Julie Trotter

TL;DR: In this paper, the authors argue that ocean acidification from anthropogenic CO2 emissions is largely an open ocean syndrome and that a concept of anthro- pogenic impacts on marine pH, which is applicable across the entire ocean, from coastal to open-ocean environments, provides a superior framework to consider the multiple components of the anthropogenic perturbation of marine pH trajectories.

TL;DR: A favorable climate regime implies not only that the oxygen isotopic composition of Ordovician seawater was similar to that of today, but also that climate played an overarching role in promoting the unprecedented increases in biodiversity that characterized this period.

TL;DR: It is shown how scleractinian corals up-regulate pH at their site of calcification such that internal changes are approximately one-half of those in ambient seawater, thereby increasing calcification rates at little additional energy cost.

TL;DR: The overwhelming majority of applied Zn was not absorbed, although blood and urine samples from all subjects exhibited small increases in levels of tracer (68)Zn, and stable isotope tracing allowed dermally absorbed zinc to be distinguished from naturally occurring zinc.

TL;DR: In this paper, the boron isotope systematics for azooxanthellate scleractinian corals from a wide range of both deep-sea and shallow-water environments were determined.