Title Information
Title
Evidence of late Pleistocene and Holocene Centennial-Scale Drought from Southeastern Massachusetts
Name: Personal
Name Part
Newby, Paige E
Role
Role Term: Text
creator
Origin Information
Copyright Date
2010
Physical Description
Extent
xiv, 169 p.
digitalOrigin
born digital
Note
Thesis (Ph.D. -- Brown University (2010)
Name: Personal
Name Part
Donnelly, Jeffrey
Role
Role Term: Text
Director
Name: Personal
Name Part
Herbert, Timothy
Role
Role Term: Text
Director
Name: Personal
Name Part
Tullis, Jan
Role
Role Term: Text
Reader
Name: Personal
Name Part
Russell, James
Role
Role Term: Text
Reader
Name: Personal
Name Part
Anderson, Douglas
Role
Role Term: Text
Reader
Name: Corporate
Name Part
Brown University. Geological Sciences
Role
Role Term: Text
sponsor
Genre (aat)
theses
Abstract
Past hydroclimatic change is shown from the reconstruction of paleo-lake levels from New Long and Rocky Ponds in southeastern Massachusetts, and Davis Pond in western Massachusetts show evidence for multiple, sub-centennial-to-millennial scale lowstands during the transition from the late-Pleistocene (15.0 ka) through the Holocene (0.0 ka), and for repeated sub-millennial scale, spatially coherent, lake level changes from 8.0 - 0.0 ka. Sedimentary evidence from New Long Pond indicates a drop in water levels in the mid AD 20th century, when instrumental data show lower-than-average precipitation in the northeastern United States, and a prolonged low water stand during the Medieval Climate Anomaly like that in the American southwest, which also overlaps a 100-yr interval of warm tropical Atlantic sea surface temperatures and cool La NiƱa-like Pacific conditions. Ground penetrating radar and sediment core data from the basins indicate numerous paleo-shoreline deposits from 15.0-7.0 ka. Davis and New Long Ponds also reveal past droughts during the Holocene. Many of the late-Pleistocene/early Holocene low lake levels coincide with proposed meltwater release events or abrupt climate oscillations in the North Atlantic region, with at least three low stands during the Younger Dryas, and in association with the "9.2" and "8.2" ka events. Although the effect of summer insolation after 8.0 ka may be instrumental in a sequence of droughts from 6.2-4.8 ka, the ca. 6.0 ka and 3.1-2.7 ka droughts also coincide with reduced meridional overturning circulation in the North Atlantic region. The combined evidence of concurrent paleo-droughts in southeastern New England with documented North Atlantic abrupt cooling events, and recent drought with the modern association of low sea-surface temperatures, indicates that freshening and cooling of the western North Atlantic is a viable mechanism for decreasing moisture within the region. Large-scale changes in seasonality and ice sheet extent also may have increased the susceptibility of the northeast to dry conditions triggered by changes in the North Atlantic.
Subject
Topic
lake levels
Subject
Topic
Holocene
Subject
Topic
late Pleistocene
Subject
Topic
North Atlantic
Subject (FAST) (authorityURI="http://id.worldcat.org/fast", valueURI="http://id.worldcat.org/fast/1051497")
Topic
Paleohydrology
Subject (FAST) (authorityURI="http://id.worldcat.org/fast", valueURI="http://id.worldcat.org/fast/1353233")
Topic
Holocene Geologic Period
Subject (FAST) (authorityURI="http://id.worldcat.org/fast", valueURI="http://id.worldcat.org/fast/1241913")
Geographic
New England
Subject (FAST) (authorityURI="http://id.worldcat.org/fast", valueURI="http://id.worldcat.org/fast/1242478")
Geographic
North Atlantic Region
Record Information
Record Content Source (marcorg)
RPB
Record Creation Date (encoding="iso8601")
20111003
Language
Language Term: Code (ISO639-2B)
eng
Language Term: Text
English
Identifier: DOI
10.7301/Z0VD6WPZ
Access Condition: rights statement (href="http://rightsstatements.org/vocab/InC/1.0/")
In Copyright
Access Condition: restriction on access
Collection is open for research.
Type of Resource (primo)
dissertations