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A southern and northern control on speleothem-based Asian summer monsoon variability during MIS 4

Published online by Cambridge University Press:  09 July 2019

Dianbing Liu Open the ORCID record for Dianbing Liu [Opens in a new window] ,
Shushuang Liu  and
Yifan Fang
Dianbing Liu*
Affiliation:
School of Geography, Nanjing Normal University, Nanjing 210023, China
Shushuang Liu
Affiliation:
School of Geography, Nanjing Normal University, Nanjing 210023, China
Yifan Fang
Affiliation:
School of Geography, Nanjing Normal University, Nanjing 210023, China
*
*Corresponding author at: School of Geography, Nanjing Normal University, Nanjing 210023, China. E-mail address: ldb9921@njnu.edu.cn (D.B. Liu).
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Abstract

A 20-year-resolution speleothem δ18O record from southern China reveals a detailed Asian summer monsoon (ASM) history between 73.6 and 62.3 ka. ASM changes during Interstadial 19 and late MIS 4 matched Greenland temperature variations but were antiphased with Antarctic temperatures. However, long-term strengthening of the ASM in early MIS 4 agrees well with the gradual Antarctic warming, when Greenland remained in a stable cold state. More specifically, the ASM was less variable during peak interstadials in contrast to striking instabilities during stadials. These observations suggest that the factors dominating ASM variability change through time. During early MIS 4, negligible freshwater perturbations occurred in the North Atlantic, and sea-surface temperatures in the low- to midlatitude Pacific Ocean reached the modern level. Thus, an expansion of the Intertropical Convergence Zone (ITCZ) was likely important for the long-term ASM rise. In late MIS 4, the antiphase correlation between ASM and Antarctic temperature could be attributed to freshwater inputs into the North Atlantic and a southerly positioned ITCZ. Consequently, meridional ITCZ shifts, although within a limited latitudinal band, would result in an antiphase relationship between interhemispheric climate changes. Otherwise, an in-phase correlation could be expected if the centroid of ITCZ is stable along the equator.

Keywords

Speleothem recordASM variabilityMIS 4Interhemispheric climate correlationExpansion/contraction of ITCZ
Type
Research Article
Information
Quaternary Research , Volume 92 , Issue 3 , November 2019 , pp. 738 - 753
Copyright
Copyright © University of Washington. Published by Cambridge University Press, 2019 

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References

REFERENCES

Ampel, L., Bigler, C., Wohlfarth, B., Risberg, J., Lotter, A.F., Veres, D., 2010. Modest summer temperature variability during DO cycles in western Europe. Quaternary Science Reviews 29, 1322–1327.Google Scholar
An, Z.S., Wu, G.X., Li, J.P., Sun, Y.B., Liu, Y.M., Zhou, W.J., Cai, Y.J., et al. , 2015. Global monsoon dynamics and climate change. Annual Review of Earth and Planetary Sciences 43, 29–77.Google Scholar
Bar-Matthews, M., Ayalon, A., Kaufman, A., 2000. Timing and hydrological conditions of Sapropel events in the Eastern Mediterranean, as evident from speleothems, Soreq cave, Israel. Chemical Geology 169, 145–156.Google Scholar
Bjørk, A.A., Kjær, K.H., Korsgaard, N.J., Khan, S.A., Kjeldsen, K.K., Andresen, C.S., Box, J.E., Larsen, N.K., Funder, S., 2012. An aerial view of 80 years of climate-related glacier fluctuations in southeast Greenland. Nature Geoscience 5, 427–432.Google Scholar
Blunier, T., Brook, E.J., 2001. Timing of millennial-scale climate change in Antarctica and Greenland during the last glacial period. Science 291, 109–112.Google Scholar
Boers, N., Ghil, M., Rousseau, D.-D., 2018. Ocean circulation, ice shelf, and sea ice interactions explain Dansgaard-Oeschger cycles. Proceedings of the National Academy of Sciences USA 115, E11005–E11014.Google Scholar
Broccoli, A.J., Dahl, K.A., Stouffer, R.J., 2006. Response of the ITCZ to Northern Hemisphere cooling. Geophysical Research Letters 33, L01702.Google Scholar
Broecker, W.S., 1998. Paleocean circulation during the last deglaciation: a bipolar seesaw? Paleoceanography 13, 119–121.Google Scholar
Buizert, C., Schmittner, A., 2015. Southern Ocean control of glacial AMOC stability and Dansgaard-Oeschger interstadial duration. Paleoceanography 30. http://dx.doi.org/10.1002/2015PA002795.Google Scholar
Cai, Y.J., An, Z.S., Cheng, H., Edwards, R.L., Kelly, M.J., Liu, W.G., Wang, X.F., Shen, C.-C., 2006. High-resolution absolute-dated Indian Monsoon record between 53 and 36 ka from Xiaobailong Cave, southwestern China. Geology 34, 621–624.Google Scholar
Cai, Y.J., Fung, I.Y., Edwards, R.L., An, Z.S., Cheng, H., Lee, J.-E., Tan, L.C., et al. , 2015. Variability of stalagmite-inferred Indian monsoon precipitation over the past 252,000 y. Proceedings of the National Academy of Sciences USA 112, 2954–2959.Google Scholar
Chen, S. T., Wang, Y. J., Cheng, H., Edwards, R. L., Wang, X. F., Kong, X. G., Liu, D. B., 2016. Strong coupling of Asian Monsoon and Antarctic climates on sub-orbital timescales, Scientific Reports 6, 32995.Google Scholar
Cheng, H., Edwards, R.L., Wang, Y.J., Kong, X.G., Ming, Y.F., Kelly, M.J., Wang, X.F., Gallup, C.D., Liu, W.G., 2006. A penultimate glacial monsoon record from Hulu Cave and two-phase glacial terminations. Geology 34, 217–220.Google Scholar
Cheng, H., Edwards, R.L., Shen, C.-C., Polyak, V.J., Asmerom, Y., Woodhead, J., Hellstrom, J., et al. , 2013. Improvements in 230Th dating, 230Th and 234U half-life values, and U-Th isotopic measurements by multi-collector inductively coupled plasma mass spectrometry. Earth and Planetary Science Letters 371–372, 82–91.Google Scholar
Cheng, H., Sinha, A., Wang, X.F., Cruz, F.W., Edwards, R.L., 2012. The global paleomonsoon as seen through speleothem records from Asia and the Americas. Climate Dynamics 39, 1045–1062.Google Scholar
Clark, P.U., Pisias, N.G., Stocker, T.F., Weaver, A.J., 2002. The role of the thermohaline circulation in abrupt climate change. Nature 415, 863–869.Google Scholar
Collins, J.A., Schefuß, E., Heslop, D., Mulitza, S., Prange, M., Zabel, M., Tjallingii, R., et al. , 2011. Interhemispheric symmetry of the tropical African rainbelt over the past 23,000 years. Nature Geoscience 4, 42–45.Google Scholar
Cuffey, K.M., Clow, G.D., Steig, E.J., Buizert, C., Fudge, T.J., Koutnik, M., Waddington, E.D., Alley, R.B., Severinghaus, J.P., 2016. Deglacial temperature history of West Antarctica. Proceedings of the National Academy of Sciences USA 113, 14249–14254.Google Scholar
Cui, Y.F., Wang, Y.J., Cheng, H., Zhao, K., Kong, X.G., 2012. Isotopic and lithologic variations of one precisely-dated stalagmite across the Medieval/LIA period from Heilong Cave, central China. Climate of the Past 8, 1541–1550.Google Scholar
Denniston, R.F., Ummenhofer, C.C., Wanamaker, A.D. Jr., Lachniet, M.S., Villarini, G., Asmerom, Y., Polyak, V.J., et al. , 2016. Expansion and contraction of the Indo-Pacific tropical rain belt over the last three millennia. Scientific Reports 6. http://dx.doi.org/10.1038/srep34485.Google Scholar
Donohoe, A., Marshall, J., Ferreira, D., McGee, D., 2013. The relationship between ITCZ location and cross-equatorial atmospheric heat transport: from the seasonal cycle to the Last Glacial Maximum. Journal of Climate 26, 3597–3618.Google Scholar
Fairchild, I.J., Smith, C.L., Baker, A., Fuller, L., Spötl, C., Mattey, D., McDermott, F., 2006. Modification and preservation of environmental signals in speleothems. Earth-Science Reviews 75, 105–153.Google Scholar
Genty, D., Blamart, D., Ouahdi, R., Gilmour, M., Baker, A., Jouzel, J., Van-Exter, S., 2003. Precise dating of Dansgaard-Oeschger climate oscillations in western Europe from stalagmite data. Nature 421, 833–837.Google Scholar
Goñi, M.F.S., Landais, I., Cacho, I., Duprat, J., Rossignol, L., 2009. Contrasting intrainterstadial climatic evolution between high and middle North Atlantic latitudes: a close-up of Greenland Interstadials 8 and 12. Geochemistry, Geophysics, Geosystems 10. http://dx.doi.org/10.1029/2008GC002369.Google Scholar
Goñi, M.F.S., Landais, A., Fletcher, W., Naughton, F., Desprat, S., Duprat, J., 2008. Contrasting impacts of Dansgaard-Oeschger events over a western European latitudinal transect modulated by orbital parameters. Quaternary Science Reviews 27, 1136–1151.Google Scholar
Graham, N.E., Barnett, T.P., 1987. Sea surface temperature, surface wind divergence, and convection over tropical oceans. Science 238, 657–659.Google Scholar
Hastenrath, S., Heller, L., 1977. Dynamics of climatic hazards in northeast Brazil. Quaternary Journal of the Royal Meteorological Society 103, 79–92.Google Scholar
Hemming, S.R., 2004. Heinrich events: massive late Pleistocene detritus layers of the North Atlantic and their global climate imprint. Review of Geophysics 42, RG1005.Google Scholar
Hou, W., Yang, P., Feng, G.-L., 2008. The decadal variability and its cause of the extreme drought in China [in Chinese]. Acta Physica Sinica 57, 3932–3940.Google Scholar
Jacobel, A.W., MacManus, J.F., Anderson, R.F., Winckler, G., 2016. Large deglacial shifts of the Pacific Intertropical Convergence Zone. Nature Communications 7:10449.Google Scholar
Kalnay, E., Kanamitsu, M., Kistler, R., Collins, W., Deaven, D., Gandin, L., Iredell, M., et al. , 1996. The NCEP/NCAR 40-year reanalysis project. Bulletin of American Meteorological Society 77, 437–71.Google Scholar
Killick, R., Fearnhead, P., Eckley, I.A., 2012. Optimal detection of Changepoints with a linear computational cost. Journal of the American Statistical Association 107, 1590–1598.Google Scholar
Kindler, P., Guillevic, M., Baumgartner, M., Schwander, J., Landais, A., Leuenberger, M., 2014. Temperature reconstruction from 10 to 120 kyr b2k from the NGRIP ice core. Climate of the Past 10, 887–902.Google Scholar
Lachniet, M.S., 2009. Climatic and environmental controls on speleothem oxygen-isotope values. Quaternary Science Reviews 28, 412–423.Google Scholar
Lea, D.W., Pak, D.K., Belanger, C.L., Spero, H.J., Hall, M.A., Shackleton, N.J., 2006. Paleoclimate history of Galápagos surface waters over the last 135,000 yr. Quaternary Science Reviews 25, 1152–1167.Google Scholar
Lea, D.W., Pak, D.K., Spero, H.J., 2000. Climate impact of late Quaternary equatorial Pacific sea surface temperature variations. Science 289, 1719–1724.Google Scholar
Li, J.-Y., Li, T.-Y., 2018. Seasonal and annual changes in soil/cave air pCO2 and the δ13CDIC of cave drip water in response to changes in temperature and rainfall. Applied Geochemistry 93, 94–101.Google Scholar
Linsley, B.K., Rosenthal, Y., Oppo, D.W., 2010. Holocene evolution of the Indonesian throughflow and the western Pacific warm pool. Nature Geoscience 3, 578–583.Google Scholar
Liu, D.B., Wang, Y.J., Cheng, H., Edwards, R.L., Kong, X.G., Chen, S.T., Liu, S.S., 2018. Contrasting patterns in abrupt Asian summer monsoon changes in the last glacial period and the Holocene. Paleoceanography and Paleoclimatology 33, 214–226.Google Scholar
Liu, D.B., Wang, Y.J., Cheng, H., Edwards, R.L., Kong, X.G., Li, T.-Y., 2016. Strong coupling of centennial-scale changes of Asian monsoon and soil processes derived from stalagmite δ18O and δ13C records, southern China. Quaternary Research 85, 333–346.Google Scholar
Liu, D.B., Wang, Y.J., Cheng, H., Edwards, R.L., Kong, X.G., Wang, X.F., Hardt, B., et al. , 2010. Sub-millennial variability of Asian monsoon intensity during the early MIS 3 and its analogue to the ice age terminations. Quaternary Science Reviews 29, 1107–1115.Google Scholar
Liu, D.B., Wang, Y.J., Cheng, H., Edwards, R.L., Kong, X.G., Wang, X.F., Wu, J.Y., Chen, S.T., 2008. A detailed comparison of Asian monsoon intensity and Greenland temperature during the Allerød and Younger Dryas events. Earth and Planetary Science Letters 272, 691–697.Google Scholar
Lo, L., Shen, C.-C., Wei, K.-Y., Burr, G.S., Mii, H.-S., Chen, M.-T., Lee, S.-Y., Tsai, M.-C., 2014. Millennial meridional dynamics of the Indo-Pacific Warm Pool during the last termination. Climate of the Past 10, 2253–2261.Google Scholar
Maher, B.A., 2008. Holocene variability of the East Asian summer monsoon from Chinese cave records: a re-assessment. The Holocene 18, 861–866.Google Scholar
Maher, B.A., Thompson, R., 2012. Oxygen isotopes from Chinese caves: records not of monsoon rainfall but of circulation regime. Journal of Quaternary Science 27, 615–624.Google Scholar
Marcott, S.A., Clark, P.U., Padman, L., Klinkhammer, G.P., Springer, S.R., Liu, Z.Y., Otto-Bliesner, B.L., et al. , 2011. Ice-shelf collapse from subsurface warming as a trigger for Heinrich events. Proceedings of the National Academy of Sciences USA 108, 13415–13419.Google Scholar
Martrat, B., Grimalt, J.O., Lopez-Martinez, C., Cacho, I., Sierro, F.J., Flores, J.A., Zahn, R., Canals, M., Curtis, J.H., Hodell, D.A., 2004. Abrupt temperature changes in the western Mediterranean over the past 250,000 years. Science 306, 1762–1765.Google Scholar
Masson-Delmotte, V., Buiron, D., Ekaykin, A., Frezzotti, M., Gallée, H., Jouzel, J., Krinner, G., et al. , 2011. A comparison of the present and last interglacial periods in six Antarctic ice cores. Climate of the Past 7, 397–423.Google Scholar
McDermott, F., 2004. Palaeo-climate reconstruction from stable isotope variations in speleothems: a review. Quaternary Science Reviews 23, 901–918.Google Scholar
McGee, D., Donohoe, A., Marshall, J., Ferreira, D., 2014. Changes in ITCZ location and cross-equatorial heat transport at the Last Glacial Maximum, Heinrich Stadial 1, and the mid-Holocene. Earth and Planetary Science Letters 390, 69–79.Google Scholar
McGee, D., Moreno-Chamarro, E., Green, B., Marshall, J., Galbraith, E., Bradtmiller, L., 2018. Hemispherically asymmetric trade wind changes as signatures of past ITCZ shifts. Quaternary Science Reviews 180, 214–228.Google Scholar
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. Science 283, 971–975.Google Scholar
Meyer, K.W., Feng, W., Breecker, D.O., Banner, J.L., Guifoyle, A., 2014. Interpretation of speleothem calcite δ13C variations: evidence from monitoring soil CO2, drip water, and modern speleothem calcite in central Texas. Geochimica et Cosmochimica Acta 142, 281–298.Google Scholar
Mikolajewicz, U., Gröger, M., Maier-Reimer, E., Schurgers, G., Vizcáno, M., Winguth, A.M.E., 2007. Long-term effects of anthropogenic CO2 emissions simulated with a complex earth system model. Climate Dynamics 28, 599–633.Google Scholar
Oppo, D.W., Sun, Y.B., 2005. Amplitude and timing of sea-surface temperature change in the northern South China Sea: dynamic link to the East Asian monsoon. Geology 33, 785–788.Google Scholar
Pahnke, K., Sachs, J.P., 2006. Sea surface temperatures of southern midlatitudes 0–160 kyr B.P. Paleoceanography 21. http://dx.doi.org/10.1029/2005PA001191.Google Scholar
Pausata, F.S., Battisti, D.S., Nisancioglu, K.H., Bitz, C.M., 2011. Chinese stalagmite δ18O controlled by changes in the Indian monsoon during a simulated Heinrich event. Nature Geoscience 4, 474–480.Google Scholar
Plagnes, V., Causse, C., Genty, D., Paterne, M., Blamart, D., 2002. A discontinuous climate record from 187 to 74 ka from a speleothem of the Clamouse Cave (south of France). Earth and Planetary Science Letters 201, 87–103.Google Scholar
Porter, S.C., An, Z.S., 1995. Correlation between climate events in the North Atlantic and China during the last glaciation. Nature 375, 305–308.Google Scholar
Railsback, L.B., Akers, P.D., Wang, L.X., Holdridge, G.A., Voarintsoa, N.R., 2013. Layer-bounding surfaces in stalagmites as keys to better paleoclimatological histories and chronologies. International Journal of Speleology 42, 167–180.Google Scholar
Rasmussen, S.O., Bigler, M., Blockley, S.P., Blunier, T., Buchardt, S.L., Clausen, H.B., Cvijanovic, I., et al. , 2014. A stratigraphic framework for abrupt climatic changes during the Last Glacial period based on three synchronized Greenland ice-core records: refining and extending the INTIMATE event stratigraphy. Quaternary Science Reviews 106, 14–28.Google Scholar
Reimi, M.A., Marcantonio, F., 2016. Constrains on the magnitude of the deglacial migration of the ITCZ in the Central Equatorial Pacific Ocean. Earth and Planetary Science Letters 453, 1–8.Google Scholar
Rohling, E.J., Liu, Q.S., Roberts, A.P., Stanford, J.D., Rasmussen, S.O., Langen, P.L., Siddall, M., 2009. Controls on the East Asian monsoon during the last glacial cycle, based on comparison between Hulu Cave and polar ice-core records. Quaternary Science Reviews 28, 3291–3302.Google Scholar
Rosenthal, Y., Oppo, D.W., Linsley, B.K., 2003. The amplitude and phasing of climate change during the last deglaciation in the Sulu Sea, western equatorial Pacific. Geophysical Research Letters 30. http://dx.doi.org/10.1029/2002GL016612.Google Scholar
Sachs, J.P., Sachse, D., Smittenberg, R.H., Zhang, Z.H., Battisti, D.S., Golubic, S., 2009. Southward movement of the Pacific intertropical convergence zone AD 1400–1850. Nature Geoscience 2, 519–525.Google Scholar
Schmidt, M.W., Vautravers, M.J., Spero, H.J., 2006. Rapid subtropical North Atlantic salinity oscillations across Dansgaard-Oeschger cycles. Nature 443, 561–564.Google Scholar
Schneider, T., Bischoff, T., Haug, G.H., 2014. Migrations and dynamics of the intertropical convergence zone. Nature 513, 45–53.Google Scholar
Shakun, J.D., Clark, P.U., Marcott, S.A., Mix, A.C., Liu, Z.Y., Otto-Bliesner, B., Schmittner, A., Bard, E., 2012. Global warming preceded by increasing carbon dioxide concentrations during the last deglaciation. Nature 484, 49–54.Google Scholar
Shao, Q.F., Pons-Branchu, E., Zhu, Q.P., Wang, W., Valladas, H., Fontugne, M., 2017. High precision U/Th dating of the rock paintings at Mt. Huashan, Guangxi, southern China. Quaternary Research 88, 1–33.Google Scholar
Shen, Q., Wang, H.S., Shum, C.K., Jiang, L.M., Hsu, H.T., Dong, J.L., 2018. Recent high-resolution Antarctic ice velocity maps reveal increased mass loss in Wilkes Land, East Antarctica. Scientific Reports 8:4477.Google Scholar
Steffensen, J.P., Andersen, K.K., Bigler, M., Clausen, H.B., Dahl-Jensen, D., Fischer, H., Goto-Azuma, K., et al. , 2008. High-resolution Greenland ice core data show abrupt climate change happens in few years. Science 321, 680–684.Google Scholar
Stott, L., Poulsen, C., Lund, S., Thunell, R., 2002. Super ENSO and global climate oscillations at millennial time scales. Science 297, 222–226.Google Scholar
Stouffer, R.J., Yin, J., Gregory, J.M., Dixon, K.W., Spelman, M.J., Hurlin, W., Weaver, A.J., et al. , 2006. Investigating the causes of the response of the thermohaline circulation to past and future climate changes. Journal of Climate 19, 1365–1387.Google Scholar
Tachikawa, K., Vidal, L., Sonzogni, C., Bard, E., 2009. Glacial/interglacial sea surface temperature changes in the Southwest Pacific ocean over the past 360 ka. Quaternary Science Reviews 28, 1160–1170.Google Scholar
Tan, M., 2014. Circulation effect: response of precipitation δ18O to the ENSO cycle in monsoon regions of China. Climate Dynamics 42, 1067–1077.Google Scholar
Thomas, E.R., Wolff, E.W., Mulvaney, R., Johnsen, S.J., Steffensen, J.P., Arrowsmith, C., 2009. Anatomy of a Dansgaard-Oeschger warming transition: high-resolution analysis of the North Greenland Ice Core Project ice core. Journal of Geophysical Research 114, D08102.Google Scholar
Vautravers, M., Shackleton, N.J., Lopez-Martinez, C., Grimalt, J.O., 2004. Gulf Stream variability during marine isotope stage 3. Paleoceanography 19, PA2011.Google Scholar
Veres, D., Bazin, L., Landais, A., Kele, H.T.M., Lemieux-Dudon, B., Parrenin, F., Martinerie, P., et al. , 2013. The Antarctic ice core chronology (AICC2012): an optimized multi-parameter and multi-site dating approach for the last 120 thousand years. Climate of the Past 9, 1733–1748.Google Scholar
WAIS Divide Project Members, 2015. Precise interpolar phasing of abrupt climate change during the last ice age. Nature 520, 661–665.Google Scholar
Wang, P.X., Wang, B., Cheng, H., Fasullo, J., Guo, Z.T., Kiefer, T., Liu, Z.Y., 2014. The global monsoon across timescales: coherent variability of regional monsoons. Climate of the Past 10, 2007–2052.Google Scholar
Wang, P.X., Wang, B., Cheng, H., Fasullo, J., Guo, Z.T., Kiefer, T., Liu, Z.Y., 2017. The global monsoon across time scales: mechanisms and outstanding issues. Earth-Science Reviews 174, 84–121.Google Scholar
Wang, X.F., Auler, A.S., Edwards, R.L., Cheng, H., Ito, E., Solheid, M., 2006. Interhemispheric anti-phasing of rainfall during the last glacial period. Quaternary Science Reviews 25, 3391–3403.Google Scholar
Wang, Y.J., Cheng, H., Edwards, R.L., An, Z.S., Wu, J.Y., Shen, C.-C., Dorale, J.A., 2001. A high-resolution absolute-dated late Pleistocene monsoon record from Hulu Cave, China. Science 294, 2345–2348.Google Scholar
Wang, Y.J., Cheng, H., Edwards, R.L., Kong, X.G., Shao, X.H., Chen, S.T., Wu, J.Y., Jiang, X.Y., Wang, X.F., An, Z.S., 2008. Millennial- and orbital-scale changes in the East Asian monsoon over the past 224,000 years. Nature 451, 1090–1093.Google Scholar
Webster, P.J., Magaña, V.O., Palmer, T.N., Shukla, J., Tomas, R.A., Yanai, M., Yasunari, T., 1998. Monsoons: processes, predictability, and the prospects for prediction. Journal of Geophysical Research 103, 14,451–14,510.Google Scholar
Yan, H., Wei, W., Soon, W., An, Z.S., Zhou, W.J., Liu, Z.H., Wang, Y.H., Carter, R.M., 2015. Dynamics of the intertropical convergence zone over the western Pacific during the Little Ice Age. Nature Geoscience 8, 315–320.Google Scholar
Zarriess, M., Johnstone, H., Prange, M., Steph, S., Groeneveld, J., Mulitza, S., Machensen, A., 2011. Bipolar seesaw in the northeastern tropical Atlantic during Heinrich stadials. Geophysical Research Letters 38, L04706.Google Scholar
Zhang, D.E., 2005. Severe drought events as recorded in the climate records of China and their temperature situations over the last 1000 years. Acta Meteorologica Sinica 19, 485–491.Google Scholar
Zhang, H.B., Griffiths, M.L., Huang, J.H., Cai, Y.J., Wang, C.F., Zhang, F., Cheng, H., Ning, Y.F., Hu, C.Y., Xie, S.C., 2016. Antarctic link with East Asian summer monsoon variability during the Heinrich Stadial-Bølling interstadial transition. Earth and Planetary Science Letters 453, 243–251.Google Scholar
Zhang, H.W., Cheng, H., Spötl, C., Cai, Y.J., Sinha, A., Tan, L.C., Yi, L., et al. , 2018. A 200-year annually laminated stalagmite record of precipitation seasonality in southeastern China and its linkages to ENSO and PDO. Scientific Reports 8, 12344.Google Scholar
Zhang, J.W., Liu, S.S., Liu, D.B., Kong, X.G., Fang, Y.F., 2019. Correlation of speleothem δ18O and δ13C variability from Tian'e Cave, central China: insights into the phase relationship between Asian summer and winter monsoons. Journal of Asian Earth Sciences, submitted.Google Scholar
Zhang, T.-T., Li, T.-Y., Cheng, H., Edwards, R.L., Shen, C.-C., Spötl, C., Li, H.-C., Han, L.-Y., Li, J.-Y., Huang, C.-X., Zhao, X., 2017. Stalagmite-inferred centennial variability of the Asian summer monsoon in southwest China between 58 and 79 ka BP. Quaternary Science Reviews 160, 1–12.Google Scholar
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