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Geochemical characteristics of Holocene laminated sapropel (unit II) and underlying lacustrine unit III in the Black Sea Geochemical characteristics of Holocene laminated sapropel (unit II) and underlying lacustrine unit III in the Black Sea

eg 1 of the 1988 R/V Knorr expeditions to the Black Sea recovered 90 gravity and box cores. The longest recovery by gravity cores was about 3 meters, with an average of about 2.5 meters, recovering all of the Holocene and upper Pleistocene sections in the Black Sea. During the latest Pleistocene glaciation, sea level dropped below the 35-meters-deep Bosporus outlet sill of the Black Sea...
Authors
Walter E. Dean, Michael A. Arthur

Investigating and managing the rapid emergence of white-nose syndrome, a novel, fatal, infectious disease of hibernating bats Investigating and managing the rapid emergence of white-nose syndrome, a novel, fatal, infectious disease of hibernating bats

White-nose syndrome (WNS) is a fatal disease of bats that hibernate. The etiologic agent of WNS is the fungus Geomyces destructans, which infects the skin and wing membranes. Over 1 million bats in six species in eastern North America have died from WNS since 2006, and as a result several species of bats may become endangered or extinct. Information is lacking on the pathogenesis of G...
Authors
Janet Foley, Deana Clifford, Kevin Castle, Paul M. Cryan, Richard S. Ostfeld

Alternative states of a semiarid grassland ecosystem: implications for ecosystem services Alternative states of a semiarid grassland ecosystem: implications for ecosystem services

Ecosystems can shift between alternative states characterized by persistent differences in structure, function, and capacity to provide ecosystem services valued by society. We examined empirical evidence for alternative states in a semiarid grassland ecosystem where topographic complexity and contrasting management regimes have led to spatial variations in levels of livestock grazing...
Authors
Mark E. Miller, R. Travis Belote, Matthew A. Bowker, Steven L. Garman

U.S. Geological Survey development of a Landsat-based Fire Disturbance ECV U.S. Geological Survey development of a Landsat-based Fire Disturbance ECV

The United States Geological Survey (USGS) is the steward of the Landsat archive which includes satellite imagery dating back to 1972. The United Nations Framework Convention on Climate Change and the Intergovernmental Panel on Climate Change have specified requirements to systematically observe atmosphere, ocean, and land characteristics, or Essential Climate Variables (ECVs). The...
Authors
Susan Stitt, John D. Guthrie, Todd Hawbaker, Mary S. Dolhancey

Responses of wind erosion to climate-induced vegetation changes on the Colorado Plateau Responses of wind erosion to climate-induced vegetation changes on the Colorado Plateau

Projected increases in aridity throughout the southwestern United States due to anthropogenic climate change will likely cause reductions in perennial vegetation cover, which leaves soil surfaces exposed to erosion. Accelerated rates of dust emission from wind erosion have large implications for ecosystems and human well-being, yet there is poor understanding of the sources and magnitude...
Authors
Seth M. Munson, Jayne Belnap, Gregory S. Okin

Sea-level history of the past two interglacial periods: New evidence from U-series dating of reef corals from south Florida Sea-level history of the past two interglacial periods: New evidence from U-series dating of reef corals from south Florida

As a future warm-climate analog, much attention has been directed to studies of the Last Interglacial period or marine isotope substage (MIS) 5.5, which occurred ∼120,000 years ago. Nevertheless, there are still uncertainties with respect to its duration, warmth and magnitude of sea-level rise. Here we present new data from tectonically stable peninsular Florida and the Florida Keys that...
Authors
Daniel R. Muhs, Kathleen Simmons, R. Randall Schumann, R. B. Halley

Recent surface temperature trends in the interior of East Antarctica from borehole firn temperature measurements and geophysical inverse methods Recent surface temperature trends in the interior of East Antarctica from borehole firn temperature measurements and geophysical inverse methods

We use measured firn temperatures down to depths of 80 to 90 m at four locations in the interior of Dronning Maud Land, East Antarctica to derive surface temperature histories spanning the past few decades using two different inverse methods. We find that the mean surface temperatures near the ice divide (the highest‐elevation ridge of East Antarctic Ice Sheet) have increased...
Authors
A. Muto, T. A. Scambos, K. Steffen, A.G. Slater, Gary D. Clow

Sea ice loss enhances wave action at the Arctic coast Sea ice loss enhances wave action at the Arctic coast

Erosion rates of permafrost coasts along the Beaufort Sea accelerated over the past 50 years synchronously with Arctic‐wide declines in sea ice extent, suggesting a causal relationship between the two. A fetch‐limited wave model driven by sea ice position and local wind data from northern Alaska indicates that the exposure of permafrost bluffs to seawater increased by a factor of 2.5...
Authors
I. Overeem, R. Scott Anderson, C.W. Wobus, Gary D. Clow, Frank E. Urban, N. Matell

The angus mammoth: A decades-old scientific controversy resolved The angus mammoth: A decades-old scientific controversy resolved

The Angus Mammoth site in south-central Nebraska has been controversial since its discovery in 1931 when a fluted artifact was reported to be associated with the mammoth. For nearly 80 years it has not been known if Angus was a paleontological site predating the human occupation of North America as has been asserted by some geologists and paleontologists, or an archaeological site dating...
Authors
Steven R. Holen, D.W. May, Shannon A. Mahan

Cosmogenic nuclide and uranium-series dating of old, high shorelines in the western Great Basin, USA Cosmogenic nuclide and uranium-series dating of old, high shorelines in the western Great Basin, USA

Closed-basin pluvial lakes are sensitive recorders of effective moisture, and they provide a terrestrial signal of climate change that can be compared to marine and ice records of glacial-interglacial cycles. Although the most recent deep-lake cycle in the western Great Basin (at ca. 16 ka) has been studied intensively, comparatively little is known about the longer-term Quaternary...
Authors
G. Kurth, F. M. Phillips, Marith C. Reheis, J.L. Redwine, James B. Paces

New optically stimulated luminescence ages provide evidence of MIS3 and MIS2 eolian activity on Black Mesa, northeastern Arizona, USA New optically stimulated luminescence ages provide evidence of MIS3 and MIS2 eolian activity on Black Mesa, northeastern Arizona, USA

Eolian deposition on the semiarid southern Colorado Plateau has been attributed to episodic aridity during the Quaternary Period. However, OSL ages from three topographically controlled (e.g. falling) dunes on Black Mesa in northeastern Arizona indicate that eolian sediments there were deposited in deep tributary valleys as early as 35–30 ka, with most sand deposited before 20 ka. In...
Authors
A.L. Ellwein, Shannon A. Mahan, L. D. McFadden

Late Pliocene and Quaternary Eurasian locust infestations in the Canary Archipelago Late Pliocene and Quaternary Eurasian locust infestations in the Canary Archipelago

The Canary Archipelago has long been a sensitive location to record climate changes of the past. Interbedded with its basalt lavas are marine deposits from the principal Pleistocene interglacials, as well as aeolian sands with intercalated palaeosols. The palaeosols contain African dust and innumerable relict egg pods of a temperate‐region locust (cf. Dociostaurus maroccanusThunberg 1815...
Authors
J. Meco, D.R. Muhs, M. Fontugne, A.J. Ramos, A. Lomoschitz, D. Patterson
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