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David A. Franzi

Researcher at State University of New York at Plattsburgh

Publications -  12
Citations -  402

David A. Franzi is an academic researcher from State University of New York at Plattsburgh. The author has contributed to research in topics: Deglaciation & Younger Dryas. The author has an hindex of 7, co-authored 12 publications receiving 279 citations.

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An updated radiocarbon-based ice margin chronology for the last deglaciation of the North American Ice Sheet Complex

April S. Dalton, +75 more
TL;DR: The most up-to-date and authoritative margin chronology for the entire ice sheet complex is featured in two publications (Geological Survey of Canada Open File 1574 [Dyke et al., 2003] and as mentioned in this paper ).
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A series of large, Late Wisconsinan meltwater floods through the Champlain and Hudson Valleys, New York State, USA

TL;DR: In this article, the authors estimated steady-state and three flood pulse discharges from these large meltwater reservoirs into the North Atlantic using channel geometry and a high resolution digital elevation model of the Late Wisconsinan paleogeography of the region.
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Timing and duration of North American glacial lake discharges and the Younger Dryas climate reversal

TL;DR: In this paper, the authors 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.
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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

TL;DR: In this paper, the authors present radiocarbon ages from terrestrial organic sources in the Champlain Valley that they associate with the pre-Champlain Sea proglacial lake phases; a musk-ox bone with an AMS age of 11,362±-115 14 C years B.P.
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Epeirogenic transgression near a triple junction: the oldest (latest early–middle Cambrian) marine onlap of cratonic New York and Quebec

TL;DR: The discovery of a fossiliferous interval (Altona Formation, new unit) under the Potsdam Formation requires a new geological synthesis of a large part of the northeast Laurentian craton.