E
Edward A. Boyle
Researcher at Massachusetts Institute of Technology
Publications - 235
Citations - 32295
Edward A. Boyle is an academic researcher from Massachusetts Institute of Technology. The author has contributed to research in topics: Seawater & North Atlantic Deep Water. The author has an hindex of 92, co-authored 229 publications receiving 30131 citations. Previous affiliations of Edward A. Boyle include Heidelberg University & Singapore–MIT alliance.
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Last Glacial Maximum paleochemistry and deepwater circulation in the Southern Ocean: Evidence from foraminiferal cadmium
TL;DR: In this paper, the South Atlantic benthic foraminiferal Cd/Ca shows no glacial-interglacial variation, suggesting that the glacial contribution of North Atlantic Deep Water to the Southern Ocean was not much different than at present.
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Barium in planktonic foraminifera
David W. Lea,Edward A. Boyle +1 more
TL;DR: In this article, a series of cores were purified of non-lattice-bound Ba associated with organic or sedimentary phases by a combination of physical agitation, oxidative-reductive steps, acid leaches, and a novel alkaline-DTPA step to dissolve barite.
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Rhenium in the Black Sea: comparison with molybdenum and uranium
TL;DR: In this article, a simple two-box model is used to demonstrate that Re concentrations in the Black Sea are not in steady state with respect to current riverine inputs and authigenic fluxes, suggesting that these elements are scavenged either in the water column or slope sediments to a greater degree than U.
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Dissolved zinc in rivers
Alan M. Shiller,Edward A. Boyle +1 more
TL;DR: In this paper, the concentrations of dissolved zinc in rivers were analyzed by using a method similar to the one used for oceanic data for other metals, and it was shown that in relatively undisturbed systems dissolved zinc concentrations are typically only 10−9−10−8−8 mol kg−1, with some dependence of concentration on pH.
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Cool tropical temperatures shift the global δ18O‐T relationship: An explanation for the ice core δ18O ‐ borehole thermometry conflict?
TL;DR: In this paper, the discrepancy between central Greenland borehole temperatures and the isotopic composition of Last Glacial Maximum ice can be explained by a shift in the •5180-T relationship for the hydrological cycle linked to cooler tropical temperatures.