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Holocene History Of The East Antarctic Ice Sheet Environmental Magnetic Record From Mac. Robertson Land, Kenneth R. Kacperowski Jr.

Theses, Dissertations and Culminating Projects

A 24-m jumbo-piston core containing a 14 ka Holocene-Late Pleistocene sedimentary record was collected from Mac.Robertson Land during United States Antarctic Program cruise NBP01-01. This study uses environmental magnetism to trace the Holocene history of the East Antarctic Ice Sheet (EAIS), which is generally thought of as stable since it is grounded above sea level. Magnetic analyses are used to identify periods of terrigenous sedimentation from the EAIS, for example ice rafted debris layers or meltwater pulses. Terrigenous material contains magnetic minerals, which we expect to stand out from the dominantly biosiliceous sediment deposited along the East Antarctic Margin. Magnetic …

Paleoenvironment And Paleoclimate Of Coastal East Antarctica During The Middle Miocene : Particle Size Results Of The Andrill Southern Mcmurdo Sound Project, Candice Joy Falk

Theses, Dissertations and Culminating Projects

The ANDRILL Southern McMurdo Sound (SMS) Project was carried out in December of 2007 by an international interdisciplinary team. The AND-2A core recovered the most complete Neogene stratigraphic record from Antarctica, spanning the past 20.2 million years. Analyzing particle size distributions of samples throughout the core can determine environmental conditions of the past, such as the advance or retreat of glaciers and the rise and fall of sea level. Over 300 samples were taken at approximately 3 m intervals from the 1138.54 m AND-2A core. Samples were processed and analyzed using a Malvern Instruments Mastersizer 2000, laser diffractometer which has …

Monitoring Protocol For Two New Jersey Ponds With Littoral Zone Vegetative Restoration, Michael Wilson

Theses, Dissertations and Culminating Projects

Restoration projects are becoming more frequent and commonplace because of increased regulations on development to replace lost ecosystems. Many of these projects have marginal success and rarely achieve the desired results. The mistakes and oversights are sometimes in the planning stages, but more often are made during the installation, primarily due to improper horticultural technique, poor monitoring, education, or lack of follow-up maintenance. Wetland restoration is even more difficult, due to the variable hydrologic patterns and reliance on environmental conditions. The most difficult type of wetland plant to establish is the emergent aquatic that typically grows in water up to …

Ridge Subduction Volcanism In The Zeballos Complex, Southern Patagonian Andes, Michael Joseph Dasilva

Theses, Dissertations and Culminating Projects

The Zeballos Complex (47.0°S, 71.4°W) lies on the western side of Meseta del Lago Buenos Aires (MLBA) in the southern Andean backarc region, southeast of the Chile Triple Junction and east of ridge collision that occurred at 6 Ma. The Zeballos Complex is a bimodal, alkaline volcanic complex consisting of multiple lava flows, dikes, volcanic necks, and sub-volcanic intrusives that range from basalt to trachybasalt (47-50% SiO₂; 5-7% Na₂O+K₂O; 3-7% MgO) to highly differentiated trachyandesite, trachydacite, and trachyte (58-65% SiO₂; 8-12% Na₂O+K₂O). Intermediate compositions are relatively rare, but …

A Sedimentary Investigation Of Lineation Patterns Found In The Pinelands Of New Jersey, Jennifer Lynn Lapoma

Theses, Dissertations and Culminating Projects

Late Pleistocene (-15,000 years ago) geomorphic processes in the Pinelands of southern New Jersey were investigated after odd lineations were found on an Electromagnetic Induction (EMI) survey during the construction of a runway expansion at Lakehurst Naval Air Engineering Station. These lineations roughly matched up with alternating high and low albedo lineations identified on a 1931 aerial photomosaic approximately 17 kilometer (km) south of Lakehurst Navy Base in Davensport Branch, New Jersey. These lineations were initially hypothesized to be relicts from strong katabic winds flowing off the Laurentide Ice Sheet that would have been capable of winnowing magnetic sands from …

Geochemical And Petrographic Signatures From Marie Byrd Land And Larsen-B Ice Shelf Sediments : Implications For Provenance Tracing, Cathleen Lauren Dale

Theses, Dissertations and Culminating Projects

The goal of this study is to trace ice rafted debris in the Southern Ocean back to its most probable terrestrial source from the West Antarctic Ice Sheet (WAIS), East Antarctic Ice Sheet (EAIS), or the Antarctic Peninsula Ice Cap (APIC) in order to identify past ice sheet collapses in the geologic record. The bedrock in these areas have characteristic petrographic and geochemical signatures that are preserved in glacially transported and deposited sediment. These signatures may allow us to identify ice rafted debris and fine-grained sediment that originate from these three areas, which have undergone recent ice shelf retreat and …

Stratigraphy And Geochemistry Of Squantum Tillite, Boston Bay Group : Using Field Log And Icp Analysis, Efe Junior Erukanure

Theses, Dissertations and Culminating Projects

The Squantum Tillite has been studied in order to ascertain its depositional history. The Squantum Tillite is part of the Neoproterozoic Boston Bay Group, located in the Boston Basin. Researchers have proposed contradicting hypotheses about the origin of the rocks in the area for over a century. While some believe that the rocks were deposited by glaciers along a prograding submarine margin, others believe the rocks are of volcanic or tectonic origin. Many scientists are inclined to believe the rocks are of tectonic origin because the Squantum Tillite is located in a tectonic Basin (the Boston Basin).

Field logging was …