Articles | Volume 12, issue 12
Research article 19 Dec 2016
Research article | 19 Dec 2016
Quantitative reconstruction of summer precipitation using a mid-Holocene δ13C common millet record from Guanzhong Basin, northern China
Qing Yang et al.
Related subject area
Subject: Proxy Use-Development-Validation | Archive: Terrestrial Archives | Timescale: HoloceneSampling density and date along with species selection influence spatial representation of tree-ring reconstructionsChanges in high-intensity precipitation on the northern Apennines (Italy) as revealed by multidisciplinary data over the last 9000 yearsNeoglacial trends in diatom dynamics from a small alpine lake in the Qinling mountains of central ChinaCentennial- to millennial-scale monsoon changes since the last deglaciation linked to solar activities and North Atlantic coolingAlgal lipids reveal unprecedented warming rates in alpine areas of SW Europe during the industrial periodReconstructing seasonality through stable-isotope and trace-element analyses of the Proserpine stalagmite, Han-sur-Lesse cave, Belgium: indications for climate-driven changes during the last 400 yearsTwo millennia of Main region (southern Germany) hydroclimate variabilityCombining a pollen and macrofossil synthesis with climate simulations for spatial reconstructions of European climate using Bayesian filteringLignin oxidation products as a potential proxy for vegetation and environmental changes in speleothems and cave drip water – a first record from the Herbstlabyrinth, central GermanyHow dry was the Younger Dryas? Evidence from a coupled δ2H–δ18O biomarker paleohygrometer applied to the Gemündener Maar sediments, Western Eifel, GermanySiberian tree-ring and stable isotope proxies as indicators of temperature and moisture changes after major stratospheric volcanic eruptionsThe 4.2 ka BP Event in the Mediterranean region: an overviewTechnical note: Optimizing the utility of combined GPR, OSL, and Lidar (GOaL) to extract paleoenvironmental records and decipher shoreline evolutionThe onset of neoglaciation in Iceland and the 4.2 ka eventHydroclimatic variations in southeastern China during the 4.2 ka event reflected by stalagmite recordsFire, vegetation, and Holocene climate in a southeastern Tibetan lake: a multi-biomarker reconstruction from Paru CoClimate impact on the development of Pre-Classic Maya civilisationSynchronizing 10Be in two varved lake sediment records to IntCal13 14C during three grand solar minimaTechnical note: Open-paleo-data implementation pilot – the PAGES 2k special issueA chironomid-based record of temperature variability during the past 4000 years in northern China and its possible societal implicationsInsights into Atlantic multidecadal variability using the Last Millennium Reanalysis frameworkThree distinct Holocene intervals of stalagmite deposition and nondeposition revealed in NW Madagascar, and their paleoclimate implicationsExamining bias in pollen-based quantitative climate reconstructions induced by human impact on vegetation in ChinaA dual-biomarker approach for quantification of changes in relative humidity from sedimentary lipid D∕H ratiosPseudo-proxy tests of the analogue method to reconstruct spatially resolved global temperature during the Common EraDevelopment and evaluation of a system of proxy data assimilation for paleoclimate reconstructionA chironomid-based mean July temperature inference model from the south-east margin of the Tibetan Plateau, ChinaAssessing performance and seasonal bias of pollen-based climate reconstructions in a perfect model worldNorth Atlantic Oscillation controls on oxygen and hydrogen isotope gradients in winter precipitation across Europe; implications for palaeoclimate studiesA 368-year maximum temperature reconstruction based on tree-ring data in the northwestern Sichuan Plateau (NWSP), ChinaInferring late-Holocene climate in the Ecuadorian Andes using a chironomid-based temperature inference modelA high-altitude peatland record of environmental changes in the NW Argentine Andes (24 ° S) over the last 2100 yearsTechnical note: The Linked Paleo Data framework – a common tongue for paleoclimatologyA Bayesian hierarchical model for reconstructing relative sea level: from raw data to rates of changeInferring climate variability from nonlinear proxies: application to palaeo-ENSO studiesTechnical Note: How accurate can stalagmite formation temperatures be determined using vapour bubble radius measurements in fluid inclusions?High-resolution leaf wax carbon and hydrogen isotopic record of the late Holocene paleoclimate in arid Central AsiaArctic Holocene proxy climate database – new approaches to assessing geochronological accuracy and encoding climate variablesTesting long-term summer temperature reconstruction based on maximum density chronologies obtained by reanalysis of tree-ring data sets from northernmost Sweden and FinlandConstraining Holocene hydrological changes in the Carpathian–Balkan region using speleothem δ18O and pollen-based temperature reconstructionsSediment transport processes across the Tibetan Plateau inferred from robust grain-size end members in lake sedimentsSimilarity estimators for irregular and age-uncertain time seriesMid- and late Holocene dust deposition in western Europe: the Misten peat bog (Hautes Fagnes – Belgium)A mid-Holocene climate reconstruction for eastern South AmericaNorth–south palaeohydrological contrasts in the central Mediterranean during the Holocene: tentative synthesis and working hypothesesLate Neolithic Mondsee Culture in Austria: living on lakes and living with flood risk?Tree-ring–based summer mean temperature variations in the Adamello–Presanella Group (Italian Central Alps), 1610–2008 ADLong-term summer sunshine/moisture stress reconstruction from tree-ring widths from Bosnia and HerzegovinaStalagmite water content as a proxy for drip water supply in tropical and subtropical areasThe magnesium isotope record of cave carbonate archives
Justin T. Maxwell, Grant L. Harley, Trevis J. Matheus, Brandon M. Strange, Kayla Van Aken, Tsun Fung Au, and Joshua C. Bregy
Clim. Past, 16, 1901–1916,Short summary
We found that increasing the density of chronologies in the tree-ring network resulted in estimated soil moisture conditions that better matched the spatial variability of the values that were instrumentally recorded for droughts and, to a lesser extent, pluvials. By sampling trees in 2010 compared to 1980, the sensitivity of tree rings to soil moisture decreased in the southern portion of our region, where severe drought conditions have been absent over recent decades.
Stefano Segadelli, Federico Grazzini, Veronica Rossi, Margherita Aguzzi, Silvia Marvelli, Marco Marchesini, Alessandro Chelli, Roberto Francese, Maria Teresa De Nardo, and Sandro Nanni
Clim. Past, 16, 1547–1564,Short summary
In an attempt to consolidate trends in the hydrological cycle induced by recent warming, we conducted a multidisciplinary study combining meteorological data, climate proxies from the literature, and original coring and pollen data acquired in an area that has been hit by record-breaking precipitation events. A detailed study of recent flash-flood deposits compared with fossil peat bog and lake sediments supports the expected increase in precipitation intensity during warm climatic phases.
Bo Cheng, Jennifer Adams, Jianhui Chen, Aifeng Zhou, Qing Zhang, and Anson W. Mackay
Clim. Past, 16, 543–554,Short summary
The Qinling mountains in China are biodiversity rich. We studied one of the high-latitude lakes on Mount Taibai with a view to looking at how aquatic diversity responded to long-term changes in climate over the past 3500 years. We specifically looked at a group of single-celled algae called diatoms, as they are very sensitive to the environment. We found that these algae changed gradually over time, but they showed abrupt change during the period known as the Little Ice Age, about 400 years ago.
Xingxing Liu, Youbin Sun, Jef Vandenberghe, Peng Cheng, Xu Zhang, Evan J. Gowan, Gerrit Lohmann, and Zhisheng An
Clim. Past, 16, 315–324,Short summary
The East Asian summer monsoon and winter monsoon are anticorrelated on a centennial timescale during 16–1 ka. The centennial monsoon variability is connected to changes of both solar activity and North Atlantic cooling events during the Early Holocene. Then, North Atlantic cooling became the major forcing of events during the Late Holocene. This work presents the great challenge and potential to understand the response of the monsoon system to global climate changes in the past and the future.
Antonio García-Alix, Jaime L. Toney, Gonzalo Jiménez-Moreno, Carmen Pérez-Martínez, Laura Jiménez, Marta Rodrigo-Gámiz, R. Scott Anderson, Jon Camuera, Francisco J. Jiménez-Espejo, Dhais Peña-Angulo, and María J. Ramos-Román
Clim. Past, 16, 245–263,Short summary
In this paper we identify warming thresholds, rates, and forcing mechanisms from a novel alpine temperature record of the southern Iberian Peninsula during the Common Era in order to contextualize the modern warming and its potential impact on these vulnerable alpine ecosystems. To do so, we have developed and applied the first lacustrine temperature calibration in alpine lakes for algal compounds, called long-chain alkyl diols, which is a significant advance in biomarker paleothermometry.
Stef Vansteenberge, Niels J. de Winter, Matthias Sinnesael, Sophie Verheyden, Steven Goderis, Stijn J. M. Van Malderen, Frank Vanhaecke, and Philippe Claeys
Clim. Past, 16, 141–160,Short summary
We measured the chemical composition (trace-element concentrations and stable-isotope ratios) of a Belgian speleothem that deposited annual layers. Our sub-annual resolution dataset allows us to investigate how the chemistry of this speleothem recorded changes in the environment and climate in northwestern Europe. We then use this information to reconstruct climate change during the 16th and 17th century on the seasonal scale and demonstrate that environmental change drives speleothem chemistry.
Alexander Land, Sabine Remmele, Jutta Hofmann, Daniel Reichle, Margaret Eppli, Christian Zang, Allan Buras, Sebastian Hein, and Reiner Zimmermann
Clim. Past, 15, 1677–1690,Short summary
With the use of precipitation sensitive oak ring-width series from the Main River region (southern Germany) a 2000-year long hydroclimate reconstruction has been developed. The ring series are sensitive to the sum of rainfall from 26 February to 6 July. This region suffered from severe, long-lasting droughts in the past two millennia (e.g., AD 500/510s, 940s, 1170s, 1390s and 1160s). In the AD 550s, 1050s, 1310s and 1480s, multi-year periods with high rainfall hit the region.
Nils Weitzel, Andreas Hense, and Christian Ohlwein
Clim. Past, 15, 1275–1301,Short summary
A new method for probabilistic spatial reconstructions of past climate states is presented, which combines pollen data with a multi-model ensemble of climate simulations in a Bayesian framework. The approach is applied to reconstruct summer and winter temperature in Europe during the mid-Holocene. Our reconstructions account for multiple sources of uncertainty and are well suited for quantitative statistical analyses of the climate under different forcing conditions.
Inken Heidke, Denis Scholz, and Thorsten Hoffmann
Clim. Past, 15, 1025–1037,Short summary
This is the first quantitative study of lignin biomarkers in stalagmites and cave drip water. Lignin is only produced by higher plants; therefore, its analysis can be used to reconstruct the vegetation of the past. We compared our lignin results with stable isotope and trace element records from the same samples and found correlations or similarities with P, Ba, U and Mg concentrations as well as δ13C values. These results can help to better interpret other vegetation proxies.
Johannes Hepp, Lorenz Wüthrich, Tobias Bromm, Marcel Bliedtner, Imke Kathrin Schäfer, Bruno Glaser, Kazimierz Rozanski, Frank Sirocko, Roland Zech, and Michael Zech
Clim. Past, 15, 713–733,
Olga V. Churakova (Sidorova), Marina V. Fonti, Matthias Saurer, Sébastien Guillet, Christophe Corona, Patrick Fonti, Vladimir S. Myglan, Alexander V. Kirdyanov, Oksana V. Naumova, Dmitriy V. Ovchinnikov, Alexander V. Shashkin, Irina P. Panyushkina, Ulf Büntgen, Malcolm K. Hughes, Eugene A. Vaganov, Rolf T. W. Siegwolf, and Markus Stoffel
Clim. Past, 15, 685–700,Short summary
We present a unique dataset of multiple tree-ring and stable isotope parameters, representing temperature-sensitive Siberian ecotones, to assess climatic impacts after six large stratospheric volcanic eruptions at 535, 540, 1257, 1640, 1815, and 1991 CE. Besides the well-documented effects of temperature derived from tree-ring width and latewood density, stable carbon and oxygen isotopes in tree-ring cellulose provide information about moisture and sunshine duration changes after the events.
Monica Bini, Giovanni Zanchetta, Aurel Perşoiu, Rosine Cartier, Albert Català, Isabel Cacho, Jonathan R. Dean, Federico Di Rita, Russell N. Drysdale, Martin Finnè, Ilaria Isola, Bassem Jalali, Fabrizio Lirer, Donatella Magri, Alessia Masi, Leszek Marks, Anna Maria Mercuri, Odile Peyron, Laura Sadori, Marie-Alexandrine Sicre, Fabian Welc, Christoph Zielhofer, and Elodie Brisset
Clim. Past, 15, 555–577,Short summary
The Mediterranean region has returned some of the clearest evidence of a climatically dry period occurring approximately 4200 years ago. We reviewed selected proxies to infer regional climate patterns between 4.3 and 3.8 ka. Temperature data suggest a cooling anomaly, even if this is not uniform, whereas winter was drier, along with dry summers. However, some exceptions to this prevail, where wetter condition seems to have persisted, suggesting regional heterogeneity.
Amy J. Dougherty, Jeong-Heon Choi, Chris S. M. Turney, and Anthony Dosseto
Clim. Past, 15, 389–404,
Áslaug Geirsdóttir, Gifford H. Miller, John T. Andrews, David J. Harning, Leif S. Anderson, Christopher Florian, Darren J. Larsen, and Thor Thordarson
Clim. Past, 15, 25–40,Short summary
Compositing climate proxies in sediment from seven Iceland lakes documents abrupt summer cooling between 4.5 and 4.0 ka, statistically indistinguishable from 4.2 ka. Although the decline in summer insolation was an important factor, a combination of superposed changes in ocean circulation and explosive Icelandic volcanism were likely responsible for the abrupt perturbation recorded by our proxies. Lake and catchment proxies recovered to a colder equilibrium state following the perturbation.
Haiwei Zhang, Hai Cheng, Yanjun Cai, Christoph Spötl, Gayatri Kathayat, Ashish Sinha, R. Lawrence Edwards, and Liangcheng Tan
Clim. Past, 14, 1805–1817,Short summary
The collapses of several Neolithic cultures in China are considered to have been associated with abrupt climate change during the 4.2 ka BP event; however, the hydroclimate of this event in China is still poorly known. Based on stalagmite records from monsoonal China, we found that north China was dry but south China was wet during this event. We propose that the rain belt remained longer at its southern position, giving rise to a pronounced humidity gradient between north and south China.
Alice Callegaro, Dario Battistel, Natalie M. Kehrwald, Felipe Matsubara Pereira, Torben Kirchgeorg, Maria del Carmen Villoslada Hidalgo, Broxton W. Bird, and Carlo Barbante
Clim. Past, 14, 1543–1563,Short summary
Holocene fires and vegetation are reconstructed using different molecular markers with a single analytical method, applied for the first time to lake sediments from Tibet. The early Holocene shows oscillations between grasses and conifers, with smouldering fires represented by levoglucosan peaks, and high-temperature fires represented by PAHs. The lack of human FeSts excludes local human influence on fire and vegetation changes. Late Holocene displays an increase in local to regional combustion.
Kees Nooren, Wim Z. Hoek, Brian J. Dermody, Didier Galop, Sarah Metcalfe, Gerald Islebe, and Hans Middelkoop
Clim. Past, 14, 1253–1273,Short summary
We present two new palaeoclimatic records for the central Maya lowlands, adding valuable new insights to the impact of climate change on the development of Maya civilisation. Lake Tuspan's diatom record is indicative of precipitation changes at a local scale, while a beach ridge elevation record from the world's largest late Holocene beach ridge plain provides a regional picture.
Markus Czymzik, Raimund Muscheler, Florian Adolphi, Florian Mekhaldi, Nadine Dräger, Florian Ott, Michał Słowinski, Mirosław Błaszkiewicz, Ala Aldahan, Göran Possnert, and Achim Brauer
Clim. Past, 14, 687–696,Short summary
Our results provide a proof of concept for facilitating 10Be in varved lake sediments as a novel synchronization tool required for investigating leads and lags of proxy responses to climate variability. They also point to some limitations of 10Be in these archives mainly connected to in-lake sediment resuspension processes.
Darrell S. Kaufman and PAGES 2k special-issue editorial team
Clim. Past, 14, 593–600,Short summary
We explain the procedure used to attain a high and consistent level of data stewardship across a special issue of the journal Climate of the Past. We discuss the challenges related to (1) determining which data are essential for public archival, (2) using data generated by others, and (3) understanding data citations. We anticipate that open-data sharing in paleo sciences will accelerate as the advantages become more evident and as practices that reduce data loss become the accepted convention.
Haipeng Wang, Jianhui Chen, Shengda Zhang, David D. Zhang, Zongli Wang, Qinghai Xu, Shengqian Chen, Shijin Wang, Shichang Kang, and Fahu Chen
Clim. Past, 14, 383–396,Short summary
The chironomid-inferred temperature record from Gonghai Lake exhibits a stepwise decreasing trend since 4 ka. A cold event in the Era of Disunity, the Sui-Tang Warm Period, the Medieval Warm Period and the Little Ice Age can all be recognized in our record, as well as in many other temperature reconstructions in China. Local wars in Shanxi Province, documented in the historical literature during the past 2700 years, are statistically significantly correlated with changes in temperature.
Hansi K. A. Singh, Gregory J. Hakim, Robert Tardif, Julien Emile-Geay, and David C. Noone
Clim. Past, 14, 157–174,Short summary
The Atlantic Multidecadal Oscillation (AMO) is prominent in the climate system. We study the AMO over the last 2000 years using a novel proxy framework, the Last Millennium Reanalysis. We find that the AMO is linked to continental warming, Arctic sea ice retreat, and an Atlantic precipitation shift. Low clouds decrease globally. We find no distinct multidecadal spectral peak in the AMO over the last 2 millennia, suggesting that human activities may have enhanced the AMO in the modern era.
Ny Riavo Gilbertinie Voarintsoa, Loren Bruce Railsback, George Albert Brook, Lixin Wang, Gayatri Kathayat, Hai Cheng, Xianglei Li, Richard Lawrence Edwards, Amos Fety Michel Rakotondrazafy, and Marie Olga Madison Razanatseheno
Clim. Past, 13, 1771–1790,Short summary
This research has been an investigation of two stalagmites from two caves in NW Madagascar to reconstruct the region's paleoenvironmental changes, and to understand the linkage of such changes to the dynamics of the ITCZ. Stable isotopes, mineralogy, and petrography suggest wetter climate conditions than today during the early and late Holocene, when the mean ITCZ was south, and drier during the mid-Holocene when the ITCZ was north.
Wei Ding, Qinghai Xu, and Pavel E. Tarasov
Clim. Past, 13, 1285–1300,Short summary
Pollen-based past climate reconstruction for regions with long-term human occupation is always controversial. We examined the bias induced by the human impact on vegetation in a climate reconstruction for temperate eastern China by comparing the deviations in the reconstructed results for a fossil record based on two pollen–climate calibration sets. Climatic signals in pollen assemblages are indeed obscured by human impact; however, the extent of the bias could be assessed.
Oliver Rach, Ansgar Kahmen, Achim Brauer, and Dirk Sachse
Clim. Past, 13, 741–757,Short summary
Currently, reconstructions of past changes in the hydrological cycle are usually qualitative, which is a major drawback for testing the accuracy of models in predicting future responses. Here we present a proof of concept of a novel approach to deriving quantitative paleohydrological data, i.e. changes in relative humidity, from lacustrine sediment archives, employing a combination of organic geochemical methods and plant physiological modeling.
Juan José Gómez-Navarro, Eduardo Zorita, Christoph C. Raible, and Raphael Neukom
Clim. Past, 13, 629–648,Short summary
This contribution aims at assessing to what extent the analogue method, a classic technique used in other branches of meteorology and climatology, can be used to perform gridded reconstructions of annual temperature based on the limited information from available but un-calibrated proxies spread across different locations of the world. We conclude that it is indeed possible, albeit with certain limitations that render the method comparable to more classic techniques.
Atsushi Okazaki and Kei Yoshimura
Clim. Past, 13, 379–393,Short summary
Data assimilation has been successfully applied in the field of paleoclimatology to reconstruct past climate. However, data reconstructed from proxies have been assimilated, as opposed to the actual proxy values, which prevented full utilization of the information recorded in the proxies. This study propose a new data assimilation system in which actual proxy data are directly assimilated.
Enlou Zhang, Jie Chang, Yanmin Cao, Hongqu Tang, Pete Langdon, James Shulmeister, Rong Wang, Xiangdong Yang, and Ji Shen
Clim. Past, 13, 185–199,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.
Kira Rehfeld, Mathias Trachsel, Richard J. Telford, and Thomas Laepple
Clim. Past, 12, 2255–2270,Short summary
Indirect evidence on past climate comes from the former composition of ecological communities such as plants, preserved as pollen grains in sediments of lakes. Transfer functions convert relative counts of species to a climatologically meaningful scale (e.g. annual mean temperature in degrees C). We show that the fundamental assumptions in the algorithms impact the reconstruction results in he idealized model world, in particular if the reconstructed variables were not ecologically relevant.
Michael Deininger, Martin Werner, and Frank McDermott
Clim. Past, 12, 2127–2143,Short summary
This study investigates the NAO (Northern Atlantic Oscillation)-related mechanisms that control winter precipitation stable oxygen and hydrogen isotope gradients across Europe. The results show that past longitudinal stable oxygen and hydrogen isotope gradients in European rainfall stored in palaeoclimate archives (e.g. speleothems) can be used to infer the past winter NAO modes from its variations.
Liangjun Zhu, Yuandong Zhang, Zongshan Li, Binde Guo, and Xiaochun Wang
Clim. Past, 12, 1485–1498,Short summary
We present a 368-year late summer maximum temperature reconstruction based on spruce tree rings. It touches on the critical topic of climate reconstruction in the eastern edge of Tibetan Plateau and represents an extension and enhancement of climate records for this area. The Little Ice Age was well represented and 20th century warming was not obvious in this reconstruction. This temperature variation may be affected by global land–sea atmospheric circulation as well as solar and volcanic forcing.
Frazer Matthews-Bird, Stephen J. Brooks, Philip B. Holden, Encarni Montoya, and William D. Gosling
Clim. Past, 12, 1263–1280,Short summary
Chironomidae are a family of two-winged aquatic fly of the order Diptera. The family is species rich (> 5000 described species) and extremely sensitive to environmental change, particualy temperature. Across the Northern Hemisphere, chironomids have been widely used as paleotemperature proxies as the chitinous remains of the insect are readily preserved in lake sediments. This is the first study using chironomids as paleotemperature proxies in tropical South America.
Karsten Schittek, Sebastian T. Kock, Andreas Lücke, Jonathan Hense, Christian Ohlendorf, Julio J. Kulemeyer, Liliana C. Lupo, and Frank Schäbitz
Clim. Past, 12, 1165–1180,Short summary
Cushion peatlands are versatile climate archives for the study of past environmental changes. We present the environmental history for the last 2100 years of Cerro Tuzgle peatland, which is located in the NW Argentine Puna. The results reflect prominent late Holocene climate anomalies and provide evidence that Northern Hemisphere climate oscillations were extensive. Volcanic forcing at the beginning of the 19th century seems to have had an impact on climatic settings in the Central Andes
Nicholas P. McKay and Julien Emile-Geay
Clim. Past, 12, 1093–1100,Short summary
The lack of accepted data formats and data standards in paleoclimatology is a growing problem that slows progress in the field. Here, we propose a preliminary data standard for paleoclimate data, general enough to accommodate all the proxy and measurement types encountered in a large international collaboration (PAGES 2k). We also introduce a data format for such structured data (Linked Paleo Data, or LiPD), leveraging recent advances in knowledge representation (Linked Open Data).
Niamh Cahill, Andrew C. Kemp, Benjamin P. Horton, and Andrew C. Parnell
Clim. Past, 12, 525–542,Short summary
We propose a Bayesian model for the reconstruction and analysis of former sea levels. The model provides a single, unifying framework for reconstructing and analyzing sea level through time with fully quantified uncertainty. We illustrate our approach using a case study of Common Era (last 2000 years) sea levels from New Jersey.
J. Emile-Geay and M. Tingley
Clim. Past, 12, 31–50,Short summary
Ignoring nonlinearity in palaeoclimate records (e.g. continental run-off proxies) runs the risk of severely overstating changes in climate variability. Even with the correct model and parameters, some information is irretrievably lost by such proxies. However, we find that a simple empirical transform can do much to improve the situation, and makes them amenable to classical analyses. Doing so on two palaeo-ENSO records markedly changes some of the quantitative inferences made from such records.
F. Spadin, D. Marti, R. Hidalgo-Staub, J. Rička, D. Fleitmann, and M. Frenz
Clim. Past, 11, 905–913,Short summary
Fluid inclusions inside stalagmites retain information on the cave temperature at the time they formed and thus can be used to reconstruct the continental climate of the past. A method for extracting this information based on a thermodynamic model and size measurements of femtosecond-laser-induced vapour bubbles is presented. Applying our method to stalagmites taken from the Milandre cave in the Swiss Jura Mountains demonstrate that palaeotemperatures can be determined with an accuracy of ±1°C.
B. Aichner, S. J. Feakins, J. E. Lee, U. Herzschuh, and X. Liu
Clim. Past, 11, 619–633,
H. S. Sundqvist, D. S. Kaufman, N. P. McKay, N. L. Balascio, J. P. Briner, L. C. Cwynar, H. P. Sejrup, H. Seppä, D. A. Subetto, J. T. Andrews, Y. Axford, J. Bakke, H. J. B. Birks, S. J. Brooks, A. de Vernal, A. E. Jennings, F. C. Ljungqvist, K. M. Rühland, C. Saenger, J. P. Smol, and A. E. Viau
Clim. Past, 10, 1605–1631,
V. V. Matskovsky and S. Helama
Clim. Past, 10, 1473–1487,
V. Drăguşin, M. Staubwasser, D. L. Hoffmann, V. Ersek, B. P. Onac, and D. Veres
Clim. Past, 10, 1363–1380,
E. Dietze, F. Maussion, M. Ahlborn, B. Diekmann, K. Hartmann, K. Henkel, T. Kasper, G. Lockot, S. Opitz, and T. Haberzettl
Clim. Past, 10, 91–106,
K. Rehfeld and J. Kurths
Clim. Past, 10, 107–122,
M. Allan, G. Le Roux, N. Piotrowska, J. Beghin, E. Javaux, M. Court-Picon, N. Mattielli, S. Verheyden, and N. Fagel
Clim. Past, 9, 2285–2298,
L. F. Prado, I. Wainer, C. M. Chiessi, M.-P. Ledru, and B. Turcq
Clim. Past, 9, 2117–2133,
M. Magny, N. Combourieu-Nebout, J. L. de Beaulieu, V. Bout-Roumazeilles, D. Colombaroli, S. Desprat, A. Francke, S. Joannin, E. Ortu, O. Peyron, M. Revel, L. Sadori, G. Siani, M. A. Sicre, S. Samartin, A. Simonneau, W. Tinner, B. Vannière, B. Wagner, G. Zanchetta, F. Anselmetti, E. Brugiapaglia, E. Chapron, M. Debret, M. Desmet, J. Didier, L. Essallami, D. Galop, A. Gilli, J. N. Haas, N. Kallel, L. Millet, A. Stock, J. L. Turon, and S. Wirth
Clim. Past, 9, 2043–2071,
T. Swierczynski, S. Lauterbach, P. Dulski, and A. Brauer
Clim. Past, 9, 1601–1612,
A. Coppola, G. Leonelli, M. C. Salvatore, M. Pelfini, and C. Baroni
Clim. Past, 9, 211–221,
S. Poljanšek, A. Ceglar, and T. Levanič
Clim. Past, 9, 27–40,
N. Vogel, Y. Scheidegger, M. S. Brennwald, D. Fleitmann, S. Figura, R. Wieler, and R. Kipfer
Clim. Past, 9, 1–12,
S. Riechelmann, D. Buhl, A. Schröder-Ritzrau, D. F. C. Riechelmann, D. K. Richter, H. B. Vonhof, J. A. Wassenburg, A. Geske, C. Spötl, and A. Immenhauser
Clim. Past, 8, 1849–1867,
An, Z. M.: Prehistoric agriculture in China, Acta. Archaeol. Sin., 4, 369–381, in Chinese, 1988.
Araus, J. L. and Buxo, R.: Changes in carbon isotope discrimination in grain cereals from the north-western Mediterranean Basin during the past seven millennia, Aust. J. Plant. Physiol., 20, 117–128, 1993.
Caley, T., Roche, D. M., and Renssen, H.: Orbital Asian summer monsoon dynamics revealed using an isotope-enabled global climate model, Nat. Commun., 5, 5371, https://doi.org/10.1038/ncomms6371, 2014.
Chai, Y.: Broomcorn millet, Chinese Agriculture Press, Beijing, China, 47–70, 1999.
Chen, F. H., Xu, Q. H., Chen, J.H., Birks, H. J. B., Liu, J. B., Zhang, S. R., Jin, L., An, C. B., Telford, R. J., Cao, X. Y., Wang Z. L., Zhang, X. J., Selvaraj, K., Lu, H. Y., Li, Y.C., Zheng, Z., Wang, H. P, Zhou, A. F., Dong, G. H., Zhang, J. W., Huang, X. Z., Bloemendal, J., and Rao, Z. G.: East Asian summer monsoon precipitation variability since the last deglaciation, Sci. Rep., 5, 11186, https://doi.org/10.1038/srep11186, 2015.
Cheng, H., Edwards, R. L., Broecker, W. S., Denton, G. H., Kong, X., Wang. Y., Zhang, R., and Wang, X.: Ice Age Terminations, Science, 326, 248–252, 2009.
Cullen, H. M. and deMenocal, P. B.: North Atlantic influence on Tigris-Euphrates stream flow, Int. J. Climatol., 20, 853–863, 2000.
Cuntz, M.: Carbon cycle: A dent in carbon's gold standard, Nature, 477, 547–548, 2011.
Dawson, T. E., Mambelli, S., Plamboeck, A. H., Templer, P. H., and Tu, K. P.: Stable Isotopes in Plant Ecology, Annu. Rev. Ecol. Syst., 33, 507–559, 2002.
DeMenocal, P. B.: Cultural responses to climate change during the late Holocene, Science, 292, 667–673, 2001.
Dore, M. H. I.: Climate change and changes in global precipitation patterns: What do we know?, Environ. Int., 31, 1167–1181, 2005.
Ehleringer, J. R. and Mooney, H. A.: Photosynthesis and productivity of desert and Mediterranean climate plants, Encyclopedia Plant Physiol (NS), Springer-Verlag, New York, 205–231, 1983.
Falster, D. S., Warton, D. I., and Wright, I. J.: User's guide to SMATR: Standardised Major Axis Tests & Routines Version 2.0, Copyright 2006, http://www.bio.mq.edu.au/ecology/SMATR/ (last access: 14 December 2016), 2006.
Farquhar, G. D., Ehleringer, J. R., and Hubick, K. T.: Carbon isotope discrimination and photosynthesis, Annu. Rev. Plant Physiol. Mol. Biol., 40, 503–537, 1989.
Genty, D., Blamart, D., Ouahdi, R., Gilmour, M., Baker, A., Jouzel, J., and Van-Exter, S.: Precise dating of Dansgaard–Oeschger climate oscillations in western Europe from stalagmite data, Nature, 421, 833–837, 2003.
Guo, Z. T., Liu, T., Guiot, J., Wu, N., L, H., Han, J., Liu, J., and Gu, Z.: High frequency pulses of East Asian monsoon climate in the last two glaciations: link with the North Atlantic, Clim. Dynam, 12, 701–709, 1996.
Hadley, N. F. and Szarek, S. R.: Productivity of desert ecosystems, BioScience, 31, 747–753, 1981.
Hatté, C. and Guiot, J.: Palaeoprecipitation reconstruction by inverse modelling using the isotopic signal of loess organic matter: application to the Nußloch loess sequence (Rhine Valley, Germany), Clim. Dynam., 25, 315–327, 2005.
Hubick, K. T., Hammer, G. L., Farquhar, G. D., Wade, L. J., von Caemmerer, S., and Henderson, S. A.: Carbon isotope discrimination varies genetically in C4 species, Plant. Physiol., 92, 534–537, 1990.
Keeling, C. D. and Whorf, T. P. Atmospheric CO2 – modern record, Mauna Loa, in: Trends 91: A Compendium of Data on Global Change, ORNL/CDIAC-46, edited by: Boden, T A, Sepanski, R. J. and Stoss, F. W., Carbon Dioxide Information Analysis Center, Oak Ridge National Laboratory, Oak Ridge, Tennessee, USA, 12–15, 1992.
Körner, C. H. and Diemer, M.: In situ photosynthetic responses to light, temperature and carbon dioxide in herbaceous plants from low and high altitude, Funct. Ecol., 1, 179–194, 1987.
Körner, C. H., Newmayer, M., Palaez Menendez-Reidl, S., and Smeets-Scheel, A.: Functional morphology of mountain plants, Flora, 182, 353–383, 1989.
LeGrande, A. N. and Schmidt, G. A.: Sources of Holocene variability of oxygen isotopes in paleoclimate archives, Clim. Past, 5, 441–455, https://doi.org/10.5194/cp-5-441-2009, 2009.
Lei, X. S.: Pre-Zhou culture exploration, Science Press, Beijing, China, 2010 (in Chinese).
Leuenberger, M., Siegenthaler, U., and Langway, C. C.: Carbon isotope composition of atmospheric CO2 during the last ice age from an Antarctic ice core, Nature, 357, 488–490, 1992.
Liu, C. J., Jin, G. Y., and Kong, Z. C.: Archaeobotany – Research on Seeds and Fruits, Science Press, Beijing, China, 160–171, 2008.
Liu, J. B., Chen, J. H., Zhang, X. J., Li, Y., Rao, Z. G., and Chen, F. H.: Holocene East Asian summer monsoon records in northern China and their inconsistency with Chinese stalagmite δ18O records, Earth-Sci. Rev., 148, 194–208, 2015.
Lu, H. Y., Han, J. M., Wu, N. Q., and Guo Z. T.: The analysis of modern soil magnetic susceptibility and its paleoclimate significance, Sci. China B, 24, 1290–1297, 1994 (in Chinese).
Lu, H. Y., Wu, N. Q., Liu, T. S., Han, J. M., and Qin X. G.: Seasonal climatic variation recorded by phytolith assemblages from the Baoji loess sequence in central China over the last 150 000, Sci. China D, 39, 629–639, 1996.
Lu, H. Y., Zhang, J. P., Liu, K.-B., Wu, N. Q., Li, Y. M., Zhou, K. S., Ye, M. L., Zhang, T. Y., Zhang, H. J., Yang, X. Y., Shen, L. C., Xu, D. K., Li, Q., and Piperno, D. R.: Earliest domestication of common millet (Panicum miliaceum) in East Asia extended to 10 000 years ago, P. Natl. Acad. Sci. USA, 18, 7367–7372, 2009.
Maher, B. A. and Thompson, R.: Oxyen isotopes from Chinese caves: records not of monsoon rainfall but of circulation regime, J. Quaternary Sci., 27, 615–624, 2012.
Marino, B. D., McElroy, M. B., Salawitch, R. J., and Spaulding, W. G.: Glacial-to-interglacial variations in the carbon isotopic composition of atmospheric CO2, Nature, 357, 461–466, 1992.
Mayewski, P. A., Rohling, E. E., Stager, J. C., Karlén, W., Maasch, K. A., Meeker, L. D., Meyerson, E. A., Gasse, F., van Kreveld, S., Holmgren, K, Lee-Thorp, J., Rosqvist, G., Rack, F., Staubwasser, M., Schneider, R. R., and Steig, E. J.: Holocene climate variability, Quaternary Res., 504, 243–255, 2004.
Murphy, B. P. and Bowman, D. M. J. S.: The carbon and nitrogen isotope composition of Australian grasses in relation to climate, Funct. Ecol., 23, 1040–1049, 2009.
O'Leary, M. H.: Carbon isotopes in photosynthesis, BioScience, 38, 323–336, 1988.
Porter, S. C. and An, Z. S.: Correlation between climate events in the North Atlantic and China during the last glaciation, Nature, 375, 305–308, 1995.
Reimer, P. J., Bard, E., Bayliss, A., Beck, J. W., Blackwell, P. G., Ramsey, C. B., Buck, C. E., Hai C., Edwards, R. L., Friedrich, M., Grootes, P. M., Guilderson, T. P., Haflidason, H., Hajdas, I., Hatté, C., Heaton, T. J., Hoffmann, D. L., Hogg, A. G., Hughen, K. A., and Kaiser, K. F.: IntCal13 and Marine13 radiocarbon age calibration curves 0–50 000 years cal BP, Radiocarbon, 55, 1869–1887, 2013.
Ren, S. N. and Wu, Y. L.: The Neolithic Volume of Chinese Archaeology, Chinese Social Science Press, Beijing, China, in Chinese, 2010.
Schulze, E.-D., Ellis, R., Schulze, W., Trimborn, P., and Ziegler, H.: Diversity, metabolic types and δ13C carbon isotope ratios in the grass flora of Namibia in relation to growth form, precipitation and habitat conditions, Oecologia, 106, 352–369, 1996.
Shen, J., Liu, X. Q., Wang, S. M., and Ryo, M.: Palaeoclimatic changes in the Qinghai Lake area during the last 18 000 years, Quatern. Int., 136, 131–140, 2005.
State Cultural Relics Bureau (Ed.): Atlas of Chinese Cultural Relics: Shannxi Municipality, Xi'an Map Press, Xi'an, China, in Chinese, 1998.
Sun, J. M., Diao, G. Y., Wen, Q. Z., and Zhou, H. Y.: A preliminary study on quantitative estimate of Palaeoclimate by using geochemical transfer function in the Loess Plateau, Geochim., 28, 265–272, 1999 (in Chinese).
Sun, N., Li, X. Q., Dodson, J., Zhou, X. Y., Zhao, K. L., and Yang, Q.: Plant diversity of the Tianshui Basin in the western Loess Plateau during the mid-Holocene – charcoal records from archaeological sites, Quatern. Int., 308–309, 27–35, 2012.
Sun, N. and Li, X. Q.: The quantitative reconstruction of the palaeoclimate between 5200 and 4300 cal yr BP in the Tianshui Basin, NW China, Clim. Past, 8, 625–636, https://doi.org/10.5194/cp-8-625-2012, 2012.
Tan, M.: Circulation effect: response of precipitation δ18O to the ENSO cycle in monsoon regions of China, Clim. Dynam., 42, 1067–1077, 2012.
Tsuyuzaki, S.: Rapid seed extraction from soils by a flotation method, Weed Res., 34, 433–436, 1994.
Ubierna, N., Sun, W., and Cousins, A. B.: The efficiency of C4 photosynthesis under low light conditions: assumptions and calculations with CO2 isotope discrimination, J. Exp. Bot., 1–16, 2011.
Wang, H., Chen, J., Zhang, X., and Chen, F.: Palaeosol development in the Chinese Loess Plateau as an indicator of the strength of the East Asian summer monsoon: Evidence for a mid-Holocene maximum, Quatern. Int., 334, 155–164, 2014.
Wang, Y. J., Cheng H., Edwards, R. L., He Y. Q., Kong, X. G., An, Z. S., Wu, J. Y., Kelly, M. J., Dykoski, C. A., and Li, X. D.: The Holocene Asian monsoon: links to solar changes and North Atlantic climate, Science, 308, 854–857, 2005a.
Wang, G. A., Han, J. M., Zhou, L. P., Xiong, X. G, and Wu, Z. H.: Carbon isotope ratios of plants and occurrences of C4 species under different soil moisture regimes in arid region of Northwest China, Physiol. Plant., 125, 74–81, 2005b.
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., and An, Z. S.: Millennial- and orbital-scale changes in the East Asian monsoon over the past 224 000 years, Nature, 451, 1090–1093, 2008.
Warton, D. I., Wright I. J., Falster, D. S., and Westoby, M.: Bivariate Line-fitting methods for allometry, Biol. Rev., 81, 259–291, 2006.
Wu, W. X. and Liu, T. S.: Possible role of the “Holocene Event 3” on the collapse of Neolithic Cultures around the Central Plain of China, Quatern. Int., 117, 153–166, 2004.
Yang, Q., Li, X. Q., Zhou, X.Y., Zhao, K. L., Ji, M., and Sun, N.: Investigation of the ultrastructural characteristics of foxtail and broomcorn millet during carbonization and its application in archaeobotany, Chinese Sci. Bull, 56, 1495–1502, 2011a.
Yang, Q., Li, X. Q., Liu, W. G., Zhou, X.Y., Zhao, K. L., and Sun, N.: Carbon isotope fractionation during low temperature carbonization of foxtail and common millets, Org. Geochem., 42, 713–719, 2011b.
Yang, L. H., Wang, T., Zhou, J., Lai, Z. P., and Long, H.: OSL chronology and possible forcing mechanisms of dune evolution in the Horqin dunefield in northern China since the Last Glacial Maximum, Quaternary Res., 78, 185–196, 2012.
Yang, Q. and Li, X. Q.: Investigation of the controlled factors influencing carbon isotope composition of foxtail and common millet on the Chinese Loess Plateau, Sci. China D, 58, 2296–2308, 2015.
Yang, Q., Li, X.Q., and Zhou, X.Y.: Vegetation Succession Responding to Climate Changes since LGM in Desert-Loess Transition Zone, North China, Acta. Antherop. Sin., https://doi.org/10.16359/j.cnki.cn11-1963/q.2015.0000, 2015 (in Chinese with English abstract).
Zhang, R and Liu, X. D.: An analogy analysis of summer precipitation change patterns between mid-Holocene and future climatic warming scenarios over East Asia, Sci. Geogr. Sin., 29, 679–683, 2009 (in Chinese with English abstract).
Zhao, J. B.: Soil developed in the Holocene Megathermal and climatic migration in the Guanzhong area, Sci. Geogr. Sin., 23, 554–559, 2003 (in Chinese with English abstract).
Zhao, Z. J. and Xu L. G.: The tentative flotation result and preliminary analysis in Zhouyuan ruins (Wangjiazui site), Cult. Rel., 10, 89–96, 2004 (in Chinese).
The fossilized seeds of common millet are suited to the production of quantitative Holocene precipitation reconstructions. Our reconstructed results showed that summer precipitation from 7.7–3.4 ka BP was ~ 50 mm, or 17 % higher than present levels. Maximal mean summer precipitation peaked at 414 mm during 6.1–5.5 ka BP, ~ 109 mm, or 36 % higher than today, indicating the EASM peaked at this time. This work can provide a new proxy for further research into continuous paleoprecipitation sequences.
The fossilized seeds of common millet are suited to the production of quantitative Holocene...