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Book Series
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Availability
Barnstable County Massachusetts
Investigation of Scale-Dependent Groundwater/Surface-water Exchange in Rivers by Gradient Self-Potential Logging: Numerical Modeling and Field Experiments Available to Purchase
Combined Impacts of Ocean Acidification and Dysoxia On Survival and Growth of Four Agglutinating Foraminifera Available to Purchase
Stochastic Models of Solute Transport in Highly Heterogeneous Geologic Media All rights reserved. No part of this periodical may be reproduced or transmitted in any form or by any means, electronic or mechanical, including photocopying, recording, or any information storage and retrieval system, without permission in writing from the publisher. Available to Purchase
Induced-polarization detection and mapping of contaminant plumes Available to Purchase
Effects of spatially variable resolution on field-scale estimates of tracer concentration from electrical inversions using Archie's law Available to Purchase
Validity of the Generalized Richards Equation for the Analysis of Pumping Test Data for a Coarse-Material Aquifer Contribution of the Department of Geology and Geophysics and Water Resources Research Center, University of Hawai‘i, Honolulu, HI. WRRC Contributed Paper CP-2005-01. Available to Purchase
Optical dating of dune sand for the study of sea-level change Available to Purchase
Influence of relative sea-level change and tidal-inlet development on barrier-spit stratigraphy, Sandy Neck, Massachusetts Available to Purchase
Salinity control on the distribution of salt marsh foraminifera (Great Marshes, Massachusetts) Available to Purchase
Earthquake Recurrence Rates in the Central Atlantic United States Available to Purchase
Development of Parabolic Dunes and Interdunal Wetlands in the Provincelands, Cape Cod National Seashore Available to Purchase
Abstract The Provincelands in the Cape Cod National Seashore developed about 5 ka from wind- and waterborne Outer Cape Cod outwash sands as sea level rose to submerge offshore banks. A late Holocene chronology of sand dunes in the Provincelands is established from radiocarbon-age determinations on the basal organics from interdunal bogs and ponds. The Provincelands ponds, thought to be lakes trapped behind hooked spits, are shown here to have developed from bogs similar to those in the extant parabolic-dune field. An older, stabilized dune field in the location of the ponds is hypothesized. Episodes of alternating dune movement and interdunal-wetland formation in the Provincelands correlate with climatic changes in the North Atlantic and elsewhere during the last 1.2 ka, as interpreted from ice core, glacier movement, sea-surface temperature, tree-ring, pollen, and historical data. The dune field data suggest a periodicity of change of 0.2 ka. Before about 1.2 ka, dunes in the Provincelands were active. Between about 1.15 and 0.9 ka, bogs formed which, at least in the west-central area of the Provincelands, developed into ponds having continuous organic sedimentation until today. This evidence indicates that the west-central dune field stabilized after 1.1 ka. Between 0.9 and 0.7 ka, dunes were active in the north and east-central Provincelands, but from about 0.7 to 0.5 ka, bogs formed within that dune field, and at least one bog in the west-central area became a pond, both events indicating a warm and wet climate. During the Little Ice Age (0.5 to ∼0.2-0.1 ka), the Provincelands dunes were active, suggesting a cold, windy, and dry climate. Because of a warmer and wetter climate during the last 0.1 ka, bogs have formed again within the dunes.