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Comparison of three preservation techniques for slowing dissolution of calcareous nannofossils in organic rich sediments Comparison of three preservation techniques for slowing dissolution of calcareous nannofossils in organic rich sediments

In an attempt to halt or reduce dissolution of calcareous nannofossils in organic and/or pyrite-rich sediments, three different methods of short-term storage preservation were tested for efficacy: vacuum packing, argon gas replacement, and buffered water. Abundance counts of calcareous nannofossil assemblages over a six month period showed that none of the three preservation methods were
Authors
Ellen Seefelt, Jean Self-Trail, Arthur P. Schultz

Modelling the enigmatic Late Pliocene Glacial Event - Marine Isotope Stage M2 Modelling the enigmatic Late Pliocene Glacial Event - Marine Isotope Stage M2

The Pliocene Epoch (5.2 to 2.58 Ma) has often been targeted to investigate the nature of warm climates. However, climate records for the Pliocene exhibit significant variability and show intervals that apparently experienced a cooler than modern climate. Marine Isotope Stage (MIS) M2 (~ 3.3 Ma) is a globally recognisable cooling event that disturbs an otherwise relatively (compared to...
Authors
Aisling M. Dolan, Alan M. Haywood, Stephen J. Hunter, Julia C. Tindall, Harry J. Dowsett, Daniel J. Hill, Steven J. Pickering

Testing a small UAS for mapping artisanal diamond mining sites in Africa Testing a small UAS for mapping artisanal diamond mining sites in Africa

Remote sensing technology is advancing at an unprecedented rate. At the forefront of the new technological developments are unmanned aircraft systems (UAS). The advent of small, lightweight, low-cost, and user-friendly UAS is greatly expanding the potential applications of remote sensing technology and improving the set of tools available to researchers seeking to map and monitor terrain...
Authors
Katherine C. Malpeli, Peter G. Chirico

Biological indicators of changes in water quality and habitats of the coastal and estuarine areas of the Greater Everglades Ecosystem; Chapter 11 Biological indicators of changes in water quality and habitats of the coastal and estuarine areas of the Greater Everglades Ecosystem; Chapter 11

This chapter summarizes the application of various biological indicators to studying the anthropogenic and natural changes in water quality and habitats that have occurred in the coastal and estuarine areas of the Greater Everglades ecosystem.
Authors
Anna Wachnicka, G. Lynn Wingard

Geotechnical aspects in the epicentral region of the 2011, Mw5.8 Mineral, Virginia earthquake Geotechnical aspects in the epicentral region of the 2011, Mw5.8 Mineral, Virginia earthquake

A reconnaissance team documented the geotechnical and geological aspects in the epicentral region of the Mw (moment magnitude) 5.8 Mineral, Virginia (USA), earthquake of 23 August 2011. Tectonically and seismically induced ground deformations, evidence of liquefaction, rock slides, river bank slumps, ground subsidence, performance of earthen dams, damage to public infrastructure and...
Authors
Russell A. Green, Samuel Lasley, Mark W. Carter, Jeffrey W. Munsey, Brett W. Maurer, Martitia P. Tuttle

Evidence for large compositional ranges in coeval melts erupted from Kīlauea's summit reservoir Evidence for large compositional ranges in coeval melts erupted from Kīlauea's summit reservoir

Petrologic observations on Kīlauea's lavas include abundant microprobe analyses of glasses, which show the range of melts available in Kīlauea's summit reservoir over time. During the past two centuries, compositions of melts erupted within the caldera have been limited to MgO = 6.3–7.5 wt%. Extracaldera lavas of the 1959, 1971, and 1974 eruptions contain melts with up to 10.2, 8.9, and...
Authors
Rosalind T. Helz, David A. Clague, Larry G. Mastin, Timothy R. Rose

High influx of carbon in walls of agglutinated foraminifers during the Permian-Triassic transition in global oceans High influx of carbon in walls of agglutinated foraminifers during the Permian-Triassic transition in global oceans

The Permian–Triassic mass extinction is postulated to be related to the rapid volcanism that produced the Siberian flood basalt (Traps). Unrelated volcanic eruptions producing several episodes of ash falls synchronous with the Siberian Traps are found in South China and Australia. Such regional eruptions could have caused wildfires, burning of coal deposits, and the dispersion of coal...
Authors
Galina P. Nestell, Merlynd K. Nestell, Brooks B. Ellwood, Bruce R. Wardlaw, Asish R. Basu, Nilotpal Ghosh, Luu Thi Phuong Lan, Harry D. Rowe, Andrew G. Hunt, Jonathan H. Tomkin, Kenneth T. Ratcliffe

Taxonomic revision of deep-sea Ostracoda from the Arctic Ocean Taxonomic revision of deep-sea Ostracoda from the Arctic Ocean

Taxonomic revision of deep-sea Ostracoda from the Arctic Ocean was conducted to reduce taxonomic uncertainty that will improve our understanding of species ecology, biogeography and relationship to faunas from other deep-sea regions. Fifteen genera and 40 species were examined and (re-)illustrated with high-resolution scanning electron microscopy images, covering most of known deep-sea...
Authors
Moriaki Yasuhara, Anna Stepanova, Hisayo Okahashi, Thomas M. Cronin, Elisabeth M. Brouwers

An early to mid-Pleistocene deep Arctic Ocean ostracode fauna with North Atlantic affinities An early to mid-Pleistocene deep Arctic Ocean ostracode fauna with North Atlantic affinities

An early to middle Pleistocene ostracode fauna was discovered in sediment core P1-93-AR-23 (P23, 76.95°N, 155.07°W) from 951 meter water depth from the Northwind Ridge, western Arctic Ocean. Piston core P23 yielded more than 30,000 specimens and a total of about 30 species. Several early to mid-Pleistocene species in the genera Krithe,Echinocythereis, Pterygocythereis, and Arcacythere...
Authors
Lauren H. DeNinno, Thomas M. Cronin, J. Rodriquez-Lazaro, Alec R. Brenner

Instrumenting caves to collect hydrologic and geochemical data: case study from James Cave, Virginia Instrumenting caves to collect hydrologic and geochemical data: case study from James Cave, Virginia

Karst aquifers are productive groundwater systems, supplying approximately 25 % of the world’s drinking water. Sustainable use of this critical water supply requires information about rates of recharge to karst aquifers. The overall goal of this project is to collect long-term, high-resolution hydrologic and geochemical datasets at James Cave, Virginia, to evaluate the quantity and...
Authors
Madeline E. Schreiber, Benjamin F. Schwartz, William Orndorff, Daniel H. Doctor, Sarah D. Eagle, Jonathan D. Gerst

Thermokarst lake methanogenesis along a complete talik profile Thermokarst lake methanogenesis along a complete talik profile

Thermokarst (thaw) lakes emit methane (CH4) to the atmosphere formed from thawed permafrost organic matter (OM), but the relative magnitude of CH4 production in surface lake sediments vs. deeper thawed permafrost horizons is not well understood. We assessed anaerobic CH4 production potentials from various depths along a 590 cm long lake sediment core that captured the entire sediment...
Authors
J.K. Heslop, K.M. Walter Anthony, A. Sepulveda-Jauregui, K. Martinez-Cruz, A. Bondurant, G. Grosse, Miriam C. Jones

Hydrologic and geochemical dynamics of vadose zone recharge in a mantled karst aquifer: Results of monitoring drip waters in Mystery Cave, Minnesota Hydrologic and geochemical dynamics of vadose zone recharge in a mantled karst aquifer: Results of monitoring drip waters in Mystery Cave, Minnesota

Caves provide direct access to flows through the vadose zone that recharge karst aquifers. Although many recent studies have documented the highly dynamic processes associated with vadose zone flows in karst settings, few have been conducted in mantled karst settings, such as that of southeastern Minnesota. Here we present some results of a long-term program of cave drip monitoring...
Authors
Daniel H. Doctor, E. Calvin Alexander, Roy A. Jameson, Scott C. Alexander
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