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DOI:​10.1016/J.PALAEO.2006.10.027
Corpus ID: 128877976
Evidence from the Lake Champlain Valley for a later onset of the Champlain Sea and implications for late glacial meltwater routing to the North Atlantic
J. A. Rayburn, D. Franzi, P. Knuepfer
Published 2007
Geology

Palaeogeography, Palaeoclimatology, Palaeoecology
Abstract Ocean circulation models indicate that freshwater runoff from the North American continent during the last deglaciation may have had an effect on North Atlantic Ocean circulation, and… Expand
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41 Citations
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41 Citations
Timing and duration of North American glacial lake discharges and the Younger Dryas climate reversal
J. A. Rayburn, T. Cronin, D. Franzi, P. Knuepfer, D. Willard
GeologyQuaternary Research
2011
Abstract Radiocarbon-dated sediment cores from the Champlain Valley (northeastern USA) contain stratigraphic and micropaleontologic evidence for multiple, high-magnitude, freshwater discharges from… Expand
48 Citations
Evidence for meltwater drainage via the St. Lawrence River Valley in marine cores from the Laurentian Channel at the time of the Younger Dryas
E. Levac, M. Lewis, Vanessa Stretch, Katie Duchesne, Thomas Neulieb
Geology
2015
Abstract Debate is ongoing about the source(s) and paths of meltwater that drained into the North Atlantic Ocean at the time of the Younger Dryas (YD), especially the eastern route from glacial Lake… Expand
18 Citations
Impacts of post-glacial lake drainage events and revised chronology of the Champlain Sea episode 13-9 ka
T. Cronin, P. Manley, +6 authors M. Berke
Geology
2008
Abstract Lithologic, CHIRP (Compressed High Intensity Radar Pulse) sonar, paleomagnetic, stable isotopic and micropaleontological analyses of sediment cores from Lake Champlain (New York, Vermont)… Expand
49 Citations
A new water-level history for Lake Ontario basin: evidence for a climate-driven early Holocene lowstand
T. Anderson, C. Lewis
GeologyJournal of Paleolimnology
2011
Piston cores from deep-water bottom deposits in Lake Ontario contain shallow-water sediments such as, shell-rich sand and silt, marl, gyttja, and formerly exposed shore deposits including woody… Expand
24 Citations
The champlain sea/lake champlain transition recorded in the northeast arm of Lake Champlain, USA-Canada
Ashliegh Theresa Belrose
Geology
2015
Sediment accumulated on a lakebed archives information about past climate and changes in the regional environment. Previous studies (Burgess, 2007; Koff, 2011; Palmer, 2012) in the Northeast Arm of… Expand
From Sea To Lake: The Depositional History Of Saint Albans Bay, Vt, Usa
Matthew P. Kraft
Geology
2018
Sediment accumulated in lakes stores valuable information about past environments and paleoclimatological conditions. Cores previously obtained from Saint Albans Bay, located in the Northeast Arm of… Expand
Identification of Younger Dryas outburst flood path from Lake Agassiz to the Arctic Ocean
J. Murton, M. Bateman, S. Dallimore, J. Teller, Zhirong Yang
Environmental Science, MedicineNature
2010
TLDR
A large flood into the Arctic Ocean at the start of the Younger Dryas leads us to reject the widespread view that Agassiz overflow at this time was solely eastward into the North Atlantic Ocean. Expand
235 Citations
PDF
Stable isotope evidence for glacial lake drainage through the St. Lawrence Estuary, eastern Canada, ∼13.1–12.9 ka
T. Cronin, J. A. Rayburn, J. Guilbault, R. Thunell, D. Franzi
Geology
2012
Abstract Postglacial varved and rhythmically-laminated clays deposited during the transition from glacial Lake Vermont (LV) to the Champlain Sea (CS) record hydrological changes in the Champlain-St.… Expand
26 Citations
Oxygen-isotope Variations in Post-glacial Lake Ontario
Ryan Hladyniuk, F. Longstaffe
Geology
2016
Abstract The role of glacial meltwater input to the Atlantic Ocean in triggering the Younger Dryas (YD) cooling event has been the subject of controversy in recent literature. Lake Ontario is ideally… Expand
Lifting the Champlain Sea: A CAS Record of the Transition to Modern Lake Champlain
A. Robinson
Geology
2012
Author(s): Robinson, Andrew | Advisor(s): Lyons, Timothy | Abstract: Between about 9 and 13 ky bp, the isostatically depressed area of the Champlain, Ottawa and St Lawrence valleys were engulfed by… Expand
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References
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Geology
1994
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Freshwater outbursts to the oceans from glacial Lake Agassiz and their role in climate change during the last deglaciation
J. Teller, D. Leverington, J. Mann
Geology
2002
Abstract Lake Agassiz was the largest lake in North America during the last deglaciation. As the Laurentide Ice Sheet (LIS) retreated, large volumes of water stored in this proglacial lake were… Expand
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Geology
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Abstract Overflow from glacial Lake Agassiz has been implicated in affecting late-glacial ocean circulation and climate. The timing of the diversion of Lake Agassiz overflow away from its southern… Expand
125 Citations
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J. Donnelly, N. Driscoll, +4 authors S. Swift
Geology
2005
Glacial freshwater discharge to the Atlantic Ocean during de- glaciation may have inhibited oceanic thermohaline circulation, and is often postulated to have driven climatic fluctuations. Yet… Expand
72 Citations
A series of large, Late Wisconsinan meltwater floods through the Champlain and Hudson Valleys, New York State, USA
J. A. Rayburn, P. Knuepfer, D. Franzi
Geology
2005
Abstract The Champlain Valley in northeastern New York lies at the junction of two important Late Wisconsinan proglacial outflow routes, the Hudson Valley to the south and the St. Lawrence Valley to… Expand
65 Citations
14C chronology for ice retreat and inception of Champlain Sea in the St. Lawrence Lowlands, Canada
P. Richard, S. Occhietti
GeologyQuaternary Research
2005
AMS radiocarbon cross-dating of plant debris and marine shells trapped in a lake basin on Mount St. Hilaire (Québec, Canada) provides a direct assessment of a reservoir effect totaling ca. 1800 14C… Expand
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Routing of meltwater from the Laurentide Ice Sheet during the Younger Dryas cold episode
W. Broecker, J. Kennett, +4 authors W. Wolfli
Geology
Nature

1989
ROOTH1 proposed that the Younger Dryas cold episode, which chilled the North Atlantic region from 11,000 to 10,000 yr BP, was initiated by a diversion of meltwater from the Mississippi drainage to… Expand
Reduced meltwater outflow from the Laurentide ice margin during the Younger Dryas
A. Vernal, C. Hillaire‐Marcel, G. Bilodeau
Geology
Nature

1996
THE cause of the Younger Dryas cold event, which interrupted the last deglaciation, is still a matter of debate1. A prevalent hypothesis, proposed by Broecker et al.2 is that the abrupt climate… Expand
129 Citations
Late Wisconsinan Deglaciation and Champlain Sea Invasion in the St. Lawrence Valley, Québec
M. Parent, S. Occhietti
Geology
2007
Champlain Sea history is directly linked to Late Wisconsinan deglacial episodes. Champlain Sea Phase I (Charlesbourg Phase) began in the Quebec area at about 12.4 ka. It represented a western… Expand
82 Citations
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Successions of invertebrate microfossils and the late quaternary deglaciation of the central St Lawrence Lowland, Canada and United States
C. G. Rodrigues
Geology
1992
Abstract Foraminiferal and ostracode assemblages in late glacial and early post-glacial sediments of the Central St Lawrence Lowland show that a proglacial lake (Glacial Lake St Lawrence) preceded… Expand
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