Sulfur Cycling in the Cariaco Basin and the Meromictic Green Lake in Fayetteville, New York
<p> An imbalance in the flux of oxidants and reductants to the suboxic zone (which lies between layers containing oxygen (O<sub>2</sub>) and hydrogen sulfide (H<sub>2</sub>S)) has been observed in many anoxic basins. These basins also have high levels of chemoautotrophy...
Main Author: | Butler, Kristen Ann |
---|---|
Language: | EN |
Published: |
State University of New York at Stony Brook
2018
|
Subjects: | |
Online Access: | http://pqdtopen.proquest.com/#viewpdf?dispub=10622596 |
Similar Items
-
Vertical structure of the bacterial diversity in meromictic Fayetteville Green Lake
by: Kaleigh R. Block, et al.
Published: (2021-08-01) -
Cycling of reduced trace gases and hydroxylamine in coastal waters
by: Butler, James H.
Published: (2012) - The Biogeochemical Cycle of Mercury in the Northern Gulf of Mexico as Constrained by Carbon, Nitrogen, Sulfur, and Mercury Isotopic Ratios in Marine Fish
- Carbon Biogeochemistry of Pristine and Impacted Catchments of the Congo Basin
-
Phototropic sulfur and sulfate-reducing bacteria in the chemocline of meromictic Lake Cadagno, Switzerland
by: Raffaele PEDUZZI, et al.
Published: (2004-08-01)