 1995. Pollen flora of China[M]. 2nd ed. Beijing: Science Press. (in Chinese)

    Google Scholar

    [71] WANG H C, 2022. Variation of Asian summer monsoon intensity in late MIS6 derived from grayscale and Mg/Ca, Sr/Ca, Ba/Ca records of a stalagmite in Wanxiang Cave, eastern Qinghai-Tibet Plateau[D]. Lanzhou: Lanzhou University. (in Chinese with English abstract)

    Google Scholar

    [72] 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. doi: 10.1038/nature06692

    CrossRef Google Scholar

    [73] WANG Y J, LIU D B, 2016. Speleothem records of Asian paleomonsoon variability and mechanisms[J]. Chinese Science Bulletin, 61(9): 938-951. (in Chinese with English abstract) doi: 10.1360/N972015-01022

    CrossRef Google Scholar

    [74] WANG Z B, WANG J Y, HE L L, et al. , 2021. Characteristics and evolution process of the ridge-groove sequence of the Jiulongtan glacial accumulation in Mengshan, Shandong: with the discussion on the difference of accumulation sequence of glacier and debris flow[J]. Journal of Geomechanics, 27(1): 105-116,doi: 10.12090/j.issn.1006-6616.2021.27.01.011. (in Chinese with English abstract)

    CrossRef Google Scholar

    [75] WEI L J, 2021. Cenozoic paleontological characteristics and paleoenvironment of King George Island, West Antarctica[J]. Journal of Geomechanics, 27(5): 855-866,doi: 10.12090/j.issn.1006-6616.2021.27.05.069. (in Chinese with English abstract)

    CrossRef Google Scholar

    [76] WEI L J, LI Z H, LI M T, et al. , 2023. Palynological records and paleoclimatic significance during the middle and late Late Pleistocene in the Qingshuihe Basin, Ningxia[J]. Journal of Geomechanics,doi: 10.12090/j.issn.1006-6616.2023015. (in Chinese with English abstract)

    Google Scholar

    [77] WEN R L, XIAO J L, MA Y Z, et al. , 2013. Pollen–climate transfer functions intended for temperate eastern Asia[J]. Quaternary International, 311: 3-11. doi: 10.1016/j.quaint.2013.04.025

    CrossRef Google Scholar

    [78] XU K K, YANG Z J, NING K, et al. , 2021. MIS6—MIS5 climate change of Yinchuan Basin based on end-member method[J]. Geoscience, 35(5): 1311-1322. (in Chinese with English abstract)

    Google Scholar

    [79] XU Q H, LI Y C, BUNTING M J, et al. , 2010. The effects of training set selection on the relationship between pollen assemblages and climate parameters: Implications for reconstructing past climate[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 289(1-4): 123-133. doi: 10.1016/j.palaeo.2010.02.024

    CrossRef Google Scholar

    [80] XUE C F, HOU W, ZHAO J H, et al. , 2013. The application of ensemble empirical mode decomposition method in multiscale analysis of region precipitation and its response to the climate change[J]. Acta Physica Sinica, 62(10): 109203. (in Chinese with English abstract) doi: 10.7498/aps.62.109203

    CrossRef Google Scholar

    [81] YANG X D, WANG S M, TONG G B, et al. , 1998. The Late Pleistocene pollen record in the lake sediments from ancient Heqing Lake and its significance for palaeoclimate[J]. Quaternary Sciences, 18(4): 335-343. (in Chinese with English abstract)

    Google Scholar

    [82] YANG Z J, LIU Z M, ZHANG J P, et al. , 2001a. Sporopollen records and paleocl imate study of Yinchuan Basin since mid-Pleistocene[J]. Marine Geology & Quaternary Geology, 21(3): 43-49. (in Chinese with English abstract)

    Google Scholar

    [83] YANG Z J, ZHENG H R, TONG G B, et al. , 2001b. Study on palynoflora and paleoclimatic cycles since Mid-Pleistocene in Yinchuan Basin[J]. Journal of Changchun University of Science and Technology, 31(3): 213-216. (in Chinese with English abstract)

    Google Scholar

    [84] YAO T D, 1999. Abrupt climatic changes on the Tibetan Plateau during the Last Ice Age: comparative study of the Guliya ice core with the Greenland GRIP ice core[J]. Science China Earth Sciences, 42(4): 358-368.

    Google Scholar

    [85] ZHANG Q, HAN Y X, SONG L C, 2005. The summarize of development of global climate change and its effect factors[J]. Advances in Earth Science, 20(9): 990-998. (in Chinese with English abstract)

    Google Scholar

    [86] ZHANG X F, LI J J, ZHANG X B, et al. , 2021. Evolution of the climate and sedimentary environment since the Middle Pleistocene on the Northwestern Coast of the Bohai Bay[J]. Acta Geologica Sinica, 95(6): 1868-1888. (in Chinese with English abstract)

    Google Scholar

    [87] ZHAO H, HUANG W, XIE T T, et al. , 2019. Optimization and evaluation of a monthly air temperature and precipitation gridded dataset with a 0.025° spatial resolution in China during 1951-2011[J]. Theoretical and Applied Climatology, 138(1-2): 491-507. doi: 10.1007/s00704-019-02830-y

    CrossRef Google Scholar

    [88] ZHAO Y, TZEDAKIS P C, LI Q, et al. , 2020. Evolution of vegetation and climate variability on the Tibetan Plateau over the past 1.74 million years[J]. Science Advances, 6(19): eaay6193,doi: 10.1126/sciadv.aay6193.

    CrossRef Google Scholar

    [89] ZHAO Y, LIANG C, CUI Q Y, et al. , 2021. Temperature reconstructions for the last 1.74-Ma on the eastern Tibetan Plateau based on a novel pollen-based quantitative method[J]. Global and Planetary Change, 199: 103433,doi: 10.1016/j.gloplacha.2021.103433.

    CrossRef Google Scholar

    [90] 陈海燕, 徐德宇, 廖梦娜, 等, 2021. 中国现代花粉数据集[J]. 植物生态学报, 45(7): 799-808.

    Google Scholar

    [91] 陈建徽, 吕飞亚, 黄小忠, 等, 2018. 基于孢粉的古气候参数定量重建: 一种新思路及其在中国的应用实例[J]. 中国科学: 地球科学, 48(1): 42-50.

    Google Scholar

    [92] 丁仲礼, 刘东生, 刘秀铭, 等, 1989. 250万年以来的37个气候旋迴[J]. 科学通报, 34(19): 1494-1496.

    Google Scholar

    [93] 范淑贤, 郑宏瑞, 刘平贵, 等, 2002. 银川盆地晚第四纪孢粉记录的快速气候波动事件[J]. 中国地质, 29(4): 431-434.

    Google Scholar

    [94] 管东红, 奚晓霞, 郝永萍, 等, 1996. 北塬剖面碳酸钙记录的末次间冰期气候不稳定性[J]. 冰川冻土, 18(2): 119-124.

    Google Scholar

    [95] 黄康有, 魏金辉, 陈碧珊, 2013. 最佳类比法的孢粉-古气候定量重建研究进展[J]. 第四纪研究, 33(6): 1069-1079.

    Google Scholar

    [96] 黄小忠, 向丽雄, 张恩源, 等, 2019. 全新世中期7ka前后降温事件对中国北方植被生态的影响[J]. 第四纪研究, 39(3): 687-700.

    Google Scholar

    [97] 姜修洋, 孔兴功, 汪永进, 等, 2011. 神农架三宝洞倒数第二次冰期高分辨率石笋δ13C记录[J]. 第四纪研究, 31(1): 1-7.

    Google Scholar

    [98] 梁琛, 赵艳, 秦锋, 等, 2020. 孢粉—气候定量重建方法体系的建立及其应用: 以青藏高原东部全新世温度重建为例[J]. 中国科学: 地球科学, 50(7): 977-994.

    Google Scholar

    [99] 刘平贵, 范淑贤, 李雪菊, 2000. 银川盆地第四纪地球化学元素特征及沉积环境[J]. 地质力学学报, 6(4): 43-50, 94.

    Google Scholar

    [100] 陆浩, 贾佳, 夏敦胜, 等, 2015. 黄土高原记录的MIS 6.5期东亚夏季风信号及其古气候意义[J]. 第四纪研究, 35(6): 1402-1411. doi: 10.11928/j.issn.1001-7410.2015.06.09

    CrossRef Google Scholar

    [101] 明艳芳, 2004. 初探MIS6东亚夏季风亚轨道尺度气候变化[D]. 南京: 南京师范大学.

    Google Scholar

    [102] 裴巧敏, 马玉贞, 胡彩莉, 等, 2016. 全球典型地区MIS5e阶段气候特征研究进展[J]. 地球科学进展, 31(11): 1182-1196. doi: 10.11867/j.issn.1001-8166.2016.11.1182

    CrossRef Google Scholar

    [103] 秦锋, 赵艳, 2013. 基于孢粉组合定量重建古气候的方法在中国的运用及思考[J]. 第四纪研究, 33(6): 1054-1068. doi: 10.3969/j.issn.1001-7410.2013.06.02

    CrossRef Google Scholar

    [104] 秦锋, 2021. 青藏高原草原带和荒漠带湖泊表层沉积物现代花粉研究[J]. 中国科学: 地球科学, 51(3): 437-452.

    Google Scholar

    [105] 孙湘君, 杜乃秋, 翁成郁, 等, 1994. 新疆玛纳斯湖盆周围近14000年以来的古植被古环境[J]. 第四纪研究, 14(3): 239-248. doi: 10.3321/j.issn:1001-7410.1994.03.005

    CrossRef Google Scholar

    [106] 田晏嫣, 周助, 迟长婷, 等, 2020. 银川盆地PL02钻孔孢粉记录的晚上新世-早更新世时期的古气候变化周期[J]. 第四纪研究, 40(6): 1418-1430. doi: 10.11928/j.issn.1001-7410.2020.06.04

    CrossRef Google Scholar

    [107] 童国榜, 石英, 范淑贤, 等, 1995a. 银川盆地晚第四纪环境特征[J]. 地球科学, 4(4): 421-426.

    Google Scholar

    [108] 童国榜, 郑宏瑞, 杨振京, 等, 1995b. 中国4 Ma来孢粉植物群气候的多重旋回模型[J]. 海洋地质与第四纪地质, 15(4): 81-96.

    Google Scholar

    [109] 王伏雄, 钱南芬, 张玉龙等, 1995. 中国植物花粉形态[M]. 2版. 北京: 科学出版社.

    Google Scholar

    [110] 王海川, 2022. 青藏高原东部万象洞石笋灰度与Mg/Ca、Sr/Ca、Ba/Ca记录推演的MIS6晚期亚洲夏季风变化[D]. 兰州: 兰州大学.

    Google Scholar

    [111] 汪永进, 刘殿兵, 2016. 亚洲古季风变率和机制的洞穴石笋档案[J]. 科学通报, 61(9): 938-951.

    Google Scholar

    [112] 王照波, 王江月, 何乐龙, 等, 2021. 山东蒙山九龙潭冰川堆积“垄槽序列”的特征及演化过程研究: 兼论冰川、泥石流堆积序列的差异性[J]. 地质力学学报, 27(1): 105-116,doi: 10.12090/j.issn.1006-6616.2021.27.01.011.

    CrossRef Google Scholar

    [113] 韦利杰, 2021. 西南极乔治王岛新生代古生物特征及古环境探讨[J]. 地质力学学报, 27(5): 855-866,doi: 10.12090/j.issn.1006-6616.2021.27.05.069.

    CrossRef Google Scholar

    [114] 韦利杰, 李振宏, 李明涛, 等, 2023. 宁夏清水河盆地晚更新世中晚期孢粉记录及古气候意义[J]. 地质力学学报, doi: 10.12090/j.issn.1006-6616.2023015.

    Google Scholar

    [115] 许可可, 杨振京, 宁凯, 等, 2021. 基于端元法的银川盆地MIS6—MIS5气候变化探究[J]. 现代地质, 35(5): 1311-1322.

    Google Scholar

    [116] 薛春芳, 侯威, 赵俊虎, 等, 2013. 集合经验模态分解在区域降水变化多尺度分析及气候变化响应研究中的应用[J]. 物理学报, 62(10): 109203. doi: 10.7498/aps.62.109203

    CrossRef Google Scholar

    [117] 羊向东, 王苏民, 童国榜, 等, 1998. 云南鹤庆古湖晚更新世的孢粉记录及其古气候学意义[J]. 第四纪研究, 18(4): 335-343. doi: 10.3321/j.issn:1001-7410.1998.04.006

    CrossRef Google Scholar

    [118] 杨振京, 刘志明, 张俊牌, 等, 2001a. 银川盆地中更新世以来的孢粉记录及古气候研究[J]. 海洋地质与第四纪地质, 21(3): 43-49.

    Google Scholar

    [119] 杨振京, 郑宏瑞, 童国榜, 等, 2001b. 银川盆地中更新世以来的孢粉植物群古气候旋回探讨[J]. 长春科技大学学报, 31(3): 213-216.

    Google Scholar

    [120] 姚檀栋, 1999. 末次冰期青藏高原的气候突变: 古里雅冰芯与格陵兰GRIP冰芯对比研究[J]. 中国科学(D辑), 29(2): 175-180.

    Google Scholar

    [121] 张强, 韩永翔, 宋连春, 2005. 全球气候变化及其影响因素研究进展综述[J]. 地球科学进展, 20(9): 990-998.

    Google Scholar

    [122] 张晓飞, 李继军, 张学斌, 等, 2021. 渤海湾西北岸中更新世中期以来的气候环境和沉积环境演变[J]. 地质学报, 95(6): 1868-1888. doi: 10.3969/j.issn.0001-5717.2021.06.014

    CrossRef Google Scholar

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