@article {5255,
	title = {A 1400-Year B{\o}lling-Aller{\o}d Tree-Ring Record from the U.S. Great Lakes Region},
	journal = {Tree-Ring ResearchTree-Ring Research},
	volume = {73},
	year = {2017},
	month = {2017/07/01},
	pages = {102 - 112},
	isbn = {1536-1098},
	url = {https://doi.org/10.3959/1536-1098-73.2.102},
	author = {Panyushkina, Irina P. and Leavitt, Steven W. and Mode, William N.}
}
@article {5236,
	title = {Deglacial hydroclimate for Midcontinental North America.},
	journal = {Quaternary Research },
	volume = {83},
	year = {2015},
	chapter = {336},
	doi = {10.1016/j.yqres.2015.01.001 },
	author = {Voelker, S.L and Stambaugh, M.C. and Guyette, R.P. and Feng, X. and Grimley, D.A. and Leavitt, S.W. and Panyushkina, I.P. and Grimm, E.C. and Marsicek, J.P. and Shuman, B. and Curry, B.B.}
}
@article {5238,
	title = {Tree-ring investigation of Holocene flood-deposited wood from the Oneida Lake watershed, New York State.},
	journal = {Tree-Ring Research},
	volume = {71},
	year = {2015},
	chapter = {83},
	author = {Panyushkina, I.P. and Leavitt, S.W. and Domack, E.W. and Wiedenhoeft, A.C.}
}
@article {5237,
	title = {. Ancient boreal forests under the environmental instability of the glacial to post-glacial transition in the Great Lakes region (14,000-11,000 years BP)},
	journal = {Canadian Journal of Forest Research },
	volume = {43},
	year = {2013},
	chapter = {1032},
	doi = {10.1139/cjfr-2012-0339},
	author = {Panyushkina, I.P. and Leavitt, S.W.}
}
@article {5235,
	title = {Tapping Ancient Tree-Ring Archives in the U.S. Great Lakes Region.},
	volume = {91 (50)},
	number = {489},
	year = {2010},
	author = {Panyushkina, I.P. and Leavitt, S.W.}
}
@article {5225,
	title = {Environment and paleoecology of a 12 ka mid-North American Younger Dryas forest chronicled in tree rings},
	journal = {Quaternary Research},
	volume = {70},
	year = {2008},
	month = {11/2008},
	pages = {433{\textendash}441},
	chapter = {433},
	abstract = {<p>Until now, availability of wood from the Younger Dryas abrupt cooling event (YDE) in N. America ca. 12.9 to 11.6 ka has been insufficient to develop high-resolution chronologies for refining our understanding of YDE conditions. Here we present a multi-proxy tree-ring chronology (ring widths, {\textquotedblleft}events{\textquotedblright} evidenced by microanatomy and macro features, stable isotopes) from a buried black spruce forest in the Great Lakes area (Liverpool East site), spanning 116\&nbsp;yr at ca. 12,000\&nbsp;cal yr BP. During this largely cold and wet period, the proxies convey a coherent and precise forest history including frost events, tilting, drowning and burial in estuarine sands as the Laurentide Ice Sheet deteriorated. In the middle of the period, a short mild interval appears to have launched the final and largest episode of tree recruitment. Ultimately the tops of the trees were sheared off after death, perhaps by wind-driven ice floes, culminating an interval of rising water and sediment deposition around the base of the trees. Although relative influences of the continental ice sheet and local effects from ancestral Lake Michigan are indeterminate, the tree-ring proxies provide important insight into environment and ecology of a N. American YDE boreal forest stand.</p>
},
	issn = {00335894},
	doi = {10.1016/j.yqres.2008.08.006},
	author = {Irina P. Panyushkina and Steven W. Leavitt and Todd A. Thompson and Allan F. Schneider and Todd Lange}
}
@inbook {5240,
	title = {Insights into Late Pleistocene{\textendash}Early Holocene Paleoecology from fossil wood around the Great Lakes region. In: Late-Glacial History of East-central Wisconsin},
	booktitle = {Late-Glacial History of East-central Wisconsin. },
	year = {2007},
	edition = { T.S. Hooyer},
	author = {Panyushkina, I.P. and Leavitt, S.W.}
}
@inbook {5241,
	title = {Late-glacial and early Holocene paleoecology: Schneider farm, Calumet County. In: Late-Glacial History of East-central Wisconsin},
	booktitle = {Late-Glacial History of East-central Wisconsin},
	year = {2007},
	edition = {T.S. Hooyer},
	author = {Mode, W.N. and Panyushkina, I.P. and Leavitt, S.W. and Williams, J.W. and Santiago, A. and Gill, J. and Edwards, C. and Gertz, H.}
}
@article {5234,
	title = {Radiocarbon {\textquotedblleft}wiggles{\textquotedblright} in Great Lakes wood ca. 10,000 to 12,000 BP},
	journal = {Radiocarbon},
	volume = {49},
	year = {2007},
	chapter = {855},
	author = {Leavitt, S.W. and Panyushkina, I.P. and Lange, T. and Cheng, L. and Schneider, A.F. and Hughes, J.}
}
@article {5232,
	title = {Climate in the Great Lakes region between 14,000 and 4,000 years ago from isotopic composition of conifer wood},
	journal = {Radiocarbon},
	volume = {48},
	year = {2006},
	chapter = {205},
	author = {Leavitt, S.W. and Panyushkina, I.P and Lange, T. and Wiedenhoeft, A. and Cheng, L. and Hunter, R.D.}
}
@article {5229,
	title = {A multiproxy environmental investigation of Holocene wood from a submerged conifer forest in Lake Huron, USA},
	journal = {Quaternary Research},
	volume = {66},
	year = {2006},
	month = {07/2006},
	pages = {67{\textendash}77},
	chapter = {67},
	abstract = {<p>Remains of a Holocene drowned forest in southern Lake Huron discovered in 12.5\&nbsp;m of water (164\&nbsp;m above sea level), 4.5\&nbsp;km east of Lexington, Michigan USA (Sanilac site), provided wood to investigate environment and lake history using several proxies. Macrofossil evidence indicates a forest comprised primarily of conifers equivalent to the modern {\textquotedblleft}rich conifer swamp{\textquotedblright} community, despite generally low regional abundance of these species in pollen records. Ages range from 7095 {\textpm} 50 to 6420 {\textpm} 70 <sup>14</sup>C yr BP, but the clustering of stump dates and the development of 2 floating tree-ring chronologies suggest a briefer forest interval of no more than c. 400 years. Dendrochronological analysis indicates an environment with high inter-annual climate variability. Stable-carbon isotope composition falls within the range of modern trees from this region, but the stable-oxygen composition is consistent with warmer conditions than today. Both our tree-ring and isotope data provide support for a warmer environment in this region, consistent with a mid-Holocene thermal maximum. This drowned forest also provides a dated elevation in the Nipissing transgression at about 6420 <sup>14</sup>C yr BP (7350 cal yr BP) in the southern Lake Huron basin, a few hundred years before reopening of the St. Clair River drainage.</p>
},
	doi = {10.1016/j.yqres.2006.03.008},
	author = {Hunter, R. Douglas and Panyushkina, Irina P. and Leavitt, Steven W. and Wiedenhoeft, Alex C. and Zawiskie, John}
}
@article {5230,
	title = {Tree-ring records of near-Younger Dryas time in Central North America- preliminary results from the Lincoln quarry site, central Illinois, USA},
	journal = {Radiocarbon},
	volume = {46},
	year = {2004},
	chapter = {933},
	author = {Panyushkina, I.P. and Leavitt, S.W. and Wiedenhoeft, A. and Noggle, S. and Curry, B. and Grimm, E.}
}
@article {5249,
	title = {A buried spruce forest provides evidence at the stand and landscape scale for the effects of environment on vegetation at the Pleistocene/Holocene boundary},
	journal = {Journal of Ecology},
	volume = {88},
	year = {2000},
	chapter = {45},
	doi = {10.1046/j.1365-2745.2000.00432.x. },
	author = {Pregitzer, K.S. and Reed, D.D. and Bornhorst, T.J. and Foster, D.R. and Mroz, G.D. and McLachlin, J.S. and Laks, P.E., and Stokke, D.D., and Martin, P.E., and Brown, S.E.}
}
