Novel climates, no‐analog communities, and ecological surprises

No-analog communities (communities that are compositionally unlike any found today) occurred frequently in the past and will develop in the greenhouse world of the future. The well documented no-analog plant communities of late-glacial North America are closely linked to “novel” climates also lacking modern analogs, characterized by high seasonality of temperature. In climate simulations for the Intergovernmental Panel on Climate Change A2 and B1 emission scenarios, novel climates arise by 2100 AD, primarily in tropical and subtropical regions. These future novel climates are warmer than any present climates globally, with spatially variable shifts in precipitation, and increase the risk of species reshuffling into future no-analog communities and other ecological surprises. Most ecological models are at least partially parameterized from modern observations and so may fail to accurately predict ecological responses to these novel climates. There is an urgent need to test the robustness of ecological mode...

[1]  Martijn Gough Climate change , 2009, Canadian Medical Association Journal.

[2]  Vincent R. Gray Climate Change 2007: The Physical Science Basis Summary for Policymakers , 2007 .

[3]  Simon Brewer,et al.  Dominant factors controlling glacial and interglacial variations in the treeline elevation in tropical Africa , 2007, Proceedings of the National Academy of Sciences.

[4]  John E. Kutzbach,et al.  Projected distributions of novel and disappearing climates by 2100 AD , 2006, Proceedings of the National Academy of Sciences.

[5]  M. Araújo,et al.  Five (or so) challenges for species distribution modelling , 2006 .

[6]  Emmanuel S. Gritti,et al.  Towards European climate risk surfaces: the extent and distribution of analogous and non-analogous climates 1931–2100 , 2006 .

[7]  A. Gillespie,et al.  The Quaternary Period in the United States , 2006 .

[8]  D. Richardson,et al.  Novel ecosystems: theoretical and management aspects of the new ecological world order , 2006 .

[9]  T. Stocker,et al.  Atmospheric Methane and Nitrous Oxide of the Late Pleistocene from Antarctic Ice Cores , 2005, Science.

[10]  T. Stocker,et al.  Stable Carbon Cycle–Climate Relationship During the Late Pleistocene , 2005, Science.

[11]  Scott L Wing,et al.  Transient Floral Change and Rapid Global Warming at the Paleocene-Eocene Boundary , 2005, Science.

[12]  R. Graham Quaternary Mammal Communities: Relevance of the Individualistic Response and Non-Analogue Faunas , 2005 .

[13]  K. Gajewski,et al.  Modern pollen data from North America and Greenland for multi-scale paleoenvironmental applications , 2005 .

[14]  James S. Clark,et al.  MOLECULAR INDICATORS OF TREE MIGRATION CAPACITY UNDER RAPID CLIMATE CHANGE , 2005 .

[15]  M. Edwards,et al.  STRUCTURALLY NOVEL BIOMES: A RESPONSE TO PAST WARMING IN BERINGIA , 2005 .

[16]  Julie R. Etterson,et al.  EVOLUTIONARY RESPONSES TO CHANGING CLIMATE , 2005 .

[17]  M. Sykes,et al.  Climate change threats to plant diversity in Europe. , 2005, Proceedings of the National Academy of Sciences of the United States of America.

[18]  D. Burney,et al.  LANDSCAPE PALEOECOLOGY AND MEGAFAUNAL EXTINCTION IN SOUTHEASTERN NEW YORK STATE , 2005 .

[19]  A. Peterson,et al.  Ecological niches as stable distributional constraints on mammal species, with implications for Pleistocene extinctions and climate change projections for biodiversity , 2004 .

[20]  Mark W. Schwartz,et al.  How fast and far might tree species migrate in the eastern United States due to climate change , 2004 .

[21]  Stephen T. Jackson,et al.  MODERN ANALOGS IN QUATERNARY PALEOECOLOGY: Here Today, Gone Yesterday, Gone Tomorrow? , 2004 .

[22]  P. Bartlein,et al.  LATE‐QUATERNARY VEGETATION DYNAMICS IN NORTH AMERICA: SCALING FROM TAXA TO BIOMES , 2004 .

[23]  A. Kitamura Effects of seasonality, forced by orbital-insolation cycles, on offshore molluscan faunal change during rapid warming in the Sea of Japan , 2004 .

[24]  O. Phillips,et al.  Extinction risk from climate change , 2004, Nature.

[25]  J. Whitmore North American and Greenland modern pollen data for multi-scale paleoecological and paleoclimatic applications , 2004 .

[26]  S. Milton 'Emerging ecosystems' - a washing-stone for ecologists, economists and sociologists? , 2003 .

[27]  J. Overpeck,et al.  Terrestrial Biosphere Dynamics in the Climate System: Past and Future , 2003 .

[28]  John W. Williams,et al.  Climatically forced vegetation dynamics in eastern North America during the late Quaternary Period , 2003 .

[29]  G. Jacobson,et al.  Late-Quaternary vegetation history of the eastern United States , 2003 .

[30]  Keith Alverson,et al.  Paleoclimate, global change and the future , 2003 .

[31]  O. Hoegh‐Guldberg,et al.  Ecological responses to recent climate change , 2002, Nature.

[32]  F. Woodward,et al.  Conservation of Biodiversity in a Changing Climate , 2002, Conservation biology : the journal of the Society for Conservation Biology.

[33]  John W. Williams,et al.  DISSIMILARITY ANALYSES OF LATE-QUATERNARY VEGETATION AND CLIMATE IN EASTERN NORTH AMERICA , 2001 .

[34]  Julie R. Etterson,et al.  Constraint to Adaptive Evolution in Response to Global Warming , 2001, Science.

[35]  S. Carpenter,et al.  Ecological forecasts: an emerging imperative. , 2001, Science.

[36]  R. Shaw,et al.  Range shifts and adaptive responses to Quaternary climate change. , 2001, Science.

[37]  F. Woodward,et al.  Global response of terrestrial ecosystem structure and function to CO2 and climate change: results from six dynamic global vegetation models , 2001 .

[38]  Michael J. Mac,et al.  Status and trends of the nation's biological resources , 2001 .

[39]  P. Valdes,et al.  Sensitivity of the Northern Hemisphere climate of the Last Glacial Maximum to sea surface temperatures , 2001 .

[40]  J. R. Coleman,et al.  Effects of low atmospheric CO(2) on plants: more than a thing of the past. , 2001, Trends in plant science.

[41]  J. Overpeck,et al.  Responses of plant populations and communities to environmental changes of the late Quaternary , 2000, Paleobiology.

[42]  K. Willis,et al.  The Full-Glacial Forests of Central and Southeastern Europe , 2000, Quaternary Research.

[43]  J. Southon,et al.  First accelerator mass spectrometry 14C dates documenting contemporaneity of nonanalog species in late Pleistocene mammal communities , 1999 .

[44]  Alan C. Mix,et al.  Foraminiferal faunal estimates of paleotemperature: Circumventing the No‐analog problem yields cool Ice Age tropics , 1999 .

[45]  James P. Kennett,et al.  Biotic response to late Quaternary rapid climate switches in Santa Barbara Basin: Ecological and evolutionary implications , 1999 .

[46]  Robert S. Thompson,et al.  Atlas of relations between climatic parameters and distributions of important trees and shrubs in North America , 1999 .

[47]  Robert S. Webb,et al.  Mechanisms of global climate change at millennial time scales , 1999 .

[48]  Sandy P. Harrison,et al.  Climate and biome simulations for the past 21 , 1998 .

[49]  H. Gregory McDonald,et al.  Spatial Response of Mammals to Late Quaternary Environmental Fluctuations , 1996, Science.

[50]  H. Delcourt,et al.  Postglacial Rise and Decline of Ostrya virginiana (Mill.) K. Koch and Carpinus caroliniana Walt. In Eastern North America: Predictable Responses of Forest Species to Cyclic Changes in Seasonality of Climates , 1994 .

[51]  J. Overpeck,et al.  Mapping eastern North American vegetation change of the past 18 ka: No-analogs and the future , 1992 .

[52]  Patrick J. Bartlein,et al.  VEGETATION AND CLIMATE CHANGE IN EASTERN NORTH AMERICA SINCE THE LAST GLACIAL MAXIMUM , 1991 .

[53]  M. Davis Packrat middens: The last 40,000 years of biotic change , 1991 .

[54]  André Berger,et al.  Insolation values for the climate of the last 10 , 1991 .

[55]  Brian Huntley,et al.  Dissimilarity Mapping Between Fossil and Contemporary Pollen Spectra in Europe for the Past 13,000 Years , 1990, Quaternary Research.

[56]  Brian Huntley,et al.  Climatic control of the distribution and abundance of beech (Fagus L.) in Europe and North America. , 1989 .

[57]  K. Gajewski,et al.  Modern Analogues of Late-Quaternary Pollen Spectra from the Western Interior of North America , 1989 .

[58]  N. Owen‐Smith,et al.  Pleistocene extinctions: the pivotal role of megaherbivores , 1987, Paleobiology.

[59]  M. B. Davis,et al.  Quaternary history and the stability of forest communities , 1981 .

[60]  A. Morgan,et al.  FAUNAL ASSEMBLAGES AND DISTRIBUTIONAL SHIFTS OF COLEOPTERA DURING THE LATE PLEISTOCENE IN CANADA AND THE NORTHERN UNITED STATES , 1980, The Canadian Entomologist.

[61]  A. Sakai,et al.  Freezing Resistance of Trees in North America with Reference to Tree Regions , 1973 .

[62]  H. Gleason The individualistic concept of the plant association , 1926 .

[63]  U. S. E. N. Wed MODELING DYNAMIC VEGETATION RESPONSE TO RAPID CLIMATE CHANGE USING BIOCLIMATIC CLASSIFICATION , 2022 .

[64]  M. Bush,et al.  Amazonian paleoecological histories : one hill , three watersheds , 2022 .