Publications
Filter Total Items: 881
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
Aftershocks illuminate the 2011 Mineral, Virginia, earthquake causative fault zone and nearby active faults Aftershocks illuminate the 2011 Mineral, Virginia, earthquake causative fault zone and nearby active faults
Deployment of temporary seismic stations after the 2011 Mineral, Virginia (USA), earthquake produced a well-recorded aftershock sequence. The majority of aftershocks are in a tabular cluster that delineates the previously unknown Quail fault zone. Quail fault zone aftershocks range from ~3 to 8 km in depth and are in a 1-km-thick zone striking ~036° and dipping ~50°SE, consistent with a...
Authors
J. Wright Horton, Anjana K. Shah, Daniel E. McNamara, Stephen L. Snyder, Aina M Carter
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
A revision of the Norian Conchostracan Zonation in North America and its implications for Late Triassic North American tectonic history A revision of the Norian Conchostracan Zonation in North America and its implications for Late Triassic North American tectonic history
Collections of Upper Triassic (Norian) conchostracans from the upper Cumnock and lower Sanford formations (North Carolina), Bull Run Formation (Virginia), Gettysburg Formation (Pennsylvania), Passaic Formation (New Jersey), Blomidon Formation (Nova Scotia), and Redonda Formation (New Mexico) have significantly expanded our knowledge of the Norian conchostracan faunas in these units...
Authors
Robert E. Weems, Spencer G. Lucas
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
Preface Preface
This book grew out of a topical session on “Central Virginia Earthquakes of 2011: Geology, Geophysics, and Significance for Seismic Hazards in Eastern North America” at the 2012 The Geological Society of America (GSA) Annual Meeting in Charlotte, North Carolina (USA). It also benefitted from related sessions at other meetings. The goal of this volume, The 2011 Mineral, Virginia...
Authors
J. Wright Horton, Martin C. Chapman, Russell A. Green
Ordovician of Germany Valley, West Virginia Ordovician of Germany Valley, West Virginia
This trip will consist of stops at five locations (Fig. 1) that provide a detailed look at the strata in a major part of the Ordovician section in Germany Valley, Pendleton County, West Virginia. At these stops, we will highlight a varied sequence of carbonate and siliciclastic strata that accumulated during the Middle to Late Ordovician, and which record changes in depositional...
Authors
John T. Haynes, Keith E. Goggin, Randall C. Orndorff, Lisa R. Goggin
Field trip guidebook for the post-meeting field trip: The Central Appalachians Field trip guidebook for the post-meeting field trip: The Central Appalachians
The lower Paleozoic rocks to be examined on this trip through the central Appalachians represent an extreme range of depositional environments. The lithofacies we will examine range from pelagic radiolarian chert and interbedded mudstone that originated on the deep floor of the Iapetus Ocean, through mud cracked supratidal dolomitic laminites that formed during episodes of emergence of...
Authors
John F. Taylor, James D. Loch, G. Robert Ganis, John E. Repetski, Charles E. Mitchell, Gale C. Blackmer, David K. Brezinski, Daniel Goldman, Randall C. Orndorff, Bryan K. Sell
The 2011 Mineral, Virginia, earthquake and its significance for seismic hazards in eastern North America: overview and synthesis The 2011 Mineral, Virginia, earthquake and its significance for seismic hazards in eastern North America: overview and synthesis
The 23 August 2011 Mw (moment magnitude) 5.7 ± 0.1, Mineral, Virginia, earthquake was the largest and most damaging in the central and eastern United States since the 1886 Mw 6.8–7.0, Charleston, South Carolina, earthquake. Seismic data indicate that the earthquake rupture occurred on a southeast-dipping reverse fault and consisted of three subevents that progressed northeastward and...
Authors
J. Wright Horton, Martin C. Chapman, Russell A. Green
Pollen and spores of terrestrial plants Pollen and spores of terrestrial plants
Pollen and spores are valuable tools in reconstructing past sea level and climate because of their ubiquity, abundance, and durability as well as their reciprocity with source vegetation to environmental change (Cronin, 1999; Traverse, 2007; Willard and Bernhardt, 2011). Pollan is found in many sedimentary environments, from freshwater to saltwater, terrestrial to marine. It can be...
Authors
Christopher E. Bernhardt, Debra A. Willard