Hostname: page-component-78c5997874-4rdpn Total loading time: 0 Render date: 2024-11-06T13:21:03.377Z Has data issue: false hasContentIssue false

Did Ground Cover Change Over Geologic Time?

Published online by Cambridge University Press:  21 July 2017

Ben A. LePage
Affiliation:
Department of Earth and Environmental Science, University of Pennsylvania, Philadelphia, PA, 19104–6316 USA
Hermann W. Pfefferkorn
Affiliation:
Department of Earth and Environmental Science, University of Pennsylvania, Philadelphia, PA, 19104–6316 USA
Get access

Extract

When one hears the term “ground cover,” one immediately thinks of “grasses.” This perception is so deep-seated that paleobotanists even have been overheard to proclaim that “there was no ground cover before grasses.” Today grasses are so predominant in many environments that this perception is perpetuated easily. On the other hand, it is difficult to imagine the absence or lack of ground cover prior to the mid-Tertiary. We tested the hypothesis that different forms of ground cover existed in the past against examples from the Recent and the fossil record (Table 1). The Recent data were obtained from a large number of sources including those in the ecological, horticultural, and microbiological literature. Other data were derived from our knowledge of Precambrian life, sedimentology and paleosols, and the plant fossil record, especially in situ floras and fossil “monocultures.” Some of the data are original observations, but many others are from the literature. A detailed account of these results will be presented elsewhere (Pfefferkorn and LePage, in preparation).

Type
Research Article
Copyright
Copyright © 2000 by the 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

Alleman, V., Pfefferkorn, H.W., and Erwin, D.M. 1995. Los contextos paleoecológicos variados de las floras Carboníferas de Paracas (Ica, Perú). Boletin de la Sociedad Geologica del Peru, 84:3742.Google Scholar
Andrews, H.N., Kasper, A.E., Forbes, W.H., Gensel, P.G., and Chaloner, W.G. 1977. Early Devonian flora of the Trout Valley Formation of northern Maine. Review of Paleobotany and Palynology, 23:255285.Google Scholar
Basinger, J.F. 1991. The fossil forests of the Buchanan Lake Formation (early Tertiary), Axel Heiberg Island, Canadian Arctic Archipelago: preliminary floristics and paleoclimate. Geological Survey of Canada Bulletin, 403:3965.Google Scholar
Basinger, J.F., Greenwood, D.G., and Sweda, T., 1994. Early Tertiary vegetation of Arctic Canada and its relevance to paleoclimatic interpretation. NATO ASI Series, 127:175198.Google Scholar
Beeunas, M.A., and Knauth, L.P. 1985. Preserved stable isotopic signature of subserial diagenesis in the 1.2-b.y. Mescal Limestone, central Arizona: implications for the timing and development of terrestrial plant cover. Geological Society of America Bulletin, 96:737745.Google Scholar
Cai, S., Ouyang, S., Wang, Y., Fang, Z., Rong, J., Geng, L., and Li, X. 1996. An Early Silurian vascular plant. Nature, 379:592.Google Scholar
Campbell, S.E. 1979. Soil stabilization by a prokaryotic desert crust: implications for Precambrian land biota. Origins of Life, 9:335348.Google Scholar
Collinson, M.E., and Scott, A.C. 1987. Factors controlling the organization and evolution of ancient plant communities, p. 399420. In Gee, J.H.R. and Giller, P.S. (eds.), Organization of past communities: past and present. Blackwell Scientific Publications, Oxford.Google Scholar
Cotter, E. 1978. The evolution of fluvial style, with special reference to the central Appalachian Paleozoic. Canadian Society of Petroleum Geologists Memoir, 5:361384.Google Scholar
Edwards, D. 1996. New insights into early land ecosystems: a glimpse of a Lilliputian world. Review of Paleobotany and Palynology, 90:159174.Google Scholar
Edwards, D., and Fanning, U. 1985. Evolution and environment in the late Silurian-early Devonian: the rise of the pteridophytes. Philosophical Transactions of the Royal Society of London B, 309:147165.Google Scholar
Edwards, D., Davies, K.L., and Axe, L. 1992. A vascular conducting strand in the land plant Cooksonia . Nature, 357:683685.Google Scholar
Fisher, A.G. 1965. Fossils, early life and atmospheric history. Proceedings of the National Academy of Sciences, USA, 53:12051213.Google Scholar
Folk, R.L., Roberts, H.H., and Moore, C.H. 1973. Black phytokarst from Hell, Cayman Islands, British West Indies. Geological Society of America Bulletin, 84:23512360.Google Scholar
Friedmann, E.I. 1980. Endolithic microbial life in hot and cold deserts. Origins of Life, 10:223235.Google Scholar
Friedmann, E.I. 1982. Endolithic microorganisms in the Antarctic cold desert. Science, 215:10451053.CrossRefGoogle ScholarPubMed
Gastaldo, R.A., Dimichele, W. A., and Pfefferkorn, H.W. 1995. Taphonomic and sedimentologic characterization of roof-shale floras. Geological Society of America, Memoir, 185:341352.Google Scholar
Gastaldo, R.A., Riegel, W., Püttmann, W., Linnemann, U.G., and Zetter, R. 1998. A multidisciplinary approach to reconstruct the late Oligocene vegetation in central Europe. Review of Paleobotany and Palynology, 101:7194.CrossRefGoogle Scholar
Gensel, P.G., and Andrews, H.N. 1984. Plant life in the Devonian. Praeger, New York.Google Scholar
Golubic, S., and Campbell, S.E. 1979. Analogous microbial forms in recent subaerial habitats in Precambrian chert: Gloeothece coerulea Geitler and Eosynechococcus moorei Hofmann. Precambrian Research, 8:201217.Google Scholar
Grand'Eury, M.F.C. 1877. Mémoire sur la flore Carbonifière. Mémoires a 1′Academie des Sciences de l'Institut Nationale de France, 24:1624.Google Scholar
Gray, J. 1988. Land plant spores and the Ordovician-Silurian boundary. Bulletin of the British Museum. Natural History. Geology Series, v. 43, p. 351358.Google Scholar
Hallbauer, D.K. 1986. The mineralogy and geochemistry of Witwatersrtand pyrite, gold, uranium, and carbonaceous matter, p. 731752. In Anhaeusser, C.R. and Maske, S., Mineral Deposits of Southern Africa, Geological Society of South Africa, Johannesburg, South Africa.Google Scholar
Hallbauer, D.K., and Van Warmelo, K.T. 1974. Fossilized plants in thucholite from Precambrian rocks of the Witwatersrand, South Africa. Precambrian Research, 1:199212.Google Scholar
Holland, H.D., and Kasting, J.F. 1992. The environments of the Archean Earth, p. 2124. In Schopf, J.W. and Klein, C. (eds.), The Proterozoic biosphere: a multidisciplinary study. Cambridge University Press, Cambridge.Google Scholar
Horodyski, R.J., and Knauth, L.P. 1994. Life on land in the Precambrian. Science, 263:494498.Google Scholar
Keller, C.K., and Wood, B.D. 1993. Possibility of chemical weathering before the advent of vascular plants. Nature, 364:223225.Google Scholar
Kidston, R., and Lang, W.H. 1917. On Old Red Sandstone plants showing structure form the Rhynie chert beds, Aberdeenshire. Parts I. Rhynia gwynne-vaughanii, Kidston and Lang. Transactions of the Royal Society of Edinburgh, 51:761784.Google Scholar
Kidston, R., and Lang, W.H. 1920a. On Old Red Sandstone plants showing structure form the Rhynie chert beds, Aberdeenshire. Parts II. Additional notes on Rhynia gwynne-vaughanii, Kidston and Lang; with descriptions of Rhynia major n. sp. and Hornea lignieri n.g., n.sp. Transactions of the Royal Society of Edinburgh, 52:603627.Google Scholar
Kidston, R., and Lang, W.H. 1920b. On Old Red Sandstone plants showing structure form the Rhynie chert beds, Aberdeenshire. Parts III. Asteroxylon mackiei, Kidston and Lang. Transactions of the Royal Society of Edinburgh, 52:643680.Google Scholar
Kidston, R., and Lang, W.H. 1921a. On Old Red Sandstone plants showing structure form the Rhynie chert beds, Aberdeenshire. Parts IV. Restoration of the vascular cryptogams, and discussion on their bearing on the general morphology of Pteridophyta and the origin of the organization of land plants. Transactions of the Royal Society of Edinburgh, 52:831854.Google Scholar
Kidston, R., and Lang, W.H. 1921b. On Old Red Sandstone plants showing structure form the Rhynie chert beds, Aberdeenshire. Parts V. The Thallophyta occurring in the peatbed; the succession of the plants throughout a vertical section of the bed, and conditions of accumulation and preservation of the deposit. Transactions of the Royal Society of Edinburgh, 52:855902.Google Scholar
Knoll, A.H. 1984. Patterns of extinction in the fossil record of vascular plants, p. 2168. In Nitecki, M.H. (ed.), Extinctions. The University of Chicago Press, Chicago.Google Scholar
Knoll, A.H., Niklas, K.J., and Tiffney, B.H. 1979. Phanerozoic land-plant diversity in North America. Science, 206:14001402.CrossRefGoogle ScholarPubMed
Krasilov, V.A. 1975. Paleoecology of terrestrial plants: basic principles and techniques. John Wiley & Sons, New York.Google Scholar
LePage, B.A., and Basinger, J.F. 1995a. The evolutionary history of the genus Larix (Pinaceae). United States Department of Agriculture, Forest Service, Intermontane Research Station, General Technical Report, GTR-INT-319:1929.Google Scholar
LePage, B.A., and Basinger, J.F. 1995b. Evolutionary and biogeographic history of the genus Pseudolarix (Pinaceae). International Journal of Plant Science, 156:910950.Google Scholar
Martini, J.E.J. 1994. A Late Archaean-Palaeoproterozoic (2.6 Ga) palaeosol on ultramafics in the eastern Transvaal, South Africa. Precambrian Research, 67:159180.Google Scholar
McIntyre, D.J. 1991. Pollen and spore flora of an Eocene forest, eastern Axel Heiberg Island, N.W.T. Geological Survey of Canada, Bulletin, 403:8397.Google Scholar
Metting, B. 1991. Biological surface features of semiarid lands and deserts, p. 257293. In Skujins, J. (ed.), Semiarid lands and deserts: soil resource and reclamation. Marcel Dekker, Inc., New York.Google Scholar
Miller, C.N. Jr. 1987. Land plants of the northern Rocky Mountains before the appearance of flowering plants. Annals of the Missouri Botanical Garden,74:692706.Google Scholar
Niklas, K.J., Tiffney, B.H., and Knoll, A.H. 1985. Patterns of vascular land plant diversification: an analysis at the species level, p. 97128. In Valentine, J.W. (ed.), Phanerozoic diversity patterns: profiles in macroevolution. Princeton University Press, Princeton.Google Scholar
Pettijohn, F.J. 1957. Sedimentary rocks, 2nd ed. Harper & Brothers, New York.Google Scholar
Pfefferkorn, H.W. 1999. Recuperation from mass extinctions. Proceedings of the National Academy of Sciences, 96:1359713599.Google Scholar
Pfefferkorn, H.W., and Fuchs, K. 1991. A field classification of fossil plant substrate interactions. Neues Jahrbuch für Geologie und Palaontologie, Abhandlungen, 183: 1736.Google Scholar
Pfefferkorn, H.W., and Zodrow, E.L. 1982. A comparison of standing forests from the Pennsylvanian of Nova Scotia with modern tropical forests. Botanical Society of America, Abstracts 1982, p. 6263 (Abstr.).Google Scholar
Pfefferkorn, H.W., Fuchs, K., Hecht, C., Hofmann, C., Rabold, J.M., and Wagner, T. 1988. Recent geology and taphonomy of the Orinoco Delta: overview and field observations. Heidelberger Geowissenschaftliche Abhandlungen, 20:2156.Google Scholar
Pratt, L.M., Phillips, T.L., and Dennison, J.M. 1978. Evidence of non-vascular land plants from the Early Silurian (Llandoverian) of Virginia, U.S.A. Review of Palaeobotany and Palynology, 25:121149.Google Scholar
Remy, W. 1982. Lower Devonian gametophytes: relation to the phylogeny of land plants. Science, 215:16251627.Google Scholar
Remy, W., and Remy, R. 1980a. Devonian gametophytes with anatomically preserved gametangia. Science, 208:295296.Google Scholar
Remy, W., and Remy, R. 1980b. Lyonophyton rhyniensis nov. gen. et nov. sp., ein Gametophyt aus dem Chert von Rhynie (Unterdevon, Schottland). Argumenta Palaeobotanica, 6:3772.Google Scholar
Retallack, G.J. 1986. Reappraisal of a 2200 Ma-old paleosol near Waterval Onder, South Africa. Precambrian Research, 32:195232.Google Scholar
Retallack, G.J. 1992a. What to call early plant formations on land. Palaios, 7:508520.Google Scholar
Retallack, G.J. 1992b. How to find a Precambrian paleosol, p. 1630. In Schidlowski, M., Golubic, S., Kimberley, M.M., McKirdy, D.M., and Trudinger, P.A. (eds.), Early organic evolution. Springer, New York.Google Scholar
Retallack, G.J. 1994. Were the Ediacaran fossils lichens? Paleobiology, 20:523544.Google Scholar
Retallack, G.J., and Feakes, C.R. 1987. Trace fossil evidence for Late Ordovician animals on land. Science, 235:6163.CrossRefGoogle ScholarPubMed
Rothwell, G.W., Grauvogel-Stamm, L., and Mapes, G. 2000. An herbaceous fossil conifer: gymnospermous ruderals in the evolution of Mesozoic vegetation. Palaeogeography, Palaeoclimatology, Palaeoecology, 156:139145.Google Scholar
Scheihing, M.H., and Pfefferkorn, H.W. 1984. The taphonomy of land plants in the Orinoco Delta: a model for the incorporation of plant parts in clastic sediments of Late Carboniferous age of Euramerica. Review of Palaeobotany and Palynology, 41:205240.Google Scholar
Schidlowski, M. P., and Aharon, P. 1992. Carbon cycle and carbon isotope record: geochemical impact of life over 3.8 Ga of Earth history, p. 147175. In Schidlowski, M., Golubic, S., Kimberley, M.M., McKirdy, D.M., and Trudinger, P.A. (eds.), Early organic evolution. Springer, New York.Google Scholar
Schopf, J.W. 1992. Paleobiology of the Archean, p. 2539. In Schopf, J.W. and Klein, C. (eds.), The Proterozoic biosphere: a multidisciplinary study. Cambridge University Press, Cambridge.Google Scholar
Schopf, J.W., and Walter, M.R. 1983. Archean microfossils: new evidence of ancient microbes, p. 214239. In Schopf, J.W. (ed.), Earth's earliest biosphere: its origin and evolution. Princeton University Press, Princeton.Google Scholar
Schopf, J.W., and Packer, B.M. 1987. Early Archean (3.3 billion to 3.5 billion-year-old) microfossils from Warrawoona Group, Australia. Science, 237:7073.Google Scholar
Stein, W.E., Harmon, G.D., and Hueber, F.M. 1993. Lichens in the Lower Devonian of North America. Geological Society of America, Abstracts, 25:A82.Google Scholar
Strother, P.K., Al-Hajri, S., and Traverse, A. 1996. New evidence for land plants from the lower Middle Ordovician of Saudi Arabia. Geology, 24:5558.Google Scholar
Taylor, T.N., Hass, H., Remy, W., and Kerp, H. 1995. The oldest fossil lichen. Nature, 378:244.Google Scholar
Tiffney, B.H., and Niklas, K.J. 1985. Clonal growth in land plants: a paleobotanical perspective, p. 3566. In Jackson, J.B.C., Buss, L.W., and Cook, R.E. (eds.), Population biology and evolution of clonal organisms. Yale University Press, New Haven.Google Scholar
Viles, H.A. 1984. Biokarst: review and prospect. Progress in Physical Geography, 8:523542.Google Scholar
West, N.E. 1990. Structure and function of microphytic soil crusts in wildland ecosystems of arid to semi-arid regions. Advances in Ecological Research, 20:179223.Google Scholar
Williams, G.E. 1986. Precambrian permafrost horizons as indicators of paleoclimate. Precambrian Research, 32:233242.Google Scholar
Wing, S.L., Hickey, L.J., and Swisher, C.C. 1993. Implications of an exceptional fossil flora for Late Cretaceous vegetation. Nature, 363:342344.Google Scholar
Wright, V.P. 1985. The precursor environment for vascular plant colonization. Philosophical Transactions of the Royal Society of London B, 309:143145.Google Scholar