Hostname: page-component-586b7cd67f-r5fsc Total loading time: 0 Render date: 2024-11-25T22:28:59.308Z Has data issue: false hasContentIssue false

Constructing the past from late-Quaternary pollen data: Temporal resolution and a zoom lens space-time perspective

Published online by Cambridge University Press:  17 July 2017

Thompson Webb III*
Affiliation:
Department of Geological Sciences, Brown University, Providence, RI 02912-1846

Extract

Pollen analysis is an exercise in seeing. The ultimate goal is to see into the past, to send down a periscope and view what went on. The metaphor of the periscope is too limited, however; a video recorder from high in space with resolution in places up to 10 m is more encompassing of what is possible. The images that are retrieved can be of high or low resolution temporally, spatially, taxonomically, and numerically, and they can illustrate local to global changes in plant populations, vegetation, climate, human activity, fire frequency, and plant diseases over decades to millennia. Because each of these entities or phenomena varies spatially and temporally, records of data covering a breadth of scales in space and time are needed. To obtain the highest quality images about a specific phenomenon requires an understanding of the sensing system that accumulated the data. How does the periscope or video recorder work and what are the scaling characteristics of the images that it registers? These characteristics include breadth of coverage, sampling resolution, and sampling density in time, space, and taxonomy. Actualistic and taphonomic studies of Quaternary data covering a variety of temporal and spatial scales have helped provide this understanding, and temporal resolution is just one concern in these studies.

Type
Research Article
Copyright
Copyright © 1993 Paleontological Society 

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Adam, D. P. 1988. Palynology of two upper Quaternary cores from Clear Lake, Lake County, California. U. S. Geological Survey Professional Paper, 1363:186.Google Scholar
Allison, T. D., Moeller, R. E., and Davis, M. B. 1986. Pollen in laminated sediments provides evidence for a mid-Holocene forest pathogen attack. Ecology, 67:11011105.CrossRefGoogle Scholar
Banchoff, T. F. 1990. Beyond the Third Dimension. Scientific American Library, New York, 210 p.Google Scholar
Behrensmeyer, A. K., and Hook, R. W. 1992. Paleoenvironmental contexts and taphonomic modes, p. 7381. In Behrensmeyer, A. K., Damuth, J. D., DiMichele, W. A., Potts, R., Sues, H.-D. and Wing, S. L. (eds.), Terrestrial Ecosystems Through Time. University of Chicago Press, Chicago.Google Scholar
Bennett, K. D. 1992. Holocene history of forest trees on the Bruce Peninsula, southern Ontario. Canadian Journal of Botany, 70:618.CrossRefGoogle Scholar
Bernabo, J. C. 1981. Quantitative estimates of temperature changes over the last 2700 years in Michigan based on pollen data. Quaternary Research, 15:143159.Google Scholar
Betancourt, J. L., Van Devender, T. R., and Martin, P. S., eds. 1990. Packrat Middens: The Last 40,000 Years of Biotic Change. University of Arizona Press, Tucson,, 469 p.Google Scholar
Birks, H. H., Whiteside, M. C., Stark, D. M., and Bright, R. C. 1976. Recent paleolimnology of three lakes in northwestern Minnesota. Quaternary Research, 6:249272.CrossRefGoogle Scholar
Bradshaw, R. H. W. 1988. Spatially-precise studies of forest dynamics, p. 725751. In Huntley, B. and Webb, T. III (eds.), Vegetation History. Kluwer Academic Publishers, Dordrecht, The Netherlands.Google Scholar
Bradshaw, R. H. W., and Miller, N. G. 1988. Recent successional processes investigated by pollen analysis of closed-canopy forest sites. Vegetation, 76:4554.CrossRefGoogle Scholar
Bradshaw, R. H. W., and Webb, T. III. 1985. Relationships between contemporary pollen and vegetation data from Wisconsin and Michigan, USA. Ecology, 66:721737.Google Scholar
Brown, T. A., Nelson, D. E., Mathewes, R. W., and Vogel, J. S. 1989. Radiocarbon dating of pollen by accelerator mass spectrometry. Quaternary Research, 32:205212.CrossRefGoogle Scholar
Brubaker, L. B. 1975. Postglacial forest patterns associated with till and outwash in northcentral upper Michigan. Quaternary Research, 5:499527.Google Scholar
Members, Cohmap. 1988. Climate changes of the last 18,000 years: observations and model simulations. Science, 241:10431052.Google Scholar
Davis, M. B. 1969. Palynology and environmental history during the Quaternary period. American Scientist, 57:317332.Google Scholar
Davis, M. B., Brubaker, L. B., and Bieswenger, M. 1971. Pollen grains in lake sediments: pollen percentages in surface sediments from southern Michigan. Quaternary Research, 1:450467.CrossRefGoogle Scholar
Davis, M. B., Moeller, R. E., and Ford, J. 1984. Sediment focusing and pollen influx, p. 261293. In Haworth, E. Y. and Lund, J. W. G. (eds.), Lake sediments and environmental history. University of Leicester Press, Leicester.Google Scholar
Davis, M. B., Schwartz, M. W., and Woods, K. 1991. Detecting a species limit from pollen in sediments. Journal of Biogeography, 18:653668.Google Scholar
Davis, R. B. 1967. Pollen studies of near-surface sediments in Maine lakes, p. 143173. In Cushing, E. J. and Wright, H. E. (eds.), Quaternary Paleoecology. Yale University Press, New Haven.Google Scholar
Davis, R. B. 1974. Stratigraphic effects of tubificids in profundal lake sediments. Limnology and Oceanography, 19:466488.Google Scholar
Davis, R. B., Brewster, L. A., and Sutherland, J. 1969. Variation in pollen spectra within lakes (1). Pollen et Spores, 11:557571.Google Scholar
Dunwiddie, P. W. 1987. Macrofossil and pollen representation of coniferous trees in modern sediments from Washington. Ecology, 68:111.CrossRefGoogle Scholar
Faegri, K., and Iversen, J. 1989. Textbook of Pollen Analysis. (IV ed.) John Wiley and Sons, Chicester, 328 p.Google Scholar
Farley, M. B. 1989. Palynological facies fossils in nonmarine environments in the Paleogene of the Bighorn Basin. Palaios, 4:565573.Google Scholar
Foster, D. R., and Zebryk, T. M. 1993. Long-term vegetation dynamic and disturbance history of a Tsuga-dominated forest in New England. Ecology, in press.Google Scholar
Gajewski, K., Winkler, M. G., and Swain, A. M. 1985. Vegetation and fire history from three lakes with varved sediments in northwestern Wisconsin (U.S.A.). Review of Palaeobotany and Palynology, 44:277292.CrossRefGoogle Scholar
Gaudreau, D. C. 1986. Late-Quaternary vegetational history of the Northeast: paleoecological implications of topographic patterns in pollen distributions [Ph.D. dissertation]. Yale University, New Haven.Google Scholar
Gaudreau, D. C., Jackson, S. T., and Webb, T. III. 1989. The use of pollen data to record vegetational patterns in regions of moderate to high relief. Acta Botanica Nederlandica, 38:369390.Google Scholar
Graumlich, L. J., and Davis, M. B. 1993. Holocene variation in spatial scales of vegetation pattern in the upper Great Lakes. Ecology, 74:826839.Google Scholar
Grimm, E. C. 1988. Data analysis and display, p. 4376. In Huntley, B. and Webb, T. III (eds.), Vegetation History. Kluwer Academic Publishers, Dordrecht, The Netherlands.CrossRefGoogle Scholar
Heide, K. 1984. Holocene Pollen Stratigraphy from a lake and small hollow in North-Central Wisconsin, U.S.A. Palynology, 8:319.Google Scholar
Heusser, L. E., and King, J. E. 1988. North America with special emphasis on the development of the Pacific coastal forest and prairie/forest boundary prior to the Last Glacial Maximum, p. 193236. In Huntley, B. and Webb, T. III (eds.), Vegetation History. Kluwer Academic Publishers, Dordrecht, The Netherlands.Google Scholar
Hoogheimstra, H. 1984. Vegetational and Climatic History of the High Plain of Bogota, Colombia: A Continuous Record of the Last 3.5 Million Years. A.R. Gantner Verlag Kommanditgesellschaft, Vaduz, Germany, 368 p.Google Scholar
Howe, S. E., and Webb, T. III. 1977. Testing the statistical assumptions of paleoclimatic calibration functions, p. 152157. In Fifth Conference on Probability and Statistics. American Meteorological Society, Boston, MA.Google Scholar
Huntley, B., and Birks, H. J. B. 1983. An Atlas of Past and Present Pollen Maps for Europe: 0-13000 Years Ago. Cambridge University Press, Cambridge, 667 p.Google Scholar
Huntley, B., and Webb, T. III. 1988. Vegetation History. Kluwer Academic Publishers, Dordrecht, 811 p.Google Scholar
Huntley, B., and Webb, T. III. 1989. Migration: species' response to climatic variations caused by changes in the earth's orbit. Journal of Biogeography, 16:519.Google Scholar
Jackson, S. T. 1991. Pollen representation of vegetation patterns along an elevational gradient. Journal of Vegetation Science, 2:641653.Google Scholar
Jackson, S. T. 1993. Pollen and spores in Quaternary lake sediments as sensors of vegetation composition: theoretical models and empirical evidence. In Traverse, A. (eds.), Sedimentation of Organic Particles. Cambridge University Press, Cambridge, in press.Google Scholar
Jackson, S. T., and Whitehead, D. R. 1991. Holocene vegetation patterns in the Adirondack Mountains. Ecology, 72:641653.CrossRefGoogle Scholar
Jacobson, G. L. Jr. 1979. The paleoecology of white pine (Pinus strobus) in Minnesota. Journal of Ecology, 67:697726.Google Scholar
Jacobson, G. L. Jr. 1988. Ancient permanent plots: sampling in paleovegetational studies, p. 316. In Huntley, B. and Webb, T. III (eds.), Vegetation History. Kluwer Academic Publishers, Dordrecht.Google Scholar
Janssen, C. R. 1966. Recent pollen spectra from the deciduous and coniferous-deciduous forests of northeastern Minnesota: a study in pollen dispersal. Ecology, 37:804825.Google Scholar
Janssen, C. R. 1967. Stevens Pond: a postglacial pollen diagram from a small typha swamp in northeastern Minnesota interpreted from pollen indicators and surface samples. Ecological Monographs, 37:145172.CrossRefGoogle Scholar
Kershaw, A. P. 1988. Australasia, p. 237306. In Huntley, B. and Webb, T. III (eds.), Vegetation History. Kluwer Academic Publishers, Dordrecht, The Netherlands.Google Scholar
Knoerr, A. P., Webb, T. III, and Colthurst, T. W. 1991. Dynamic visualization of late Quaternary pollen data, p. 340343. In Keramidas, A. M. and Kaufman, S. M. (eds.), Computing Science and Statistics: Proceedings of the 23rd Symposium on the Interface. Interface Foundation of North America, Inc., Fairfax Station, VA.Google Scholar
Kutzbach, J. E., and Webb, T. III. 1991. Late Quaternary climatic and vegetational change in eastern North America: concepts, models, and dates, p. 175217. In Shane, L. C. K. and Cushing, E. J. (eds.), Quaternary Landscapes. University of Minnesota Press, Minneapolis.Google Scholar
Lotter, A. F., Eicher, U., Seigenthaler, U., and Birks, H. J. B. 1992. Late-glacial climatic oscillations as recorded in Swiss lake sediments. Journal of Quaternary Science, 7:187204.Google Scholar
Maher, L. J. 1972. Nomagrams for computing 0.95 confidence limits of pollen data. Review of Palaeobotany and Palynology, 13:8592.Google Scholar
Maher, L. J. 1981. Statistics for microfossil concentration measurements employing samples spiked with marker grains. Review of Palaeobotany and Palynology, 32:153191.Google Scholar
McDowell, P. F., Bartlein, P. J., and Webb, T. III. 1990. Long-term environmental change, p. 143162. In Turner Ii, B. J., Clark, W. C., Kates, R. W., Richards, J. F., Matthews, J. T. and Meyer, W. B. (eds.), The Earth as Transformed by Human Action. Cambridge University Press, New York.Google Scholar
Olsson, I. U. 1986. Radiometric Dating, Berglund, B. E. (eds.), Handbook of Holocene Palaeoecology and Palaeohydrology. John Wiley and Sons, Chicester.Google Scholar
Peglar, S. M., Fritz, S. C., Alapieti, T., Saarnisto, M., and Birks, H. J. B. 1984. Composition and formation of laminated sediments in Diss Mere, Norfolk, England. Boreas, 13:1328.Google Scholar
Pilcher, J. R. 1993. Radiocarbon dating and the palynologist: a realistic approach to precision and accuracy, p. 2332. In Chambers, F. M. (eds.), Climate Change and Human Impact on the Landscape. Chapman and Hall, London.Google Scholar
Prentice, I. C. 1985. Pollen representation, source area, and basin size: toward a unified theory of pollen analysis. Quaternary Research, 23:7686.Google Scholar
Prentice, I. C. 1988. Records of vegetation in time and space: the principles of pollen analysis, p. 603632. In Huntley, B. and Webb, T. III (eds.), Vegetation History. Kluwer Academic Publishers, Dordrecht.Google Scholar
Saarnisto, M. 1986. Annually laminated lake sediments, p. 343370. In Berglund, B. E. (eds.), Handbook of Holocene Palaeoecology and Palaeohydrology. John Wiley and Sons, Chichester.Google Scholar
Simmons, I. G. 1993. Vegetation change during the Mesolithic in the British Isles: some amplifications, p. 109118. In Chambers, F. M. (eds.), Climate Change and Human Impact on the Landscape. Chapman and Hall, London.Google Scholar
Smith, A. G., and Pilcher, J. R. 1973. Radiocarbon dates and vegetational history of the British Isles. New Phytologist, 72:903914.Google Scholar
Solomon, A. M., and Webb, T. III. 1985. Computer-aided reconstruction of late-Quaternary landscape dynamics. Annual Review of Ecology and Systematics, 16:6384.Google Scholar
Stuiver, M. 1967. Origin and extent of atmospheric C14 variations during the past 10,000 years, p. 2740. In Anonymous (ed.), Radio-active dating and methods of low-level counting. International Atomic Energy Agency, Vienna.Google Scholar
Sugita, S. 1993. A model of pollen source area for an entire lake surface. Quaternary Research, 39:239244.Google Scholar
Tornqvist, T.E., De Jong, A.F.M., Oosterbaan, W.A., and Van Der Borg, K. 1992. Accurate dating of organic deposits by AMS 14C measurements of macrofossils. Radiocarbon, 34:566577.CrossRefGoogle Scholar
Turner, J., and Peglar, S. M. 1988. Temporally-precise studies of vegetation history, p. 753777. In Huntley, B. and Webb, T. III (eds.), Vegetation History. Kluwer Academic Publishers, Dordrecht.Google Scholar
Van Zant, K. L., Webb, T. III, Peterson, G. M., and Baker, R. G. 1979. Increased Cannabis/Humulus pollen, an indicator of European agriculture in Iowa. Palynology, 3:227233.Google Scholar
Watts, W. A. 1988. Europe, p. 155192. In Huntley, B. and Webb, T. III (eds.), Vegetation History. Kluwer Academic Publishers, Dordrecht.Google Scholar
Watts, W. A., and Winter, T. C. 1966. Plant macrofossils from Kirchner Marsh, Minnesota – a paleoecological study. Geological Society of America Bulletin, 77:13391360.Google Scholar
Webb, R. S., and Webb, T. III. 1988. Rates of sediment accumulation in pollen cores from small lakes and mires of eastern North America. Quaternary Research, 30:284297.CrossRefGoogle Scholar
Webb, T. III. 1974a. Corresponding distributions of modern pollen and vegetation in lower Michigan. Ecology, 55:1728.CrossRefGoogle Scholar
Webb, T. III. 1974b. A vegetational history from northern Wisconsin: evidence from modern and fossil pollen. American Midland Naturalist, 92:1234.Google Scholar
Webb, T. III. 1981. 11,000 years of vegetational change in eastern North America. Bioscience, 31:501506.Google Scholar
Webb, T. III. 1982. Temporal resolution in Holocene pollen data. Third North American Paleontological Convention, Proceedings, 2:569572.Google Scholar
Webb, T. III. 1988. Eastern North America, p. 385414. In Huntley, B. and Webb, T. III (eds.), Vegetation History. Kluwer Academic Publishers, Dordrecht, The Netherlands.Google Scholar
Webb, T. III, Richard, P. J. H., and Mott, R. J. 1983. A mapped history of Holocene vegetation in southern Quebec. Syllogeus, 49:273336.Google Scholar
Woods, K. D., and Davis, M. B. 1989. Paleoecology of range limits: beech in the upper peninsula of Michigan. Ecology, 70:681696.Google Scholar
Wright, H. E. Jr., Kutzbach, J. E., Webb, T. III, Ruddiman, W. F., Street-Perrott, F. A., and Barrtlein, P. J. (eds.). 1993. Global Climates Since the Last Glacial Maximum. University of Minnesota Press, Minneapolis, in press.Google Scholar