Climatic response surfaces from pollen data for some eastern North American taxa

Ecological response surfaces are nonlinear functions describing the way in which the abundances of taxa depend on the joint effects of two or more environmental variables. Continental-scale patterns in the relative abundances of plant taxa are dominated by the effects of macroclimate on the competitive balance among taxa. Pollen analyses record such regional variations for major vegetation components. Empirical ecological response surfaces were derived from high-resolution climate models to yield testable reconstructions of vegeta- eastern North America. The surfaces were obtained by second- or third-degree polynomial regression on two predictor variables, mean July temperature and annual precipitation, with various nonlinear transformations of variables to allow flexibility of shape. Response surface analysis consists of a remapping of abundance patterns from geographic space into climate space, and complements efforts to explain distri- butions in terms of biological processes. Each fitted surface is unique. The surfaces focus attention on the climatic location of range limits and optima, and on less obvious phenomena such as the spatial pattern in the relative sensitivity of different taxa to spatial variation in the climatic variables. Given certain assump- tions, response surfaces based directly on pollen data may be used collectively in a global nonlinear method for estimating past climates from postglacial pollen data. Such response surfaces may also be coupled to palaeoclimatic simulations from high-resolution climate models to yield testable reconstructions of vegeta- tional history.

[1]  B. Maher,et al.  Formation of ultrafine-grained magnetite in soils , 1988, Nature.

[2]  G. Kukla,et al.  Pleistocene climates in China dated by magnetic susceptibility , 1988 .

[3]  K. Pye,et al.  Stratigraphy, geochemistry, and thermoluminescence ages of lower Mississippi Valley loess , 1988 .

[4]  U. Schwertmann Occurrence and Formation of Iron Oxides in Various Pedoenvironments , 1988 .

[5]  J. D. Hays,et al.  Age Dating and the Orbital Theory of the Ice Ages: Development of a High-Resolution 0 to 300,000-Year Chronostratigraphy , 1987, Quaternary Research.

[6]  H. E. Wright Synthesis; The land south of the ice sheets , 1987 .

[7]  K. Pye Aeolian dust and dust deposits , 1987 .

[8]  Hojatollah Vali,et al.  Fossil bacterial magnetite in deep-sea sediments from the South Atlantic Ocean , 1986, Nature.

[9]  B. Maher Characterisation of soils by mineralmagnetic measurements , 1986 .

[10]  S. Robinson The late Pleistocene palaeoclimatic record of North Atlantic deep-sea sediments revealed by mineral-magnetic measurements , 1986 .

[11]  D. Fullerton,et al.  Introduction to quaternary glaciations in the United States of America , 1986 .

[12]  R. Berner,et al.  Pyrite formation in euxinic and semi-euxinic sediments , 1985 .

[13]  T. Webb,,et al.  Relationships between Contemporary Pollen and Vegetation Data from Wisconsin and Michigan, USA , 1985 .

[14]  M. Kaminsky,et al.  Auger spectroscopy analysis of magnesian calcite overgrowths precipitated from seawater and solutions of similar composition , 1985 .

[15]  B. Huntley,et al.  Atlas of Mapped Distributions of Dominance and Modern Pollen Percentages for Important Tree Taxa of Eastern North America. , 1985 .

[16]  J. Kutzbach,et al.  Simulation of the climate of 18,000 years BP: Results for the North American/North Atlantic/European sector and comparison with the geologic record of North America , 1985 .

[17]  J. Overpeck,et al.  Quantitative Interpretation of Fossil Pollen Spectra: Dissimilarity Coefficients and the Method of Modern Analogs , 1985, Quaternary Research.

[18]  I. Prentice Pollen Representation, Source Area, and Basin Size: Toward a Unified Theory of Pollen Analysis , 1985, Quaternary Research.

[19]  Patrick J. Bartlein,et al.  Holocene Climatic Change in the Northern Midwest: Pollen-Derived Estimates , 1984, Quaternary Research.

[20]  W. O'reilly Rock and Mineral Magnetism , 1984 .

[21]  J. Kutzbach,et al.  Sensitivity of late-glacial and Holocene climates to the combined effects of orbital parameter changes and lower boundary condition changes: , 1984 .

[22]  B. Huntley,et al.  An Atlas of Past and Present Pollen Maps for Europe , 1984 .

[23]  J. H. Wright,et al.  Late-Quaternary Environments of the United States , 1983 .

[24]  R. D. Cook,et al.  Transformations and Influential Cases in Regression , 1983 .

[25]  Ronald P. Neilson,et al.  Biogeography of two southwest American oaks in relation to atmospheric dynamics , 1983 .

[26]  I. Prentice,et al.  Postglacial climatic change , 1983 .

[27]  A. Newman The specific surface of soils determined by water sorption , 1983 .

[28]  Hugh G. Gauch,et al.  Multivariate analysis in community ecology , 1984 .

[29]  J. M. Ryan,et al.  Linear Transformations of Polynomial Regression Models , 1982 .

[30]  Subir K. Banerjee,et al.  A preliminary magnetic study of soil samples from west-central Minnesota , 1982 .

[31]  H. Delcourt,et al.  Dynamic plant ecology: the spectrum of vegetational change in space and time , 1982 .

[32]  J. Andrews Modern pollen deposition and Holocene paleotemperature reconstructions, central northern Canada , 1981 .

[33]  J. Kutzbach,et al.  Monsoon Climate of the Early Holocene: Climate Experiment with the Earth's Orbital Parameters for 9000 Years Ago , 1981, Science.

[34]  T. Webb,,et al.  Estimating plant abundances from pollen percentages: The use of regression analysis , 1981 .

[35]  T. Hassard,et al.  Applied Linear Regression , 2005 .

[36]  E. Box Macroclimate and Plant Forms , 1981, Tasks for Vegetation Science.

[37]  H. E. Wright Surge Moraines of the Klutlan Glacier, Yukon Territory, Canada: Origin, Wastage, Vegetation Succession, Lake Development, and Application to the Late-Glacial of Minnesota , 1980, Quaternary Research.

[38]  R. Whittaker Direct Gradient Analysis , 1978 .

[39]  Sidney Addelman,et al.  trans-Dimethanolbis(1,1,1-trifluoro-5,5-dimethylhexane-2,4-dionato)zinc(II) , 2008, Acta crystallographica. Section E, Structure reports online.

[40]  T. Webb,,et al.  Changing Patterns in the Holocene Pollen Record of Northeastern North America: A Mapped Summary , 1977, Quaternary Research.

[41]  C. E. Mullins,et al.  MAGNETIC SUSCEPTIBILITY OF THE SOIL AND ITS SIGNIFICANCE IN SOIL SCIENCE – A REVIEW , 1977 .

[42]  Neil Wrigley,et al.  Probability surface mapping: a new approach to trend surface mapping , 1977 .

[43]  H. Soffel Pseudo-single-domain effects and single-domain multidomain transition in natural pyrrhotite deduced from domain structure observations , 1976 .

[44]  R Mead,et al.  A review of response surface methodology from a biometric viewpoint. , 1975, Biometrics.

[45]  C. Pigott EXPERIMENTAL STUDIES ON THE INFLUENCE OF CLIMATE ON THE GEOGRAPHICAL DISTRIBUTION OF PLANTS , 1975 .

[46]  Hugh G. Gauch,et al.  Fitting the Gaussian Curve to Ecological Data , 1974 .

[47]  Subir K. Banerjee,et al.  The physical principles of rock magnetism , 1974 .

[48]  J. Lindsey Fitting Response Surfaces with Power Transformations , 1972 .

[49]  J. R. Wallis,et al.  Some ecological consequences of a computer model of forest growth , 1972 .

[50]  Y. Miyahara Impurity Effects on the Transition Temperature of Magnetite , 1972 .

[51]  W. Reese,et al.  Atlas of United States Trees. Volume 1. Conifers and Important Hardwoods , 1972 .

[52]  R. Mead A NOTE ON THE USE AND MISUSE OF REGRESSION MODELS IN ECOLOGY , 1971 .

[53]  E. L. Little Atlas of United States trees. , 1971 .

[54]  E. L. Little Conifers and important hardwoods , 1971 .

[55]  David R. Cox The analysis of binary data , 1970 .

[56]  Peter Mazur,et al.  Freezing Injury in Plants , 1969 .

[57]  G. A. Yarranton Plant Ecology: A Unifying Model , 1969 .

[58]  J. McAndrews POLLEN EVIDENCE FOR THE PROTOHISTORIC DEVELOPMENT OF THE "BIG WOODS" IN MINNESOTA (U.S.A.) , 1968 .

[59]  J. Mather,et al.  THE ROLE OF CLIMATE IN THE DISTRIBUTION OF VEGETATION , 1968 .

[60]  J. McAndrews Pollen analysis and vegetational history of the Itasca region, Minnesota , 1967 .

[61]  T. C. Winter,et al.  Plant Macrofossils from Kirchner Marsh, Minnesota—A Paleoecological Study , 1966 .

[62]  D. Cox,et al.  An Analysis of Transformations , 1964 .

[63]  T. C. Winter,et al.  Two Pollen Diagrams from Southeastern Minnesota: Problems in the Regional Late-Glacial and Postglacial Vegetational History , 1963 .

[64]  R. Whittaker Vegetation of the Siskiyou Mountains, Oregon and California , 1960 .

[65]  E. L. Borgne Influence du feu sur les proprietes magnetiques du sol et sur celles du schiste et du granite , 1960 .

[66]  Robert H. Whittaker,et al.  Vegetation of the Great Smoky Mountains , 1956 .

[67]  E. L. Borgne Susceptibilité magnétique anormale du sol superficiel , 1955 .

[68]  D. C. Peattie,et al.  A Natural History of Trees of Eastern and Central North America. , 1952 .

[69]  F. Morin Magnetic Susceptibility of αFe 2 O 3 and αFe 2 O 3 with Added Titanium , 1950 .

[70]  F. J. Anscombe,et al.  THE TRANSFORMATION OF POISSON, BINOMIAL AND NEGATIVE-BINOMIAL DATA , 1948 .

[71]  T. Shaw,et al.  The Specific Surface and Density of Some Soils and Their Colloids1 , 1938 .