Natural, potential and actual vegetation in North America

The potential natural vegetation (PNV) concept has parallel applications in Europe and North America. Paleoecological studies in parts of North America provide records of vegetation patterns and dynamics under little or no human disturbance. Something resembling PNV emerges at millennial temporal scales and at regional to subcontinental spatial scales. However, at finer spatial and temporal scales, actual vegetation often displays properties of inertia, contingency and hysteresis, most frequently because of climatic variability across multiple timescales and the episodic nature of disturbance and establishment. Thus, in the absence of human disturbance, the actual vegetation that develops at a site may not resemble a particular PNV ideal, but could instead represent one of any number of potential outcomes constrained by historically contingent processes. PNV may best be viewed as an artificial construct, with utility in some settings. Its utility may diminish and even be detrimental in a rapidly changing environment.

[1]  S. T. Jackson Conservation and Resource Management in a Changing World: Extending Historical Range of Variation Beyond the Baseline , 2012 .

[2]  Jacquelyn L. Gill,et al.  Climatic and megaherbivory controls on late-glacial vegetation dynamics: a new, high-resolution, multi-proxy record from Silver Lake, Ohio , 2012 .

[3]  M. Clifford,et al.  Multi-decadal drought and amplified moisture variability drove rapid forest community change in a humid region. , 2012, Ecology.

[4]  K. Gajewski,et al.  Synchronous environmental and cultural change in the prehistory of the northeastern United States , 2010, Proceedings of the National Academy of Sciences.

[5]  M. Araújo,et al.  The concept of potential natural vegetation: an epitaph? , 2010 .

[6]  W. Reiners,et al.  Philosophical Foundations for the Practices of Ecology , 2009 .

[7]  John W. Williams,et al.  Pleistocene Megafaunal Collapse, Novel Plant Communities, and Enhanced Fire Regimes in North America , 2009, Science.

[8]  Julio L. Betancourt,et al.  Ecology and the ratchet of events: Climate variability, niche dimensions, and species distributions , 2009, Proceedings of the National Academy of Sciences.

[9]  B. Shuman,et al.  Woodland-to-forest transition during prolonged drought in Minnesota after ca. AD 1300. , 2009, Ecology.

[10]  J. Donnelly,et al.  Abrupt climate change as an important agent of ecological change in the Northeast U.S. throughout the past 15,000 years , 2009 .

[11]  Randy Calcote,et al.  Response of vegetation and fire to Little Ice Age climate change: regional continuity and landscape heterogeneity , 2007, Landscape Ecology.

[12]  S. T. Jackson Vegetation, environment, and time: The origination and termination of ecosystems , 2006 .

[13]  J. Betancourt,et al.  Role of multidecadal climate variability in a range extension of pinyon pine. , 2006, Ecology.

[14]  R. Mitchell,et al.  Conservation management of Pinus palustris ecosystems from a landscape perspective , 2006 .

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

[16]  Julio L. Betancourt,et al.  INFLUENCE OF LANDSCAPE STRUCTURE AND CLIMATE VARIABILITY ON A LATE HOLOCENE PLANT MIGRATION , 2003 .

[17]  S. Pyne,et al.  Fire, Native Peoples, and the Natural Landscape , 2003 .

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

[19]  P. Bartlein,et al.  Variations in fire frequency and climate over the past 17 000 yr in central Yellowstone National Park , 2000 .

[20]  H. Takahara,et al.  PATCHY INVASION AND THE ORIGIN OF A HEMLOCK–HARDWOODS FOREST MOSAIC , 1998 .

[21]  T. Swetnam,et al.  Mesoscale Disturbance and Ecological Response to Decadal Climatic Variability in the American Southwest , 1998 .

[22]  Werner Härdtle,et al.  On the theoretical concept of the potential natural vegetation and proposals for an up-to-date modification , 1995, Folia Geobotanica.

[23]  P. White,et al.  On the existence of ecological communities , 1994 .

[24]  C. Whitlock Postglacial Vegetation and Climate of Grand Teton and Southern Yellowstone National Parks , 1993 .

[25]  T. Webb, Is vegetation in equilibrium with climate? How to interpret late-Quaternary pollen data , 1986, Vegetatio.

[26]  T. Allen,et al.  Will similar forests develop on similar sites , 1985 .

[27]  T. Webb,,et al.  The Past 11,000 Years of Vegetational Change in Eastern North America , 1981 .

[28]  R Daubenmire,et al.  Vegetation: identification of typal communities. , 1966, Science.

[29]  R. Daubenmire,et al.  Forest Vegetation of Northern Idaho and Adjacent Washington, and Its Bearing on Concepts of Vegetation Classification , 1952 .

[30]  H. Chapman Is the Longleaf Type a Climax? , 1932, Fire Ecology.

[31]  Henry C. Cowles,et al.  The Physiographic Ecology of Chicago and Vicinity; A Study of the Origin, Development, and Classification of Plant Societies , 1901, Botanical Gazette.

[32]  J. Hiers,et al.  Silviculture that sustains : the nexus between silviculture, frequent prescribed fire, and conservation of biodiversity in longleaf pine forests of the southeastern United States , 2006 .

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

[34]  John M. Crowley,et al.  Küchler, A.Q. Potential Natural Vegetation of the Conterminous United States. American Geographical Society Special Pub. No. 36. New York, American Geographical Society, 1964. Carte accompagnée d’un manuel : illustrations, bibliographie. , 1964 .

[35]  H. Cowles The physiographic ecology of Chicago and vicinity , 1901 .