@article {136,
	title = {Corrigendum to {\textquotedblleft}Timing and duration of North American glacial lake discharges and the Younger Dryas climate reversal{\textquotedblright} [Quaternary Research 75 (2011) 541{\textendash}551]},
	journal = {Quaternary Research},
	volume = {77},
	year = {2012},
	note = {id: 2156},
	pages = {214},
	issn = {0033-5894},
	doi = {10.1016/j.yqres.2011.09.008},
	url = {http://www.sciencedirect.com/science/article/pii/S0033589411001190},
	author = {Rayburn, John A. and Cronin, Thomas M. and Franzi, David A. and Knuepfer, Peter L. K. and Willard, Debra A.}
}
@article {218,
	title = {Micropaleontologic record of Quaternary paleoenvironments in the Central Albemarle Embayment, North Carolina, U.S.A},
	journal = {Palaeogeography, Palaeoclimatology, Palaeoecology},
	volume = {305},
	year = {2011},
	note = {id: 2182},
	pages = {227-249},
	abstract = {To understand the temporal and spatial variation of eustatic sea-level fluctuations, glacio{\textendash}hydro{\textendash}isostacy, tectonics, subsidence, geologic environments and sedimentation patterns for the Quaternary of a passive continental margin, a nearly complete stratigraphic record that is fully integrated with a three dimensional chronostratigraphic framework, and paleoenvironmental information are necessary. The Albemarle Embayment, a Cenozoic regional depositional basin in eastern North Carolina located on the southeast Atlantic coast of the USA, is an ideal setting to unravel these dynamic, interrelated processes. Micropaleontological data, coupled with sedimentologic, chronostratigraphic and seismic data provide the bases for detailed interpretations of paleoenvironmental evolution and paleoclimates in the 90 m thick Quaternary record of the Albemarle Embayment. The data presented here come from a transect of cores drilled through a barrier island complex in the central Albemarle Embayment. This area sits in a ramp-like setting between late Pleistocene incised valleys. The data document the episodic infilling of the Albemarle Embayment throughout the Quaternary as a series of transgressive{\textendash}regressive (T{\textendash}R) cycles, characterized by inner shelf, midshelf, and shoreface assemblages, that overlie remnants of fluvial to estuarine valley-fill. Barrier island and marginal marine deposits have a low preservation potential. Inner to mid-shelf deposits of the early Pleistocene are overlain by similar middle Pleistocene shelf sediments in the south of the study area but entirely by inner shelf deposits in the north. Late Pleistocene marine sediments are of inner shelf origin and Holocene deposits are marginal marine in nature. Pleistocene marine sediments are incised, particularly in the northern half of the embayment by lowstand paleovalleys, partly filled by fluvial/floodplain deposits and in some cases, overlain by remnants of transgressive estuarine sediments. The shallowing through time of Quaternary sediments reflects the eastward progradational geometry of the continental shelf. The preservation potential of marginal marine deposits (barrier island, shoreface, backbarrier deposits) is not high, except in topographic lows associated with late Pleistocene paleovalleys and inlets because the current interglacial highstand has not yet reached its highest level. Given the documented increase in rate of relative sea-level rise in this region, shallow marine conditions are likely to return to the central Albemarle Embayment in the near future.},
	issn = {0031-0182},
	doi = {10.1016/j.palaeo.2011.03.004},
	url = {http://www.sciencedirect.com/science/article/pii/S0031018211001143},
	author = {Culver, Stephen J. and Farrell, Kathleen M. and Mallinson, David J. and Willard, Debra A. and Horton, Benjamin P. and Riggs, Stanley R. and Thieler, E. Robert and Wehmiller, John F. and Parham, Peter and Snyder, Scott W. and Hillier, Caroline}
}
@article {186,
	title = {Timing and duration of North American glacial lake discharges and the Younger Dryas climate reversal},
	journal = {Quaternary Research},
	volume = {75},
	year = {2011},
	note = {id: 2184},
	pages = {541-551},
	abstract = {Radiocarbon-dated sediment cores from the Champlain Valley (northeastern USA) contain stratigraphic and micropaleontologic evidence for multiple, high-magnitude, freshwater discharges from North American proglacial lakes to the North Atlantic. Of particular interest are two large, closely spaced outflows that entered the North Atlantic Ocean via the St. Lawrence estuary about 13,200{\textendash}12,900 cal yr BP, near the beginning of the Younger Dryas cold event. We estimate from varve chronology, sedimentation rates and proglacial lake volumes that the duration of the first outflow was less than 1 yr and its discharge was approximately 0.1 Sv (1 Sverdrup = 106 m3 s-1). The second outflow lasted about a century with a sustained discharge sufficient to keep the Champlain Sea relatively fresh for its duration. According to climate models, both outflows may have had sufficient discharge, duration and timing to affect meridional ocean circulation and climate. In this report we compare the proglacial lake discharge record in the Champlain and St. Lawrence valleys to paleoclimate records from Greenland Ice cores and Cariaco Basin and discuss the two-step nature of the inception of the Younger Dryas.},
	issn = {0033-5894},
	doi = {10.1016/j.yqres.2011.02.004},
	url = {http://www.sciencedirect.com/science/article/pii/S003358941100024X},
	author = {Rayburn, John A. and Cronin, Thomas M. and Franzi, David A. and Knuepfer, Peter L. K. and Willard, Debra A.}
}
@article {391,
	title = {Sea level rise in Tampa Bay},
	journal = {Eos, Transactions, American Geophysical Union},
	volume = {88},
	year = {2007},
	note = {id: 1899; References: 14; illus. incl. geol. sketch map Latitude:N272700,N280200 Longitude:W0822200,W0825100Y},
	pages = {117-118},
	issn = {0096-3941},
	doi = {10.1029/2007eo100002},
	author = {Cronin, Thomas M. and Edgar, N. Terence and Brooks, Gregg and Hastings, David and Larson, Rebekka and Hine, Albert and Locker, Stanley and Suthard, Beau and Flower, Benjamin and Hollander, David and Wehmiller, John and Willard, Debra A. and Smith, Shannon}
}
