@article {919,
	title = {Hydrology, vegetation, and climate change in the southern Everglades during the Holocene},
	journal = {Bulletin of American Paleontology},
	volume = {361},
	year = {2001},
	note = {id: 125},
	pages = {57-99},
	abstract = {Paleoecological study of 18 AMS-dated sediment cores from the southern Everglades provides evidence of a shifting mosaic of biotic communities in the past similar to those on the Everglades landscape today. Our results also indicate initiation of Everglades peatlands at 5900 yr B. P., the importance of fire (from charcoal analysis) as a structuring agent in the tropical Everglades, evidence of past plant communities (Isoetes marshes) not present in the modern landscape, and the introduction of exotic plants (Schinus, Casuarina, etc.) today. Past vegetation changes are documented by pollen and sclereid changes. Past water level changes are documented by plant community changes, diatom species and habitat changes, sponge spicule changes, and by intervals of peat (wet) or marl (dry) deposition in the sediment cores. Marl deposition dominates today at these sites in the southern Everglades, a long-term trend exacerbated by human impacts. The Everglades may become less complex in the near future as introduced plants outcompete native vegetation and decreased water levels result in decreased peat production. A rewatering plan must include both wet and dry seasonal cycles in order to preserve the shifting mosaic nature of the landscape and to maintain the Everglades as a functional habitat for both plants and animals.},
	author = {Winkler, M. G. and Sanford, P. R. and Kaplan, S. W.}
}
@article {1520,
	title = {Environmental changes in the last centure in Little Trout Lake, Inkspot Bay, Great Corn and Little Corn Lakes, Lac du Flambeau Tribal Lands, Wisconsin. Report},
	volume = {Final Report to Water Resources Division, Lac du Flambeau Tribe},
	year = {2000},
	note = {id: 128},
	month = {2000},
	pages = {44},
	author = {Winkler, M. G. and Sanford, P. R.}
}
@article {1517,
	title = {Environmental changes in the last centure in Little Trout Lake and Inkspot Bay, Lac du Flambeau Tribal Lands, Wisconsin. Preliminary Results Report},
	year = {1999},
	note = {id: 1320},
	month = {1999},
	pages = {12},
	institution = {Water Resources Division, Lac du Flambeau Tribe},
	author = {Winkler, M. G. and Sanford, P. R.}
}
@article {1513,
	title = {Environmental changes since deglaciation in Voyageurs National Park: A summary for park personnel in Holocene Paleoenvironnments in Western Great Lakes Park. Report},
	volume = {9; Final report},
	year = {1998},
	note = {id: 129},
	month = {1998},
	pages = {3},
	institution = {National Park Service},
	author = {Winkler, M. G. and Sanford, P. R.}
}
@article {1514,
	title = {Western Great Lakes paleoecology study, global climate change initiative. In Holocene Paleoenvironments in Western Great Lakes Parks. Report},
	volume = {Final report},
	year = {1998},
	note = {id: 130},
	month = {1998},
	institution = {National Park Service \& USGS Biological Resources Div., Northern Prairie Wildlife Research Center},
	address = {Columbia, Missouri},
	author = {Winkler, M. G. and Sanford, P. R.}
}
@article {1509,
	title = {Paleoecological research at Isle Royale, Apostle Islands, and Voyageurs National Parks. Report},
	year = {1997},
	note = {id: 1321},
	month = {1997},
	pages = {85},
	author = {Winkler, M. G. and Sanford, P. R.}
}
@article {2278,
	title = {Paleolimnology research at Isle Royale, Apostle Island, and Voyageurs National Parks},
	journal = {USGS Biological Resources Division, Global Change Research Program},
	volume = {Summary Report},
	year = {1997},
	note = {id: 1299},
	month = {1997},
	author = {Winkler, M. G. and Sanford, P. R.}
}
@article {1484,
	title = {Preliminary paleoecology study of Salt Pond and Nauset Lagoon, Cape Cod National Seashore (Report)},
	volume = {Final Report},
	year = {1997},
	note = {id: 131},
	month = {1997},
	pages = {40},
	institution = {National Park Service, North Atlantic Region},
	author = {Cole, K. and Winkler, M. G. and Sanford, P. R.}
}
@article {1510,
	title = {Western Great Lakes Paleoecology Study. Report},
	volume = {Interim Report},
	year = {1997},
	note = {id: 1322},
	month = {1997},
	pages = {71},
	institution = {National Biological Service Global Climate Change Initiative},
	author = {Winkler, M. G. and Sanford, P. R.}
}
@article {2277,
	title = {Western Great Lakes regional paleoenvironmental changes: island and inland contrasts},
	journal = {Ecological Society of America Bulletin},
	year = {1997},
	note = {id: 1301},
	month = {1997},
	author = {Winkler, M. G. and Sanford, P. R. and Cole, K. L. and Flakne, R. L.}
}
@conference {1737,
	title = {Paleoecology of the Everglades National Park Paper},
	booktitle = {Florida Bay Science Conference},
	year = {1996},
	note = {id: 1298},
	month = {1996},
	pages = {121-124},
	address = {Florida},
	author = {Winkler, M. G. and Sanford, P. R. and Kaplan, S. W.}
}
@article {1507,
	title = {Paleoecology of the Everglades National Park. Report},
	volume = {Technical Report 97-006},
	year = {1996},
	note = {id: 1324},
	month = {1996},
	pages = {212},
	institution = {National Park Service, Everglades National Park},
	address = {Homestead, Florida},
	author = {Winkler, M. G. and Sanford, P. R. and Kaplan, S.}
}
@article {868,
	title = {Coastal Massachusetts Pond Development - Edaphic, Climatic, and Sea-Level Impacts since Deglaciation},
	journal = {Journal of Paleolimnology},
	volume = {14},
	year = {1995},
	note = {Td951Times Cited:1Cited References Count:62},
	month = {Nov},
	pages = {311-336},
	abstract = {Kettle ponds in the Cape Cod National Seashore in southeastern Massachusetts differ in their evolution due to depth of the original ice block, the clay content of outwash in their drainage basins, and their siting in relation to geomorphic changes caused by sea-level rise, barrier beach formation, and saltmarsh development. Stratigraphic records of microfossil, carbon isotope, and sediment changes also document late-glacial and Holocene climatic changes.The ponds are separated into 3 groups, each of which follow different development scenarios. Group I ponds date from the late-glacial. They formed in clay-rich outwash, have perched aquifers and continuous lake sediment deposition. The earliest pollen and macrofossil assemblages in Group I pond sediments suggest tundra and spruce-willow parklands before 12 000 yr B.P., boreal forest between 12 000 and 10 500 yr B.P., bog/heath initiation and expansion during the Younger Dryas between 11 000 and 10 000 yr B.P., northern conifer forest between 10 500 and 9500 yr B.P., and establishment of the Cape oak and pitch pine barrens vegetation after 9500 yr B.P. Sedimentation rate changes suggest lowered freshwater levels between 9000 and 5000 yr B.P. caused by decreased precipitation on the Atlantic Coastal Plain. Lake sediment deposition began in the middle Holocene in Group II ponds which formed in clay-poor outwash. These ponds date from about 6000-5000 yr B.P. In these ponds sediment deposition began as sea level rose and the freshwater lens intersected the dry basins. The basal radiocarbon dates of these ponds and stable carbon isotope analyses of the pond sediments suggest a sea-level curve for Cape Cod Bay. Holocene topographic changes in upland and the landscape surrounding the ponds is reconstructed for this coastal area.Group III ponds in the late Holocene landscape of the Provincelands dunes originated as interdunal bogs about 1000 yr B.P. and became ponds more recently as water-levels increased. Feat formation in the Provincelands reflects climatic changes evident on both sides of the Atlantic region.},
	issn = {0921-2728},
	doi = {10.1007/Bf00682431},
	author = {Winkler, M. G. and Sanford, P. R.}
}
