Articles | Volume 16, issue 3
https://doi.org/10.5194/cp-16-833-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-16-833-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Archaeal lipid-inferred paleohydrology and paleotemperature of Lake Chenghai during the Pleistocene–Holocene transition
Weiwei Sun
State Key Laboratory of Lake Science and Environment, Nanjing
Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing
210008, China
Enlou Zhang
CORRESPONDING AUTHOR
State Key Laboratory of Lake Science and Environment, Nanjing
Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing
210008, China
Center for Excellence in Quaternary Science and Global Change,
Chinese Academy of Science, Xian 710061, China
Jie Chang
State Key Laboratory of Lake Science and Environment, Nanjing
Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing
210008, China
James Shulmeister
School of Earth and Environmental Sciences, The University of
Queensland, St Lucia, Brisbane, Queensland, 4072, Australia
School of Earth and Environment, University of Canterbury, Private
Bag 4800, Christchurch, New Zealand
Michael I. Bird
ARC Centre of Excellence for Australian Biodiversity and Heritage,
James Cook University, P.O. Box 6811, Cairns, Queensland, 4870, Australia
College of Science and Engineering, James Cook University, P.O. Box
6811, Cairns, Queensland, 4870, Australia
Cheng Zhao
State Key Laboratory of Lake Science and Environment, Nanjing
Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing
210008, China
Center for Excellence in Quaternary Science and Global Change,
Chinese Academy of Science, Xian 710061, China
Qingfeng Jiang
School of Geography Sciences, Nantong University, Nantong, 226007,
China
Ji Shen
State Key Laboratory of Lake Science and Environment, Nanjing
Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing
210008, China
Related authors
Mengna Liao, Kai Li, Weiwei Sun, and Jian Ni
Clim. Past, 17, 2291–2303, https://doi.org/10.5194/cp-17-2291-2021, https://doi.org/10.5194/cp-17-2291-2021, 2021
Short summary
Short summary
The long-term trajectories of precipitation, hydrological balance and soil moisture are not completely consistent in southwest China. Hydrological balance was more sensitive to temperature change on a millennial scale. For soil moisture, plant processes also played a big role in addition to precipitation and temperature. Under future climate warming, surface water shortage in southwest China can be even more serious and efforts at reforestation may bring some relief to the soil moisture deficit.
Mengna Liao, Kai Li, Weiwei Sun, and Jian Ni
Clim. Past, 17, 2291–2303, https://doi.org/10.5194/cp-17-2291-2021, https://doi.org/10.5194/cp-17-2291-2021, 2021
Short summary
Short summary
The long-term trajectories of precipitation, hydrological balance and soil moisture are not completely consistent in southwest China. Hydrological balance was more sensitive to temperature change on a millennial scale. For soil moisture, plant processes also played a big role in addition to precipitation and temperature. Under future climate warming, surface water shortage in southwest China can be even more serious and efforts at reforestation may bring some relief to the soil moisture deficit.
Zhitong Yu, Xiujun Wang, Guangxuan Han, Xingqi Liu, and Enlou Zhang
Biogeosciences Discuss., https://doi.org/10.5194/bg-2017-353, https://doi.org/10.5194/bg-2017-353, 2017
Manuscript not accepted for further review
Xiayun Xiao, Simon G. Haberle, Ji Shen, Bin Xue, Mark Burrows, and Sumin Wang
Clim. Past, 13, 613–627, https://doi.org/10.5194/cp-13-613-2017, https://doi.org/10.5194/cp-13-613-2017, 2017
Short summary
Short summary
Knowledge of the past fire activity is a key for making sustainable management policies for forest ecosystems. A high-resolution macroscopic charcoal record from southwestern China reveals the postglacial fire history. Combined with the regional climate records and vegetation histories, it is concluded that fire was mainly controlled by climate before 4.3 ka and by combined action of climate and humans after 4.3 ka, and the relationship between fire activity and vegetation were also examined.
Enlou Zhang, Jie Chang, Yanmin Cao, Hongqu Tang, Pete Langdon, James Shulmeister, Rong Wang, Xiangdong Yang, and Ji Shen
Clim. Past, 13, 185–199, https://doi.org/10.5194/cp-13-185-2017, https://doi.org/10.5194/cp-13-185-2017, 2017
Short summary
Short summary
This paper reports the first development of sub-fossil chironomid-based mean July temperature transfer functions from China. The transfer functions yield reliable reconstructions that are comparable to the instrumental record. The application of this new tool will provide long-term quantitative palaeoclimate estimates from south-western China which is a critical region for understanding the dynamic and evolution of the Indian Ocean south-west Monsoon system.
James Shulmeister, Justine Kemp, Kathryn E. Fitzsimmons, and Allen Gontz
Clim. Past, 12, 1435–1444, https://doi.org/10.5194/cp-12-1435-2016, https://doi.org/10.5194/cp-12-1435-2016, 2016
Short summary
Short summary
This paper highlights that small dunes (lunettes) formed on the eastern side of a lake in the Australian sub-tropics at the height of the last ice age (about 21,000 years ago) and in the early part of the current interglacial (9–6,000 years ago). This means that it was fairly wet at these times and also that there were strong westerly winds to form the dunes. Today strong westerly winds occur in winter, and we infer that the same was also true at those times, suggesting no change in circulation.
Enlou Zhang, Yongbo Wang, Weiwei Sun, and Ji Shen
Clim. Past, 12, 415–427, https://doi.org/10.5194/cp-12-415-2016, https://doi.org/10.5194/cp-12-415-2016, 2016
Z. T. Yu, X. J. Wang, E. L. Zhang, C. Y. Zhao, and X. Q. Liu
Biogeosciences, 12, 6605–6615, https://doi.org/10.5194/bg-12-6605-2015, https://doi.org/10.5194/bg-12-6605-2015, 2015
Short summary
Short summary
Bosten Lake is the largest inland freshwater lake in China, which has been impacted by land use changes, with implications for carbon burial. Our study showed a large spatial variability in total organic carbon (TOC) (1.8–4.4%); 54–90% of TOC was from autochthonous sources. Higher TOC content was found in the east and central-north sections and near the mouth of the Kaidu River, which was attributable to allochthonous, autochthonous plus allochthonous, and autochthonous sources, respectively.
G. Saiz, M. Bird, C. Wurster, C. A. Quesada, P. Ascough, T. Domingues, F. Schrodt, M. Schwarz, T. R. Feldpausch, E. Veenendaal, G. Djagbletey, G. Jacobsen, F. Hien, H. Compaore, A. Diallo, and J. Lloyd
Biogeosciences, 12, 5041–5059, https://doi.org/10.5194/bg-12-5041-2015, https://doi.org/10.5194/bg-12-5041-2015, 2015
Short summary
Short summary
We demonstrate and explain differential patterns in SOM dynamics in C3/C4 mixed ecosystems at various spatial scales across contrasting climate and soils. This study shows that the interdependence between biotic and abiotic factors ultimately determines whether SOM dynamics of C3- and C4-derived vegetation are at variance in ecosystems where both vegetation types coexist. The results also highlight the far-reaching implications that vegetation thickening may have for the stability of deep SOM.
E. M. Veenendaal, M. Torello-Raventos, T. R. Feldpausch, T. F. Domingues, F. Gerard, F. Schrodt, G. Saiz, C. A. Quesada, G. Djagbletey, A. Ford, J. Kemp, B. S. Marimon, B. H. Marimon-Junior, E. Lenza, J. A. Ratter, L. Maracahipes, D. Sasaki, B. Sonké, L. Zapfack, D. Villarroel, M. Schwarz, F. Yoko Ishida, M. Gilpin, G. B. Nardoto, K. Affum-Baffoe, L. Arroyo, K. Bloomfield, G. Ceca, H. Compaore, K. Davies, A. Diallo, N. M. Fyllas, J. Gignoux, F. Hien, M. Johnson, E. Mougin, P. Hiernaux, T. Killeen, D. Metcalfe, H. S. Miranda, M. Steininger, K. Sykora, M. I. Bird, J. Grace, S. Lewis, O. L. Phillips, and J. Lloyd
Biogeosciences, 12, 2927–2951, https://doi.org/10.5194/bg-12-2927-2015, https://doi.org/10.5194/bg-12-2927-2015, 2015
Short summary
Short summary
When nearby forest and savanna stands are compared, they are not as structurally different as first seems. Moreover, savanna-forest transition zones typically occur at higher rainfall for South America than for Africa but with coexistence confined to a well-defined edaphic-climate envelope. With interacting soil cation-soil water storage–precipitations effects on canopy cover also observed we argue that both soils and climate influence the location of the two major tropical vegetation types.
G. Saiz, J. G. Wynn, C. M. Wurster, I. Goodrick, P. N. Nelson, and M. I. Bird
Biogeosciences, 12, 1849–1863, https://doi.org/10.5194/bg-12-1849-2015, https://doi.org/10.5194/bg-12-1849-2015, 2015
Short summary
Short summary
Around half of all pyrogenic carbon (charcoal+soot) derived from wildfires comes from semi-annual burning of tropical savannas. This pyrogenic carbon is significant because it is a component of global aerosols capable of modulating the greenhouse effect and is resistant to degradation. We use controlled field burns in northern Australian savannas to determine how much pyrogenic carbon is formed, how much of this is recalcitrant and how it is partitioned between ground residues and airborne soot.
K. J. Bloomfield, T. F. Domingues, G. Saiz, M. I. Bird, D. M. Crayn, A. Ford, D. J. Metcalfe, G. D. Farquhar, and J. Lloyd
Biogeosciences, 11, 7331–7347, https://doi.org/10.5194/bg-11-7331-2014, https://doi.org/10.5194/bg-11-7331-2014, 2014
Related subject area
Subject: Proxy Use-Development-Validation | Archive: Terrestrial Archives | Timescale: Millenial/D-O
Hydrological change in southern Australia over 1750 years: a bivalve oxygen isotope record from the Coorong Lagoon
Millennial hydrological variability in the continental northern Neotropics during Marine Isotope Stages (MISs) 3–2 (59–15 cal ka BP) inferred from sediments of Lake Petén Itzá, Guatemala
Greenhouse gases modulate the strength of millennial-scale subtropical rainfall, consistent with future predictions
Humidity changes and possible forcing mechanisms over the last millennium in arid Central Asia
Differing pre-industrial cooling trends between tree rings and lower-resolution temperature proxies
Dansgaard–Oeschger-like events of the penultimate climate cycle: the loess point of view
Evaluating model outputs using integrated global speleothem records of climate change since the last glacial
1200 years of warm-season temperature variability in central Scandinavia inferred from tree-ring density
Hydroclimatic variability in the Levant during the early last glacial (∼ 117–75 ka) derived from micro-facies analyses of deep Dead Sea sediments
Detailed insight into Arctic climatic variability during MIS 11c at Lake El'gygytgyn, NE Russia
Statistical framework for evaluation of climate model simulations by use of climate proxy data from the last millennium – Part 1: Theory
Impact of postglacial warming on borehole reconstructions of last millennium temperatures
Estimating 750 years of temperature variations and uncertainties in the Pyrenees by tree-ring reconstructions and climate simulations
Briony Kate Chamberlayne, Jonathan James Tyler, Deborah Haynes, Yuexiao Shao, John Tibby, and Bronwyn May Gillanders
Clim. Past, 19, 1383–1396, https://doi.org/10.5194/cp-19-1383-2023, https://doi.org/10.5194/cp-19-1383-2023, 2023
Short summary
Short summary
We used geochemical signals in shells preserved in sediments to create a 1750-year record of hydrological change in the Coorong Lagoon of South Australia. The record is interpreted to reflect the balance of evaporation and precipitation and shows that it has always been a highly evaporated system. The record also shows similarities to other environmental reconstructions from the region. This knowledge can increase our understanding of the potential impacts of environmental change.
Rodrigo Martínez-Abarca, Michelle Abstein, Frederik Schenk, David Hodell, Philipp Hoelzmann, Mark Brenner, Steffen Kutterolf, Sergio Cohuo, Laura Macario-González, Mona Stockhecke, Jason Curtis, Flavio S. Anselmetti, Daniel Ariztegui, Thomas Guilderson, Alexander Correa-Metrio, Thorsten Bauersachs, Liseth Pérez, and Antje Schwalb
Clim. Past, 19, 1409–1434, https://doi.org/10.5194/cp-19-1409-2023, https://doi.org/10.5194/cp-19-1409-2023, 2023
Short summary
Short summary
Lake Petén Itzá, northern Guatemala, is one of the oldest lakes in the northern Neotropics. In this study, we analyzed geochemical and mineralogical data to decipher the hydrological response of the lake to climate and environmental changes between 59 and 15 cal ka BP. We also compare the response of Petén Itzá with other regional records to discern the possible climate forcings that influenced them. Short-term climate oscillations such as Greenland interstadials and stadials are also detected.
Fei Guo, Steven Clemens, Yuming Liu, Ting Wang, Huimin Fan, Xingxing Liu, and Youbin Sun
Clim. Past, 18, 1675–1684, https://doi.org/10.5194/cp-18-1675-2022, https://doi.org/10.5194/cp-18-1675-2022, 2022
Short summary
Short summary
Our high-resolution loess Ca/Ti record displays millennial monsoon oscillations that persist over the last 650 kyr. Wavelet results indicate the ice volume and GHG co-modulation at the 100 kyr band and GHG and local insolation forcing at the precession band for the magnitude of millennial monsoon variability of loess Ca/Ti. The inferred mechanism calls on dynamic linkages to variability in AMOC. At the precession band, combined effects of GHG and insolation lead to increased extreme rainfall.
Shengnan Feng, Xingqi Liu, Feng Shi, Xin Mao, Yun Li, and Jiaping Wang
Clim. Past, 18, 975–988, https://doi.org/10.5194/cp-18-975-2022, https://doi.org/10.5194/cp-18-975-2022, 2022
Short summary
Short summary
We present a continuous humidity history in arid Central Asia over the past millennium based on the ~1.8-year high-resolution multiproxy record from Lake Dalongchi. Our findings emphasize that the Gleissberg solar cycle and quasi-regular period of ENSO amplitude play critical roles in controlling the effective humidity at century and multidecadal timescales, respectively. Our analysis provides new insights for hydroclimate predictions and climate simulations in arid Central Asia in the future.
Lara Klippel, Scott St. George, Ulf Büntgen, Paul J. Krusic, and Jan Esper
Clim. Past, 16, 729–742, https://doi.org/10.5194/cp-16-729-2020, https://doi.org/10.5194/cp-16-729-2020, 2020
Short summary
Short summary
The PAGES2k multiproxy database offers a new and unique opportunity to study the lack of long-term cooling trends in tree-ring data, which can be expected in Northern Hemisphere summers, particularly in the high latitudes, due to orbitally driven changes in solar irradiance. Tests of different influencing factors reveal that preserving millennial-scale cooling trends related to orbital forcing is not feasible in most tree-ring datasets.
Denis-Didier Rousseau, Pierre Antoine, Niklas Boers, France Lagroix, Michael Ghil, Johanna Lomax, Markus Fuchs, Maxime Debret, Christine Hatté, Olivier Moine, Caroline Gauthier, Diana Jordanova, and Neli Jordanova
Clim. Past, 16, 713–727, https://doi.org/10.5194/cp-16-713-2020, https://doi.org/10.5194/cp-16-713-2020, 2020
Short summary
Short summary
New investigations of European loess records from MIS 6 reveal the occurrence of paleosols and horizon showing slight pedogenesis similar to those from the last climatic cycle. These units are correlated with interstadials described in various marine, continental, and ice Northern Hemisphere records. Therefore, these MIS 6 interstadials can confidently be interpreted as DO-like events of the penultimate climate cycle.
Laia Comas-Bru, Sandy P. Harrison, Martin Werner, Kira Rehfeld, Nick Scroxton, Cristina Veiga-Pires, and SISAL working group members
Clim. Past, 15, 1557–1579, https://doi.org/10.5194/cp-15-1557-2019, https://doi.org/10.5194/cp-15-1557-2019, 2019
Short summary
Short summary
We use an updated version of the Speleothem Isotopes Synthesis and Analysis (SISAL) database and palaeoclimate simulations generated using the ECHAM5-wiso isotope-enabled climate model to provide a protocol for using speleothem isotopic data for model evaluation, including screening the observations and the optimum period for the modern observational baseline. We also illustrate techniques through which the absolute isotopic values during any time period could be used for model evaluation.
Peng Zhang, Hans W. Linderholm, Björn E. Gunnarson, Jesper Björklund, and Deliang Chen
Clim. Past, 12, 1297–1312, https://doi.org/10.5194/cp-12-1297-2016, https://doi.org/10.5194/cp-12-1297-2016, 2016
Short summary
Short summary
We present C-Scan, a new Scots pine tree-ring density based reconstruction of warm-season (April-September) temperatures for central Scandinavia back to 850 CE, extending the previous reconstruction by 250 years. Our reconstruction indicates that the warm-season warmth during a relatively-warm period of last millennium is not so pronounced in central Scandinavia, which adds further detail to our knowledge about the spatial pattern of surface air temperature on the regional scale.
I. Neugebauer, M. J. Schwab, N. D. Waldmann, R. Tjallingii, U. Frank, E. Hadzhiivanova, R. Naumann, N. Taha, A. Agnon, Y. Enzel, and A. Brauer
Clim. Past, 12, 75–90, https://doi.org/10.5194/cp-12-75-2016, https://doi.org/10.5194/cp-12-75-2016, 2016
Short summary
Short summary
Micro-facies changes and elemental variations in deep Dead Sea sediments are used to reconstruct relative lake level changes for the early last glacial period. The results indicate a close link of hydroclimatic variability in the Levant to North Atlantic-Mediterranean climates during the time of the build-up of Northern Hemisphere ice shields. First petrographic analyses of gravels in the deep core question the recent hypothesis of a Dead Sea dry-down at the end of the last interglacial.
H. Vogel, C. Meyer-Jacob, M. Melles, J. Brigham-Grette, A. A. Andreev, V. Wennrich, P. E. Tarasov, and P. Rosén
Clim. Past, 9, 1467–1479, https://doi.org/10.5194/cp-9-1467-2013, https://doi.org/10.5194/cp-9-1467-2013, 2013
R. Sundberg, A. Moberg, and A. Hind
Clim. Past, 8, 1339–1353, https://doi.org/10.5194/cp-8-1339-2012, https://doi.org/10.5194/cp-8-1339-2012, 2012
V. Rath, J. F. González Rouco, and H. Goosse
Clim. Past, 8, 1059–1066, https://doi.org/10.5194/cp-8-1059-2012, https://doi.org/10.5194/cp-8-1059-2012, 2012
I. Dorado Liñán, U. Büntgen, F. González-Rouco, E. Zorita, J. P. Montávez, J. J. Gómez-Navarro, M. Brunet, I. Heinrich, G. Helle, and E. Gutiérrez
Clim. Past, 8, 919–933, https://doi.org/10.5194/cp-8-919-2012, https://doi.org/10.5194/cp-8-919-2012, 2012
Cited articles
Alley, R. B. and Clark, P. U.: The deglaciation of the northern hemisphere: A
global perspective, Annu. Rev. Earth Planet. Sc., 27, 14–182, https://doi.org/10.1146/annurev.earth.27.1.149, 1999.
Baker, J. L., Lachniet, M. S., Chervyatsova, O., Asmerom, Y., and Polyak, V. J.:
Holocene warming in western continental Eurasia driven by glacial retreat
and greenhouse forcing, Nat. Geosci., 10, 430–435, https://doi.org/10.1038/ngeo2953,
2017.
Berger, A. and Loutre, M.-F.: Insolation values for the climate of the last 10
million years, Quaternary Sci. Rev., 10, 297–317, https://doi.org/10.1016/0277-3791(91)90033-Q, 1991.
Berke, M. A., Johnson, T. C., Werne, J. P., Schouten, S., and Sinninghe Damsté,
J. S.: A mid-Holocene thermal maximum at the end of the African Humid Period,
Earth. Planet. Sc. Lett., 351–352, 95–104, https://doi.org/10.1016/j.epsl.2012.07.008,
2012.
Blaauw, M. and Andres Christen, J.: Flexible paleoclimate age-depth models
using an autoregressive gamma process, Bayesian. Anal., 6, 457–474,
https://doi.org/10.1214/11-BA618, 2011.
Blaga, C. I., Reichart, G.-J., Heiri, O., and Sinninghe Damsté, J. S.:
Tetraether membrane lipid distributions in water-column particulate matter
and sediments: a study of 47 European lakes along a north–south transect,
J. Paleolimnol., 41, 523–540, https://doi.org/10.1007/s10933-008-9242-2, 2009.
Blaga, C. I., Reichart, G. J., Schouten, S., Lotter, A. F., Werne, J. P.,
Kosten, S., Mazzeo, N., Lacerot, G., and Damste, J. S. S.: Branched glycerol
dialkyl glycerol tetraethers in lake sediments: Can they be used as
temperature and pH proxies?, Org. Geochem., 41, 1225–1234, https://doi.org/10.1016/j.orggeochem.2010.07.002, 2010.
Blaga, C. I., Reichart, G.-J., Vissers, E. W., Lotter, A. F., Anselmetti, F. S.,
and Sinninghe Damsté, J. S.: Seasonal changes in glycerol dialkyl glycerol
tetraether concentrations and fluxes in a perialpine lake: Implications for
the use of the TEX86 and BIT proxies, Geochim. Cosmochim. Ac., 75, 6416–6428,
https://doi.org/10.1016/j.gca.2011.08.016, 2011.
Blaga, C. I., Reichart, G.-J., Lotter, A. F., Anselmetti, F. S., and Sinninghe
Damsté, J. S.: A TEX86 lake record suggests simultaneous shifts in
temperature in Central Europe and Greenland during the last deglaciation,
Geophys. Res. Lett., 40, 948–953, https://doi.org/10.1002/grl.50181, 2013.
Buckles, L. K., Villanueva, L., Weijers, J. W. H., Verschuren, D., and Damsté,
J. S. S.: Linking isoprenoidal GDGT membrane lipid distributions with gene
abundances of ammonia-oxidizing Thaumarchaeota and uncultured crenarchaeotal
groups in the water column of a tropical lake (Lake Challa, East Africa),
Environ. Microbiol., 15, 2445–2462, https://doi.org/10.1111/1462-2920.12118, 2013.
Carlson, A. E., LeGrande, A. N., Oppo, D. W., Came, R. E., Schmidt, G. A.,
Anslow, F. S., Licciardi, J. M., and Obbink, E. A.: Rapid early Holocene
deglaciation of the Laurentide ice sheet, Nat. Geosci., 1, 620–624, https://doi.org/10.1038/ngeo285, 2008.
Castañeda, I. S. and Schouten, S.: A review of molecular organic proxies for
examining modern and ancient lacustrine environments, Quaternary Sci. Rev.,
30, 2851–2891, https://doi.org/10.1016/j.quascirev.2011.07.009, 2011.
Castañeda, I. S. and Schouten, S.: Corrigendum to “A review of molecular
organic proxies for examining modern and ancient lacustrine environments”
[Quat. Sci. Rev. 30 (2011) 2851–2891], Quaternary Sci. Rev., 125, 174–176,
https://doi.org/10.1016/j.quascirev.2015.07.020, 2015.
Cheng, H., Sinha, A., Wang, X., Cruz, F. W., and Edwards, R. L.: The Global
Paleomonsoon as seen through speleothem records from Asia and the Americas,
Clim. Dynam., 39, 1045–1062, https://doi.org/10.1007/s00382-012-1363-7, 2012.
Contreras-Rosales, L. A., Jennerjahn, T., Tharammal, T., Meyer, V.,
Lückge, A., Paul, A., and Schefuß, E.: Evolution of the Indian Summer
Monsoon and terrestrial vegetation in the Bengal region during the past
18 ka, Quaternary Sci. Rev., 102, 133–148, https://doi.org/10.1016/j.quascirev.2014.08.010, 2014.
Dang, X., Ding, W., Yang, H., Pancost, R. D., Naafs, B. D. A., Xue, J., Lin,
X., Lu, J., and Xie, S.: Different temperature dependence of the bacterial
brGDGT isomers in 35 Chinese lake sediments compared to that in soils, Org.
Geochem., 72–79, https://doi.org/10.1016/j.orggeochem.2018.02.008, 2018.
Dang, X. Y., Xue, J. T., Yang, H., and Xie, S. C.: Environmental impacts on the
distribution of microbial tetraether lipids in Chinese lakes with
contrasting pH: Implications for lacustrine paleoenvironmental
reconstructions, Sci. China. Earth. Sci., 59, 939–950, https://doi.org/10.1007/s11430-015-5234-z, 2016.
Dutt, S., Gupta, A. K., Clemens, S. C., Cheng, H., Singh, R. K., Kathayat, G., and
Edwards, R. L.: Abrupt changes in Indian summer monsoon strength during
33,800 to 5500 years B.P., Geophys. Res. Lett., 42, 5526–5532, https://doi.org/10.1002/2015GL064015, 2015.
Dykoski, C. A., Edwards, R. L., Cheng, H., Yuan, D., Cai, Y., Zhang, M., Lin,
Y., Qing, J., An, Z., and Revenaugh, J.: A high-resolution, absolute-dated
Holocene and deglacial Asian monsoon record from Dongge Cave, China, Earth.
Planet. Sc. Lett., 233, 71–86, https://doi.org/10.1016/j.epsl.2005.01.036, 2005.
Feng, X., Zhao, C., D'Andrea, W. J., Liang, J., Zhou, A., and Shen, J.:
Temperature fluctuations during the Common Era in subtropical southwestern
China inferred from brGDGTs in a remote alpine lake, Earth. Planet. Sc.
Lett., 510, 26–36, https://doi.org/10.1016/j.epsl.2018.12.028, 2019.
Filippi, M. L. and Talbot, M. R.: The palaeolimnology of northern Lake Malawi
over the last 25 ka based upon the elemental and stable isotopic composition
of sedimentary organic matter, Quaternary Sci. Rev., 24, 1303–1328, https://doi.org/10.1016/j.quascirev.2004.10.009, 2005.
Gebregiorgis, D., Hathorne, E. C., Sijinkumar, A. V., Nath, B. N.,
Nürnberg, D., and Frank, M.: South Asian summer monsoon variability during
the last ∼54 kyrs inferred from surface water salinity and river
runoff proxies, Quaternary Sci. Rev., 138, 6–15, https://doi.org/10.1016/j.quascirev.2016.02.012, 2016.
Govil, P. and Divakar Naidu, P.: Variations of Indian monsoon precipitation
during the last 32 kyr reflected in the surface hydrography of the Western
Bay of Bengal, Quaternary Sci. Rev., 30, 3871–3879, https://doi.org/10.1016/j.quascirev.2011.10.004, 2011.
Günther, F., Thiele, A., Gleixner, G., Xu, B., Yao, T., and Schouten, S.:
Distribution of bacterial and archaeal ether lipids in soils and surface
sediments of Tibetan lakes: Implications for GDGT-based proxies in saline
high mountain lakes, Org. Geochem., 67, 19–30, https://doi.org/10.1016/j.orggeochem.2013.11.014, 2014.
Günther, F., Witt, R., Schouten, S., Mäusbacher, R., Daut, G., Zhu,
L., Xu, B., Yao, T., and Gleixner, G.: Quaternary ecological responses and
impacts of the Indian Ocean Summer Monsoon at Nam Co, Southern Tibetan
Plateau, Quaternary Sci. Rev., 112, 66–77, https://doi.org/10.1016/j.quascirev.2015.01.023,
2015.
Hu, J., Zhou, H., Peng, P. A., and Spiro, B.: Seasonal variability in
concentrations and fluxes of glycerol dialkyl glycerol tetraethers in
Huguangyan Maar Lake, SE China: Implications for the applicability of the
MBT-CBT paleotemperature proxy in lacustrine settings, Chem. Geol., 420,
200–212, https://doi.org/10.1016/j.chemgeo.2015.11.008, 2016.
Kathayat, G., Cheng, H., Sinha, A., Spötl, C., Edwards, R. L., Zhang, H.,
Li, X., Yi, L., Ning, Y., Cai, Y., Lui, W. L., and Breitenbach, S. F. M.: Indian
monsoon variability on millennial-orbital timescales, Sci. Rep-UK., 6, 24374, https://doi.org/10.1038/srep24374, 2016.
Kim, J.-G., Jung, M.-Y., Park, S.-J., Rijpstra, W. I. C., Sinninghe
Damsté, J. S., Madsen, E. L., Min, D., Kim, J.-S., Kim, G.-J., and Rhee,
S.-K.: Cultivation of a highly enriched ammonia-oxidizing archaeon of
thaumarchaeotal group I.1b from an agricultural soil, Environ. Microbiol.,
14, 1528–1543, https://doi.org/10.1111/j.1462-2920.2012.02740.x, 2012.
Kim, J.-H., van der Meer, J., Schouten, S., Helmke, P., Willmott, V.,
Sangiorgi, F., Koç, N., Hopmans, E. C., and Damsté, J. S. S.: New indices
and calibrations derived from the distribution of crenarchaeal isoprenoid
tetraether lipids: Implications for past sea surface temperature
reconstructions, Geochim. Cosmochim. Ac., 74, 4639–4654, https://doi.org/10.1016/j.gca.2010.05.027, 2010.
Li, J., Pancost, R. D., Naafs, B. D. A., Yang, H., Liu, D., Gong, L., Qiu, X.,
and Xie, S.: Multiple environmental and ecological controls on archaeal ether
lipid distributions in saline ponds, Chem. Geol., 529, 119293, https://doi.org/10.1016/j.chemgeo.2019.119293, 2019.
Li, J. J., Pancost, R. D., Naafs, B. D. A., Yang, H., Zhao, C., and Xie, S. C.:
Distribution of glycerol dialkyl glycerol tetraether (GDGT) lipids in a
hypersaline lake system, Org. Geochem., 99, 113–124, https://doi.org/10.1016/j.orggeochem.2016.06.007, 2016.
Li, K., Zhou, Y., Zhou, Q., Dong, Y., Zhang, Y., Chang, J., Chen, L., and Lu,
Y.: Temporal-spatial distribution of euphotic depth and its influencing
factors in Lake Chenghai, Yunnan Province, China, J. Lake Sci., 31,
256–267, https://doi.org/10.18307/2019.0124, 2019.
Li, Y., Chen, X., Xiao, X., Zhang, H., Xue, B., Shen, J., and Zhang, E.:
Diatom-based inference of Asian monsoon precipitation from a volcanic lake
in southwest China for the last 18.5 ka, Quaternary Sci. Rev., 182, 109–120,
https://doi.org/10.1016/j.quascirev.2017.11.021, 2018.
Ling, Y., Sun, Q., Zheng, M., Wang, H., Luo, Y., Dai, X., Xie, M., and Zhu, Q.:
Alkenone-based temperature and climate reconstruction during the last
deglaciation at Lake Dangxiong Co, southwestern Tibetan Plateau, Quaternary
Int., 443, 58–69, https://doi.org/10.1016/j.quaint.2016.07.036, 2017.
Ljungqvist, F. C., Krusic, P. J., Sundqvist, H. S., Zorita, E., Brattström,
G., and Frank, D.: Northern Hemisphere hydroclimate variability over the past
twelve centuries, Nature, 532, 94–98, https://doi.org/10.1038/nature17418, 2016.
Lu, Z.: Study on climatic and environmental changes of the Yunnan Chenghai
region recorded bylake sediments since 1800 [D], master Thesis,
Yunnan Normal University, Kunming, 39–43, 2018.
MARGO Project Members: Constraints on the magnitude and patterns of ocean
cooling at the Last Glacial Maximum, Nat. Geosci. 2, 127–132, https://doi.org/10.1038/ngeo411, 2009.
Marsicek, J., Shuman, B. N., Bartlein, P. J., Shafer, S. L., and Brewer, S.:
Reconciling divergent trends and millennial variations in Holocene
temperatures, Nature, 554, 92–96, https://doi.org/10.1038/nature25464, 2018.
Meegan Kumar, D., Woltering, M., Hopmans, E. C., Sinninghe Damsté, J. S.,
Schouten, S., and Werne, J. P.: The vertical distribution of Thaumarchaeota in
the water column of Lake Malawi inferred from core and intact polar
tetraether lipids, Org. Geochem., 132, 37–49, https://doi.org/10.1016/j.orggeochem.2019.03.004, 2019.
Ni, Z., Jones, R., Zhang, E., Chang, J., Shulmeister, J., Sun, W., Wang, Y.,
and Ning, D.: Contrasting effects of winter and summer climate on Holocene
montane vegetation belts evolution in southeastern Qinghai-Tibetan Plateau,
China, Palaeogeogr. Palaeocl., 533, 109232, https://doi.org/10.1016/j.palaeo.2019.06.005, 2019.
Ning, D., Zhang, E., Shulmeister, J., Chang, J., Sun, W., and Ni, Z.: Holocene
mean annual air temperature (MAAT) reconstruction based on branched glycerol
dialkyl glycerol tetraethers from Lake Ximenglongtan, southwestern China,
Org. Geochem., 133, 65–76, https://doi.org/10.1016/j.orggeochem.2019.05.003, 2019.
Pearson, E. J., Juggins, S., Talbot, H. M., Weckstrom, J., Rosen, P., Ryves,
D. B., Roberts, S. J., and Schmidt, R.: A lacustrine GDGT-temperature calibration
from the Scandinavian Arctic to Antarctic: Renewed potential for the
application of GDGT-paleothermometry in lakes, Geochim. Cosmochim. Ac., 75,
6225–6238, https://doi.org/10.1016/j.gca.2011.07.042, 2011.
Pitcher, A., Hopmans, E. C., Mosier, A. C., Park, S.-J., Rhee, S.-K., Francis,
C. A., Schouten, S., and Sinninghe Damsté, J. S.: Core and Intact Polar
Glycerol Dibiphytanyl Glycerol Tetraether Lipids of Ammonia-Oxidizing
Archaea Enriched from Marine and Estuarine Sediments, Appl. Environ. Microb.,
77, 3468, https://doi.org/10.1128/AEM.02758-10, 2011.
Powers, L., Werne, J. P., Vanderwoude, A. J., Sinninghe Damsté, J. S.,
Hopmans, E. C., and Schouten, S.: Applicability and calibration of the TEX86
paleothermometer in lakes, Org. Geochem., 41, 404–413, https://doi.org/10.1016/j.orggeochem.2009.11.009, 2010.
Powers, L. A., Werne, J. P., Johnson, T. C., Hopmans, E. C., Damsté, J. S. S., and
Schouten, S.: Crenarchaeotal membrane lipids in lake sediments: A new
paleotemperature proxy for continental paleoclimate reconstruction?, Geology,
32, 613–616, https://doi.org/10.1130/G20434.1, 2004.
Rashid, H., Flower, B. P., Poore, R. Z., and Quinn, T. M.: A ∼25 ka
Indian Ocean monsoon variability record from the Andaman Sea, Quaternary
Sci. Rev., 26, 2586–2597, https://doi.org/10.1016/j.quascirev.2007.07.002, 2007.
R Development Core Team: A language and environment for statistical
computing, R Foundation for Statistical Computing, Vienna, Austria, 2013.
Reimer, P. J., Bard, E., Bayliss, A., Beck, J. W., Blackwell, P. G., Ramsey,
C. B., Buck, C. E., Cheng, H., Edwards, R. L., and Friedrich, M.: IntCal13 and
Marine13 radiocarbon age calibration curves 0–50 000 years cal BP,
Radiocarbon, 55, 1869–1887, https://doi.org/10.2458/azu_js_rc.55.16947, 2013.
Russell, J. M., Hopmans, E. C., Loomis, S. E., Liang, J., and Sinninghe Damsté,
J. S.: Distributions of 5- and 6-methyl branched glycerol dialkyl glycerol
tetraethers (brGDGTs) in East African lake sediment: Effects of temperature,
pH, and new lacustrine paleotemperature calibrations, Org. Geochem., 117,
56–69, https://doi.org/10.1016/j.orggeochem.2017.12.003, 2018.
Saraswat, R., Lea, D. W., Nigam, R., Mackensen, A., and Naik, D. K.: Deglaciation
in the tropical Indian Ocean driven by interplay between the regional
monsoon and global teleconnections, Earth. Planet. Sc. Lett., 375, 166–175,
https://doi.org/10.1016/j.epsl.2013.05.022, 2013.
Schouten, S., Hopmans, E. C., Schefuß, E., and Sinninghe Damsté, J. S.:
Distributional variations in marine crenarchaeotal membrane lipids: a new
tool for reconstructing ancient sea water temperatures?, Earth. Planet. Sc.
Lett., 204, 265–274, https://doi.org/10.1016/S0012-821X(02)00979-2, 2002.
Schouten, S., Rijpstra, W. I. C., Durisch-Kaiser, E., Schubert, C. J.,
and Sinninghe Damsté, J. S.: Distribution of glycerol dialkyl glycerol
tetraether lipids in the water column of Lake Tanganyika, Org. Geochem., 53,
34–37, https://doi.org/10.1016/j.orggeochem.2012.01.009, 2012.
Schouten, S., Hopmans, E. C., and Sinninghe Damsté, J. S.: The organic
geochemistry of glycerol dialkyl glycerol tetraether lipids: A review, Org.
Geochem., 54, 19–61, https://doi.org/10.1016/j.orggeochem.2012.09.006, 2013.
Shen, C., Liu, K.-B., Tang, L., and Overpeck, J. T.: Quantitative relationships
between modern pollen rain and climate in the Tibetan Plateau, Rev.
Palaeobot. Palyno., 140, 61–77, https://doi.org/10.1016/j.revpalbo.2006.03.001, 2006.
Shuman, B., Bartlein, P. J., and Webb, T.: The magnitudes of millennial- and
orbital-scale climatic change in eastern North America during the Late
Quaternary, Quaternary Sci. Rev., 24, 2194–2206, https://doi.org/10.1016/j.quascirev.2005.03.018, 2005.
Sinha, A., Stott, L., Berkelhammer, M., Cheng, H., Edwards, R. L., Buckley,
B., Aldenderfer, M., and Mudelsee, M.: A global context for megadroughts in
monsoon Asia during the past millennium, Quaternary Sci. Rev., 30, 47–62,
https://doi.org/10.1016/j.quascirev.2010.10.005, 2011.
Sinha, A., Kathayat, G., Cheng, H., Breitenbach, S. F. M., Berkelhammer, M.,
Mudelsee, M., Biswas, J., and Edwards, R. L.: Trends and oscillations in the
Indian summer monsoon rainfall over the last two millennia, Nat. Commun., 6, 6309,
https://doi.org/10.1038/ncomms7309, 2015.
Sinninghe Damsté, J. S., Ossebaar, J., Abbas, B., Schouten, S.,
and Verschuren, D.: Fluxes and distribution of tetraether lipids in an
equatorial African lake: Constraints on the application of the TEX86
palaeothermometer and BIT index in lacustrine settings, Geochim. Cosmochim.
Ac., 73, 4232–4249, https://doi.org/10.1016/j.gca.2009.04.022, 2009.
Sinninghe Damsté, J. S., Ossebaar, J., Schouten, S., and Verschuren, D.:
Distribution of tetraether lipids in the 25-ka sedimentary record of Lake
Challa: extracting reliable TEX86 and MBT/CBT palaeotemperatures from
an equatorial African lake, Quaternary Sci. Rev., 50, 43–54, https://doi.org/10.1016/j.quascirev.2012.07.001, 2012a.
Sinninghe Damsté, J. S., Rijpstra, W. I. C., Hopmans, E. C., Jung, M.-Y.,
Kim, J.-G., Rhee, S.-K., Stieglmeier, M., and Schleper, C.: Intact Polar and
Core Glycerol Dibiphytanyl Glycerol Tetraether Lipids of Group I.1a and I.1b
Thaumarchaeota in Soil, Appl. Environ Microb., 78, 6866–6874, https://doi.org/10.1128/AEM.01681-12,
2012b.
Sun, W., Zhang, E., Shulmeister, J., Bird, M. I., Chang, J., and Shen, J.: Abrupt
changes in Indian summer monsoon strength during the last deglaciation and
early Holocene based on stable isotope evidence from Lake Chenghai,
southwest China, Quaternary Sci. Rev., 218, 1–9, https://doi.org/10.1016/j.quascirev.2019.06.006, 2019.
Tian, L., Wang, M., Zhang, X., Yang, X., Zong, Y., Jia, G., Zheng, Z., and Man,
M.: Synchronous change of temperature and moisture over the past 50 ka in
subtropical southwest China as indicated by biomarker records in a crater
lake, Quaternary Sci. Rev., 212, 121–134, https://doi.org/10.1016/j.quascirev.2019.04.003, 2019.
Tierney, J. E., Russell, J. M., Huang, Y., Damsté, J. S. S., Hopmans, E. C., and
Cohen, A. S.: Northern Hemisphere controls on tropical southeast African
climate during the past 60 000 years, Science, 322, 252–255, https://doi.org/10.1126/science.1160485, 2008.
Tierney, J. E., Russell, J. M., Eggermont, H., Hopmans, E. C., Verschuren, D., and
Damste, J. S. S.: Environmental controls on branched tetraether lipid
distributions in tropical East African lake sediments, Geochim. Cosmochim.
Ac., 74, 4902–4918, https://doi.org/10.1016/j.gca.2010.06.002, 2010.
Wan, G. J., Chen, J. A., Wu, F. C., Xu, S. Q., Bai, Z. G., Wan, E. Y., Wang, C. S.,
Huang, R. G., Yeager, K. M., and Santschi, P. H.: Coupling between
210Pbex and organic matter in sediments of a nutrient-enriched
lake: An example from Lake Chenghai, China. Chem Geol., 224, 223–236, https://doi.org/10.1016/j.chemgeo.2005.07.025, 2005.
Wang, H., Dong, H., Zhang, C. L., Jiang, H., Zhao, M., Liu, Z., Lai, Z., and Liu,
W.: Water depth affecting thaumarchaeol production in Lake Qinghai,
northeastern Qinghai–Tibetan plateau: Implications for paleo lake levels
and paleoclimate, Chem. Geol., 368, 76–84, https://doi.org/10.1016/j.chemgeo.2014.01.009, 2014.
Wang, H., Dong, H., Zhang, C. L., Jiang, H., Liu, Z., Zhao, M., and Liu, W.:
Deglacial and Holocene archaeal lipid-inferred paleohydrology and
paleotemperature history of Lake Qinghai, northeastern Qinghai–Tibetan
Plateau, Quaternary Res., 83, 116–126, https://doi.org/10.1016/j.yqres.2014.10.003,
2015.
Wang, H., Leng, Q., Liu, W., and Yang, H.: A rapid lake-shallowing event
terminated preservation of the Miocene Clarkia Fossil
Konservat-Lagerstätte (Idaho, USA), Geology, 45, 239–242, https://doi.org/10.1130/G38434.1, 2017.
Wang, H., He, Y., Liu, W., Zhou, A., Kolpakova, M., Krivonogov, S., and Liu, Z.:
Lake Water Depth Controlling Archaeal Tetraether Distributions in
Midlatitude Asia: Implications for Paleo Lake-Level Reconstruction, Geophys.
Res. Lett., 46, 5274–5283, https://doi.org/10.1029/2019GL082157, 2019.
Wang, M., Zheng, Z., Man, M., Hu, J., and Gao, Q.: Branched GDGT-based
paleotemperature reconstruction of the last 30,000 years in humid monsoon
region of Southeast China, Chem. Geol., 463, 94–102, https://doi.org/10.1016/j.chemgeo.2017.05.014, 2017.
Wang, M., Tian, Q., Li, X., Liang, J., He, Y., and Hou, J.: TEX86 as a
potential proxy of lake water pH in the Tibetan Plateau, Palaeogeogr.
Palaeocl., 538, 109381, https://doi.org/10.1016/j.palaeo.2019.109381, 2020.
Wang, Q., Yang, X., Anderson, N. J., Zhang, E., and Li, Y.: Diatom response to
climate forcing of a deep, alpine lake (Lugu Hu, Yunnan, SW China) during
the Last Glacial Maximum and its implications for understanding regional
monsoon variability, Quaternary Sci. Rev., 86, 1–12, https://doi.org/10.1016/j.quascirev.2013.12.024, 2014b.
Wang, S. and Dou, H.: Lakes in China, Science Press, Beijing, China, 1998 (in
Chinese).
Weijers, J. W. H., Schouten, S., Spaargaren, O. C., and Damste, J. S. S.: Occurrence
and distribution of tetraether membrane lipids in soils: Implications for
the use of the TEX86 proxy and the BIT index, Org. Geochem., 37,
1680–1693, https://doi.org/10.1016/j.orggeochem.2006.07.018, 2006.
Wu, D., Zhou, A., Chen, X., Yu, J., Zhang, J., and Sun, H.: Hydrological and
ecosystem response to abrupt changes in the Indian monsoon during the last
glacial, as recorded by sediments from Xingyun Lake, Yunnan, China,
Palaeogeogr. Palaeocl., 421, 15–23, https://doi.org/10.1016/j.palaeo.2015.01.005, 2015.
Wu, D., Chen, X., Lv, F., Brenner, M., Curtis, J., Zhou, A., Chen, J.,
Abbott, M., Yu, J., and Chen, F.: Decoupled early Holocene summer temperature
and monsoon precipitation in southwest China, Quaternary Sci. Rev., 193,
54–67, https://doi.org/10.1016/j.quascirev.2018.05.038, 2018.
Wu, J., Gagan, M. K., Jiang, X., Xia, W., and Wang, S.: Sedimentary geochemical
evidence for recent eutrophication of Lake Chenghai, Yunnan, China, J.
Paleoclim., 32, 85–94, 2004.
Yang, H., Lu, X. X., Ding, W. H., Lei, Y. Y., Dang, X. Y., and Xie, S. C.: The 6-methyl branched tetraethers significantly affect the performance of the methylation index (MBT ') in soils from an altitudinal transect at Mount Shennongjia, Org. Geochem., 82, 42–53, https://doi.org/10.1016/j.orggeochem.2015.02.003, 2015.
Yang, H., Xiao, W., Słowakiewicz, M., Ding, W., Ayari, A., Dang, X., and Pei,
H.: Depth-dependent variation of archaeal ether lipids along soil and peat
profiles from southern China: Implications for the use of isoprenoidal GDGTs
as environmental tracers, Org. Geochem., 128, 42–56, https://doi.org/10.1016/j.orggeochem.2018.12.009, 2019.
Yao, Y., Zhao, J., Bauersachs, T., and Huang, Y.: Effect of water depth on the
TEX86 proxy in volcanic lakes of northeastern China, Org. Geochem., 129,
88–98, https://doi.org/10.1016/j.orggeochem.2019.01.014, 2019.
Zhang, E., Wang, Y., Sun, W., and Shen, J.: Holocene Asian monsoon evolution revealed by a pollen record from an alpine lake on the southeastern margin of the Qinghai–Tibetan Plateau, China, Clim. Past, 12, 415–427, https://doi.org/10.5194/cp-12-415-2016, 2016.
Zhang, E., Chang, J., Cao, Y., Sun, W., Shulmeister, J., Tang, H., Langdon,
P. G., Yang, X., and Shen, J.: Holocene high-resolution quantitative summer
temperature reconstruction based on subfossil chironomids from the southeast
margin of the Qinghai-Tibetan Plateau, Quaternary Sci. Rev., 165, 1–12, https://doi.org/10.1016/j.quascirev.2017.04.008, 2017a.
Zhang, E., Zhao, C., Xue, B., Liu, Z., Yu, Z., Chen, R., and Shen, J.:
Millennial-scale hydroclimate variations in southwest China linked to
tropical Indian Ocean since the Last Glacial Maximum, Geology, 45, 435–438,
https://doi.org/10.1130/G38309.1, 2017b.
Zhang, E., Sun, W., Chang, J., Ning, D., and Shulmeister, J.: Variations of the
Indian summer monsoon over the last 30 000 years inferred from a pyrogenic
carbon record from south-west China, J. Quaternary Sci., 33, 131–138, https://doi.org/10.1002/jqs.3008, 2018.
Zhang, E., Chang, J., Shulmeister, J., Langdon, P., Sun, W., Cao, Y., Yang,
X., and Shen, J.: Summer temperature fluctuations in Southwestern China during
the end of the LGM and the last deglaciation, Earth. Planet. Sc. Lett., 509,
78–87, https://doi.org/10.1016/j.epsl.2018.12.024, 2019.
Zheng, Y., Pancost, R. D., Naafs, B. D. A., Li, Q., Liu, Z., and Yang, H.:
Transition from a warm and dry to a cold and wet climate in NE China across
the Holocene, Earth. Planet. Sc. Lett., 493, 36–46, https://doi.org/10.1016/j.epsl.2018.04.019, 2018.