Isotopic heterogeneity in U.S. Urban water supply systems reflects climatic, environmental, and sociodemographic factors: Implications for forensic identification.

The forensic application of stable oxygen isotope data from human tissues depends on naturally occurring isotopic variation in drinking water across geographic areas. One factor which complicates interpretation of forensic data is local variability: if a wide range of drinking water values is in a small geographic region it may be difficult to identify or rule out that region as a location of origin. We examine data from community collection programs documenting tap water isotope variation within 30 cities\developed areas throughout the United States.

Impact of Antidepressant Use on Intraoperative Blood Loss and Transfusion Rates in Lumbar Fusion Surgery.

Objective: A quarter of spine surgery patients take antidepressants. Basic science research has suggested serotonergic antidepressants impair platelet function. This has been supported by only a small number of works in the setting of spine surgery.

Resiliency among United States Air Force personnel: The direct and interactive influence of cognitive fitness and confidence in social connections.

The United States (U.S.) military has focused on increasing service members' (SM) mental and social fitness to bolster resiliency (successful role performance).

Design, development, and implementation of IsoBank: A centralized repository for isotopic data.

Stable isotope data have made pivotal contributions to nearly every discipline of the physical and natural sciences. As the generation and application of stable isotope data continues to grow exponentially, so does the need for a unifying data repository to improve accessibility and promote collaborative engagement. This paper provides an overview of the design, development, and implementation of IsoBank (www.

Long- and short-term coupling of sea surface temperature and atmospheric CO during the late Paleocene and early Eocene.

The late Paleocene and early Eocene (LPEE) are characterized by long-term (million years, Myr) global warming and by transient, abrupt (kiloyears, kyr) warming events, termed hyperthermals. Although both have been attributed to greenhouse (CO) forcing, the longer-term trend in climate was likely influenced by additional forcing factors (i.e.