Global biome patterns of the Middle and Late Pleistocene
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[1] H. Haberl,et al. Land use intensification increasingly drives the spatiotemporal patterns of the global human appropriation of net primary production in the last century , 2021, Global change biology.
[2] J. Singarayer,et al. Projected climatic changes lead to biome changes in areas of previously constant biome , 2021, Journal of Biogeography.
[3] J. Kadereit,et al. Plant speciation in the Quaternary , 2021, Plant Ecology & Diversity.
[4] Sam C. Levin,et al. Synthesizing tree biodiversity data to understand global patterns and processes of vegetation , 2021, Journal of Vegetation Science.
[5] R. Cowling,et al. Plant richness, turnover, and evolutionary diversity track gradients of stability and ecological opportunity in a megadiversity center , 2020, Proceedings of the National Academy of Sciences.
[6] J. Singarayer,et al. Global vegetation patterns of the past 140,000 years , 2020, Journal of Biogeography.
[7] D. Schreve. All is flux: the predictive power of fluctuating Quaternary mammalian faunal-climate scenarios , 2019, Philosophical Transactions of the Royal Society B.
[8] M. McGlone,et al. A Last Interglacial pollen-temperature reconstruction, central North Island, New Zealand , 2017 .
[9] N. Pearce,et al. Age of some Pleistocene interglacial beds and associated fossils in eastern Beringia defined by fission tracks in glass shards of Chester Bluff tephra , 2017, Quaternary Research.
[10] I. Prentice,et al. Reconstructing ice-age palaeoclimates: Quantifying low-CO2 effects on plants , 2017 .
[11] J. Singarayer,et al. Explaining patterns of avian diversity and endemicity: climate and biomes of southern Africa over the last 140,000 years , 2016 .
[12] Thomas F. Stocker,et al. Revision of the EPICA Dome C CO2 record from 800 to 600 kyr before present , 2015 .
[13] P. Jones,et al. Updated high‐resolution grids of monthly climatic observations – the CRU TS3.10 Dataset , 2014 .
[14] Atul K. Jain,et al. Evaluation of 11 terrestrial carbon–nitrogen cycle models against observations from two temperate Free-Air CO2 Enrichment studies , 2014, The New phytologist.
[15] L. Lourens,et al. Persistent 400,000-year variability of Antarctic ice volume and the carbon cycle is revealed throughout the Plio-Pleistocene , 2014, Nature Communications.
[16] B. Huntley,et al. Species distribution models indicate contrasting late‐Quaternary histories for Southern and Northern Hemisphere bird species , 2013 .
[17] L. Lourens,et al. Astronomical tuning of long pollen records reveals the dynamic history of montane biomes and lake levels in the tropical high Andes during the Quaternary , 2013 .
[18] Guy F. Midgley,et al. Carbon dioxide and the uneasy interactions of trees and savannah grasses , 2012, Philosophical Transactions of the Royal Society B: Biological Sciences.
[19] M. Collins,et al. A chronological framework for the British Quaternary based on Bithynia opercula , 2011, Nature.
[20] B. C. Hansen,et al. Pollen-based biome reconstructions for Latin America at 0, 6000 and 18 000 radiocarbon years ago , 2009 .
[21] B. Huntley,et al. Last Interglacial palaeovegetation, palaeoenvironments and chronology: a new record from Lago Grande di Monticchio, southern Italy , 2009 .
[22] P. Gibbard,et al. Global chronostratigraphical correlation table for the last 2.7 million years, version 2019 QI-500 , 2008, Quaternary International.
[23] T. Stocker,et al. High-resolution carbon dioxide concentration record 650,000–800,000 years before present , 2008, Nature.
[24] T. Stocker,et al. Orbital and millennial-scale features of atmospheric CH4 over the past 800,000 years , 2008, Nature.
[25] Richard H. W. Bradshaw,et al. Exploring climatic and biotic controls on Holocene vegetation change in Fennoscandia , 2008 .
[26] Kenji Kawamura,et al. The EDC3 chronology for the EPICA Dome C ice core , 2007 .
[27] Peter Kershaw,et al. A complete pollen record of the last 230 ka from Lynch's Crater, north-eastern Australia , 2007 .
[28] Jacques Laskar,et al. A long-term numerical solution for the insolation quantities of the Earth , 2004 .
[29] A. Rogers,et al. Rising atmospheric carbon dioxide: plants FACE the future. , 2004, Annual review of plant biology.
[30] Sandy P. Harrison,et al. Climate change and Arctic ecosystems: 1. Vegetation changes north of 55°N between the last glacial maximum, mid‐Holocene, and present , 2003 .
[31] F. I. Woodward,et al. The importance of low atmospheric CO2 and fire in promoting the spread of grasslands and savannas , 2003 .
[32] O. Urban. Physiological Impacts of Elevated CO2 Concentration Ranging from Molecular to Whole Plant Responses , 2003, Photosynthetica.
[33] J. Jouzel,et al. Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica , 1999, Nature.
[34] J. Kutzbach,et al. The Response of Northern Hemisphere Extratropical Climate and Vegetation to Orbitally Induced Changes in Insolation during the Last Interglaciation , 1995, Quaternary Research.
[35] P. Tzedakis. Vegetation Change through Glacial-Interglacial Cycles: A Long Pollen Sequence Perspective , 1994 .
[36] B. Huntley. Species-richness in north-temperate zone forests , 1993 .
[37] W. Cramer,et al. A global biome model based on plant physiology and dominance, soil properties and climate , 1992 .
[38] Gurmeet Singh,et al. Late Cainozoic History of Vegetation, Fire, Lake Levels and Climate, at Lake George, New South Wales, Australia , 1985 .
[39] A. Hall. Late Pleistocene deposits at Wing, Rutland. , 1980, Philosophical transactions of the Royal Society of London. Series B, Biological sciences.
[40] J. D. Hays,et al. Variations in the Earth ' s Orbit : Pacemaker of the Ice Ages Author ( s ) : , 2022 .
[41] P. Ciais,et al. Large inert carbon pool in the terrestrial biosphere during the Last Glacial Maximum , 2012 .
[42] Paul J. Valdes,et al. High-latitude climate sensitivity to ice-sheet forcing over the last 120 kyr , 2010 .
[43] O Hammer-Muntz,et al. PAST: paleontological statistics software package for education and data analysis version 2.09 , 2001 .