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The stratigraphy and development of a floating peatland, Pinhook Bog, Indiana

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Abstract

Pinhook Bog is an acidic, weakly-minerotrophic peatland that occupies an iceblock depression in the Valparaiso Moraine in northwest Indiana. It has a floating mat approximately 22 ha in area but no central pond. Detailed stratigraphic descriptions of the peatland were made to analyze its developmental history and determine what factors may be responsible for mat formation. Stratigraphic data along four transects identified a clay-lined basin with three major sub-basins 18, 14, and 14 m deep. The deeper parts of the sub-basins contain fibrous limnic peats with some intermixed lacustrine sediments deposited between 12000 and 4200 years ago. The younger, upper peat layers are composed primarily ofSphagnum and consist of the fibrous surface peat and two underlying layers of fluid, fibrous peat separated by a water layer about one meter thick. Peat materials from above the water layer have fallen through the water to form the lower layer of detritus peat.

In addition to the obvious factors of climate and presence of mat-forming species, the development of extensive floating peatland mats is considered to be largely a function of deep, steep-sided basins that allow horizontal mat growth to exceed vertical peat accumulation. Other important contributing factors are clay-lined basins and the lack of inlets or outlets. These factors may result in water-level changes in the basin and weakly-minerotrophic waters conducive toSphagnum growth.

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References

  • Bailey, R.E.. 1972. Late-glacial and post-glacial environmental changes in northwestern Indiana. Ph.D. Dissertation. Indiana University, Bloomington, IN, USA.

    Google Scholar 

  • Boatman, D.J. and W. Armstrong. 1968. A bog type in north-west Sutherland. Journal of Ecology 56: 129–141.

    Article  Google Scholar 

  • Brown, S.R. 1956. A piston sampler for surface sediments of lake deposits. Ecology 37: 611–613.

    Article  Google Scholar 

  • Buell, M.F. and H.F. Buell. 1941. Surface level fluctuations in Cedar Creek Bog, Minnesota. Ecology 22: 317–321.

    Article  Google Scholar 

  • Buell, M.F. and H.F. Buell. 1975. Moat bogs in the Itasca Park area, Minnesota. Bulletin of the Torrey Botanical Club 102: 6–9.

    Article  Google Scholar 

  • Changnon, S.A. 1980. More on the LaPorte anomaly: a review. Bulletin of the American Meteorological Society 61: 702–711.

    Article  Google Scholar 

  • Clymo, R.S. 1984. The limits to peat bog growth. Philosophical Transactions of the Royal Society of London Series B 303: 605–654.

    Article  Google Scholar 

  • Coburn, H., D. Dean, and G.M. Grant 1932. An ecological study of Bryant’s Bog, Cheboygan County, Michigan. Papers on the Michigan Academy of Science, Arts, and Letters 17: 57–65.

    Google Scholar 

  • Conway, V.M. 1949. The bogs of central Minnesota. Ecological Monographs 19: 173–206.

    Article  Google Scholar 

  • Engstrom, D.R. 1984. Lake development in the boreal peatlands of southeastern Labrador, Canada. Arctic and Alpine Research 16: 447–452.

    Article  Google Scholar 

  • Foster, D.R., G.A. King, P.H. Glaser, and H.E. Wright, Jr. 1983. Origin of string patterns in boreal peatlands. Nature 306: 256–258.

    Article  Google Scholar 

  • Futyma, R.P. 1985. Paleobotanical studies at Indiana Dunes National Lakeshore. National Park Service, Porter, IN, USA.

    Google Scholar 

  • Gates, F.C. 1942. The bogs of northern Lower Michigan Ecological Monographs 12: 213–254.

    Article  Google Scholar 

  • Gore, A.J.P. 1983. Introduction. p. 1–34.In A.J.P. Gore (ed.) Ecosystems of the World. Mires: Swamp, Bog, Fen and Moor. 4A. General Studies. Elsevier, Amsterdam, The Netherlands.

    Google Scholar 

  • Gorham, E. 1957. The development of peat lands. The Quarterly Review of Biology 32: 145–166.

    Article  Google Scholar 

  • Green, B.H. and M.C. Pearson 1977. The ecology of Wybunbury Moss, Cheshire. II. Post-glacial history and the formation of the Cheshire mere and mire landscape. Journal of Ecology 65: 793–814.

    Article  Google Scholar 

  • Guennel, G.K. 1950. History of forests in the glacial Lake Chicago area. Butler University Botanical Studies 9: 140–158.

    Google Scholar 

  • Hansel, A.K., D.M. Mickelson, A.F. Schneider, and C.E. Larsen. 1985. Late Wisconsinan and Holocene history of the Lake Michigan basin. p. 39–53.In P.F. Karrow and P.E. Calkin (eds.) Quaternary Evolution of the Great Lakes. Geological Association of Canada Special Paper 30.

  • Harman, J.R. and W.M. Elton. 1971. The LaPorte, Indiana precipitation anomaly. Annals of the Association of American Geographers 51: 468–480.

    Article  Google Scholar 

  • Heinselman, M.L. 1970. Landscape evolution, peatland types, and the environment of the Lake Agassiz Peatlands Natural Area, Minnesota. Ecological Monographs 40: 235–261.

    Article  Google Scholar 

  • Johnson, W.H. 1976. Quaternary stratigraphy in Illinois: status and problems. p. 161–196.In W.C. Mahaney (ed.) Quaternary Stratigraphy of North America. Dowden. Hutchinson, and Ross, Inc., Stroudsburg, PA, USA.

    Google Scholar 

  • Jowsey, P.C. 1966. An improved peat sampler. New Phytologist 65: 245–248.

    Article  Google Scholar 

  • Kratz, T.K. 1981. The formation of a northern Wisconsin kettle-hole bog: a spatial, ecosystem modeling perspective. Ph.D. Dissertation. University of Wisconsin, Madison, WI, USA

    Google Scholar 

  • Kratz, T.K. and C.B. DeWitt. 1986. Internal factors controlling peatland-lake ecosystem development. Ecology 67: 100–107.

    Article  Google Scholar 

  • Moore, P.D. 1977. Stratigraphy and pollen analysis of Claish Moss, northwest Scotland: significance for the origin of surface-pools and forest history. Journal of Ecology 65: 375–397.

    Article  Google Scholar 

  • Moore, P.D. and P.J. Beckett. 1971. Vegetation and development of Llyn, a Welsh mire. Nature 231: 363–365.

    Article  Google Scholar 

  • Moore, P.D. and D.J. Bellemy. 1974. Peatlands. Springer-Verlag, New York, NY, USA.

    Google Scholar 

  • Mörnsjö, T. 1968. Stratigraphical and chemical studies on two peatlands in Scania, South Sweden. Botaniska Notiser 121: 343–360.

    Google Scholar 

  • Osvald, H. 1970. Vegetation and stratigraphy of peatlands in North America. Nova Acta Regiae Societatis Scientarium Upsaliensis Series V: C 1: 1–96.

    Google Scholar 

  • Overpeck, J.T. 1985. A pollen study of a late Quaternary peat bog, south-central Adirondack Mountains, New York. Geological Society of America Bulletin 96: 145–154.

    Article  Google Scholar 

  • Rigg, G.B. 1940a. Comparisons of the development of some sphagnum bogs of the Atlantic coast, the interior, and the Pacific coast. American Journal of Botany 27: 1–14.

    Article  Google Scholar 

  • Rigg, G.A. 1940b. The development of sphagnum bogs in North America. Botanical Review 6: 666–693.

    Article  CAS  Google Scholar 

  • Rigg, G.B. and C.T. Richardson. 1934. The development of sphagnum bogs in the San Juan Islands. American Journal of Botany 21: 610–622.

    Article  Google Scholar 

  • Rigg, G.B. and C.T. Richardson. 1938. Profiles of some sphagnum bogs of the Pacific coast of North America. Ecology 19: 408–434.

    Article  Google Scholar 

  • Schwintzer, C.R. 1978a. Vegetation and nutrient status of northern Michigan fens. Canadian Journal of Botany 56: 3044–3051.

    Article  CAS  Google Scholar 

  • Schwintzer, C.R. 1978b. Nutrient and water levels in a small Michigan bog with high tree mortality. American Midland Naturalist 100: 441–451.

    Article  CAS  Google Scholar 

  • Schwintzer, C.R. and G. Williams. 1974. Vegetation changes in a small Michigan bog from 1917 to 1972. American Midland Naturalist 92: 447–459.

    Article  Google Scholar 

  • Sjörs, H. 1983. Mires of Sweden. p. 220–250.In A.J.P. Gore (ed.) Ecosystems of the World. Mires: Swamp, Bog, Fen and Moor. 4B. Regional Studies. Elsevier, Amsterdam, The Netherlands.

    Google Scholar 

  • Swan, J.M.A. and A.M. Gill. 1970. The origins, spread, and consolidation of a floating bog in Harvard Pond, Petersham, Massachusetts. Ecology 51: 829–840.

    Article  Google Scholar 

  • Tallis, J.H. 1973. The terrestrialization of lake basins in North Cheshire, with special reference to the development of a “Schwingmoor” structure. Journal of Ecology 61: 537–567.

    Article  Google Scholar 

  • Tallis, J.H. 1983. Changes in wetland communities. p. 311–348.In A.J.P. Gore (ed.) Ecosystems of the World. Mires: Swamp, Bog, Fen and Moor. 4A. General Studies. Elsevier, Amsterdam, The Netherlands.

    Google Scholar 

  • Tolonen, K. 1966. Stratigraphic and rhizopod analyses on an old raised bog, Varrassuo, in Hollola, South Finland. Annales Botanici Fonnici 3: 147–166.

    Google Scholar 

  • Vitt, D.H. and N.G. Slack 1975. An analysis of the vegetation ofSphagnum-dominated kettle-hole bogs in relation to environmental gradients. Canadian Journal of Botany 53: 332–359.

    Article  Google Scholar 

  • Walker, D. 1970. Direction and rate in some British post-glacial hydroseres. p. 117–139.In D. Walker and R.G. West (eds.) Studies in the Vegetational History of the British Isles. University Press of Cambridge, Cambridge, UK.

    Google Scholar 

  • Wells, G.L. 1983. Late-glacial circulation over central North America revealed by aeolian features. p. 317–330.In A. Street-Perrott, M. Berau, and R. Ratcliffe (eds.) Variations in the Global Water Budget. D. Reidel Publishing Company, Dordordrecht, The Netherlands.

    Google Scholar 

  • Wilcox, D.A. 1982. The effects of deicing salts on water chemistry and vegetation in Pinhook Bog, Indiana. Ph.D. Dissertation. Purdue University, West Lafayette, IN, USA.

    Google Scholar 

  • Wilcox, D.A. 1986a. The effects of deicing salts on water chemistry in Pinhook Bog, Indiana. Water Resources Bulletin 22: 57–65.

    CAS  Google Scholar 

  • Wilcox, D.A. 1986b. The effects of deicing salts on vegetation in Pinhook Bog, Indiana. Canadian Journal of Botany 64: 865–874.

    Article  CAS  Google Scholar 

  • Wilcox, D.A., R.J. Shedlock, and W.H. Hendrickson. 1986. Hydrology, water chemistry and ecological relations in the raised mound of Cowles Bog. Journal of Ecology 74: 1103–1117.

    Article  Google Scholar 

  • Wilcox, D.A. and H.A. Simonin. 1987. A chronosequence of aquatic macrophyte communities in dune ponds. Aquatic Botany 28: 227–242.

    Article  Google Scholar 

  • Wright, H.E., Jr. 1983. Introdution. p. xi-xvii.In H.E. Wright, Jr. (ed.) Late-Quaternary Environments of the United States. University of Minnesota Press, Minneapolis, MN, USA.

    Google Scholar 

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Wilcox, D.A., Simonin, H.A. The stratigraphy and development of a floating peatland, Pinhook Bog, Indiana. Wetlands 8, 75–91 (1988). https://doi.org/10.1007/BF03160810

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