@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.}
}
@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 {5227,
	title = {Response to Comment on {\textquotedblleft}Redefining the Age of Clovis: Implications for the Peopling of the Americas{\textquotedblright}},
	journal = {Science},
	volume = {317},
	year = {2007},
	month = {07/2007},
	pages = {320c - 320c},
	issn = {0036-8075},
	doi = {10.1126/science.1142812},
	author = {Waters, M. R. and Stafford, T. W.}
}
@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.}
}
