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Central China as a Lgm Plant Refugia: Insights from Biome Reconstruction for Palaeoclimate Information
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Outgoing claims: the papers this work cites, builds on, or argues with.
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A Last Glacial Maximum pollen record from Bodmin Moor showing a possible cryptic northern refugium in southwest England
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Reconstructing biomes from palaeoecological data: a general method and its application to European pollen data at 0 and 6 ka
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The effect of atmospheric CO2 and ice sheet topography on LGM climate
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Tropical forcing orbital-scale precipitation variations revealed by a maar lake record in South China
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Precipitation–altitude relationships on different timescales and at different precipitation magnitudes in the Qilian Mountains
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The relationship between altitude of meteorological stations and average monthly and annual precipitation
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The vegetation feature and palaeoenvironment significance in the mountainous interior of southern China from the Last Glacial Maximum
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Quantitative climatic reconstruction of the Last Glacial Maximum in China
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High-resolution geochemistry records of climate changes since late-glacial from Dajiuhu peat in Shennongjia Mountains, Central China
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Vegetation and climate change during Marine Isotope Stage 3 in China
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Spatial variation of altitudinal belts as dividing index between warm temperate and subtropical zones in the Qinling-Daba Mountains
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Vegetation history of the Loess Plateau of China during the last 100,000 years based on pollen data
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The variation of summer monsoon precipitation in central China since the last deglaciation
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Topographic and biotic factors determine forest biomass spatial distribution in a subtropical mountain moist forest
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Quantifying modern biomes based on surface pollen data in China
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An updated biomization scheme and vegetation reconstruction based on a synthesis of modern and mid-Holocene pollen data in China
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Millennial-scale variability in the Asian monsoon: Evidence from oxygen isotope records from stalagmites in southeastern China
inferredcites →https://doi.org/10.1016/j.palaeo.2010.02.008openalex-extracted
Palaeovegetation in China during the late Quaternary: Biome reconstructions based on a global scheme of plant functional types
inferredcites →https://doi.org/10.1016/j.palaeo.2011.05.026openalex-extracted
Pollen record of the past 60 ka BP in the Middle Okinawa Trough: Terrestrial provenance and reconstruction of the paleoenvironment
inferredcites →https://doi.org/10.1016/j.palaeo.2016.04.020openalex-extracted
Revisiting last glacial maximum climate over China and East Asian monsoon using PMIP3 simulations
inferredcites →https://doi.org/10.1016/j.palaeo.2017.01.038openalex-extracted
A 20,000-year high-resolution pollen record from Huguangyan Maar Lake in tropical–subtropical South China
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A 40,000 year record of vegetation, environment and climate change from Chongqing, Central China
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Environmental changes recorded by multiple indices in Erxianyan wetland in the past 1900 years, Central China
inferredcites →https://doi.org/10.1016/j.palaeo.2023.111399openalex-extracted
A continuous paleorecord of vegetation and environmental change from Erxianyan Wetland over the past 60,000 years in central China
inferredcites →https://doi.org/10.1016/j.quaint.2004.02.001openalex-extracted
The Huguang maar lake—a high-resolution record of palaeoenvironmental and palaeoclimatic changes over the last 78,000 years from South China
inferredcites →https://doi.org/10.1016/j.quaint.2012.01.009openalex-extracted
Vegetation changes during the past 40,000 years in Central China from a long fossil record
inferredcites →https://doi.org/10.1016/j.quaint.2018.11.016openalex-extracted
Large-scale vegetation history in China and its response to climate change since the Last Glacial Maximum
inferredcites →https://doi.org/10.1016/j.quascirev.2003.06.021openalex-extracted
Palaeo-climate reconstruction from stable isotope variations in speleothems: a review
inferredcites →https://doi.org/10.1016/j.quascirev.2004.06.002openalex-extracted
Trees or no trees? The environments of central and eastern Europe during the Last Glaciation
inferredcites →https://doi.org/10.1016/j.quascirev.2012.12.014openalex-extracted
Quantitative reconstructions in palaeolimnology: new paradigm or sick science?
inferredcites →https://doi.org/10.1016/j.quascirev.2015.07.021openalex-extracted
Holocene vegetation and climate dynamics of NE China based on the pollen record from Sihailongwan Maar Lake
inferredcites →https://doi.org/10.1016/j.quascirev.2019.07.034openalex-extracted
Northern Hemisphere biome changes (>30°N) since 40 cal ka BP and their driving factors inferred from model-data comparisons
inferredcites →https://doi.org/10.1016/j.quascirev.2022.107371openalex-extracted
Intensified climate drying and cooling during the last glacial culmination (20.8–17.5 cal ka BP) in the south-eastern Asian monsoon domain inferred from a high-resolution pollen record
inferredcites →https://doi.org/10.1016/j.revpalbo.2015.08.001openalex-extracted
Late Pleistocene montane vegetation and climate history from the Dajiuhu Basin in the western Hubei Province of Central China
inferredcites →https://doi.org/10.1029/2002jd002558openalex-extracted
Climate change and Arctic ecosystems: 1. Vegetation changes north of 55°N between the last glacial maximum, mid‐Holocene, and present
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Synergistic Impact of Complex Topography and Climate Variability on the Loss of Microclimate Heterogeneity in Southeast Asia
inferredcites →https://doi.org/10.1038/nature06164openalex-extracted
Millennial-scale trends in west Pacific warm pool hydrology since the Last Glacial Maximum
inferredcites →https://doi.org/10.1038/nature06692openalex-extracted
Millennial- and orbital-scale changes in the East Asian monsoon over the past 224,000 years
inferredcites →https://doi.org/10.1038/nature18591openalex-extracted
The Asian monsoon over the past 640,000 years and ice age terminations
inferredcites →https://doi.org/10.1038/s41467-018-06837-3openalex-extracted
Identifying long-term stable refugia for relict plant species in East Asia
inferredcites →https://doi.org/10.1038/s41467-019-09866-8openalex-extracted
Position and orientation of the westerly jet determined Holocene rainfall patterns in China
inferredcites →https://doi.org/10.1038/s41559-019-0842-1openalex-extracted
Global buffering of temperatures under forest canopies
inferredcites →https://doi.org/10.1038/s41586-023-06577-5openalex-extracted
The geography of climate and the global patterns of species diversity
inferredcites →https://doi.org/10.1038/srep43822openalex-extracted
Potential effects of climate change on geographic distribution of the Tertiary relict tree species Davidia involucrata in China
inferredcites →https://doi.org/10.1046/j.1365-2699.1998.00235.xopenalex-extracted
BIOME 6000: reconstructing global mid‐Holocene vegetation patterns from palaeoecological records
inferredcites →https://doi.org/10.1086/338542openalex-extracted
Species Richness and Altitude: A Comparison between Null Models and Interpolated Plant Species Richness along the Himalayan Altitudinal Gradient, Nepal
inferredcites →https://doi.org/10.1098/rstb.2006.1985openalex-extracted
Response of pollen diversity to the climate-driven altitudinal shift of vegetation in the Colombian Andes
inferredcites →https://doi.org/10.1098/rstb.2019.0297openalex-extracted
Using historical and palaeoecological data to inform ambitious species recovery targets
inferredcites →https://doi.org/10.1111/gcb.15569openalex-extracted
Forest microclimates and climate change: Importance, drivers and future research agenda
inferredcites →https://doi.org/10.1111/j.1365-2699.2008.02051.xopenalex-extracted
Glacial refugia influence plant diversity patterns in the Mediterranean Basin
inferredcites →https://doi.org/10.1111/j.1365-2699.2009.02187.xopenalex-extracted
Fossil evidence and phylogeography of temperate species: ‘glacial refugia’ and post‐glacial recolonization
inferredcites →https://doi.org/10.1126/science.1073083openalex-extracted
Buffered Tree Population Changes in a Quaternary Refugium: Evolutionary Implications
inferredcites →https://doi.org/10.1126/science.aat9393openalex-extracted
East Asian hydroclimate modulated by the position of the westerlies during Termination I
inferredcites →https://doi.org/10.1126/science.aax0149openalex-extracted
Humboldt’s enigma: What causes global patterns of mountain biodiversity?
inferredcites →https://doi.org/10.1177/0959683615584206openalex-extracted
Last deglacial and Holocene vegetation evolution and climate variability in the subalpine western Nanling Mountains in South China
inferredcites →https://doi.org/10.1371/journal.pone.0175742openalex-extracted
Response of spatial vegetation distribution in China to climate changes since the Last Glacial Maximum (LGM)
inferredcites →https://doi.org/10.17520/biods.2019283openalex-extracted
Structure and spatial distribution pattern of a native Metasequoia glyptostroboides population in Hubei
inferredcites →https://doi.org/10.3389/fevo.2021.734011openalex-extracted
Vegetation Response to Holocene Climate Change in the Qinling Mountains in the Temperate–Subtropical Transition Zone of Central–East China
inferredcites →https://doi.org/10.3724/sp.j.1261.2013.00032openalex-extracted
Artemisia pollen-indicated steppe distribution in southern China during the Last Glacial Maximum
inferredcites →https://doi.org/10.5194/cp-3-279-2007openalex-extracted
Results of PMIP2 coupled simulations of the Mid-Holocene and Last Glacial Maximum – Part 2: feedbacks with emphasis on the location of the ITCZ and mid- and high latitudes heat budget
inferredcites →https://doi.org/10.5194/cp-9-2759-2013openalex-extracted
A pollen-based biome reconstruction over the last 3.562 million years in the Far East Russian Arctic – new insights into climate–vegetation relationships at the regional scale
inferredcites →https://doi.org/10.7525/j.issn.1673-5102.2011.05.019openalex-extracted
An Overview on the Potential Quaternary Glacial Refugia of Plants in China Mainland
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