Back to search

Massachusetts Institute of Technology

The redox and iron-sulfide geochemistry of Salt Pond and the thermodynamic constraints on native magnetotactic bacteria

Abstract

dc:description.abstract

Salt pond is a meromictic system with an outlet to the sea allowing denser seawater to occupy the monimolimnion while the mixolimnion has relatively low salinity and is the site of greater mixing and microbial activity. The density contrast between the two layers allows for a unique geochemical environment characterized by steep redox gradients at the interface. This chemocline is a habitat for magnetotactic bacteria (MB), and the spatial and temporal distribution of MB in the system along with geochemical (Fe2+, H2S, pH, 02 (aq), etc.) profiles have been analyzed from 2002 - 2005. It has been previously observed that magnetite-producing cocci occupy the top of the chemocline and greigite-producing MB occur at the base of the chemocline and in the sulfidic hypolimnion. This distribution may be attributed to analyte profiles within the pond; depth profiles show a sudden drop of dissolved oxygen (DO) at the chemocline associated with an increase in dissolved Fe (II) concentrations that peak where both 02 and H2S are low. In the sulfidic hypolimnion, Fe (II) concentrations decrease, suggesting buffering of Fe(II) by sulfide phases.

Degree

thesis:*
Department dc:contributor.department
Joint Program in Oceanography/Applied Ocean Science and Engineering.
Grantor dc:publisher
Massachusetts Institute of Technology
Year dc:date.issued
2006

Author and committee

dc:creator, dc:contributor.*
Author dc:creator
  • Canovas, Peter A
Advisor dc:contributor.advisor
  • Katrina J. Edwards.

Subjects

dc:subject × 3

Rights

dc:rights
Statement dc:rights
  • M.I.T. theses are protected by copyright. They may be viewed from this source for any purpose, but reproduction or distribution in any format is prohibited without written permission. See provided URL for inquiries about permission.
Language dc:language.iso
eng

Identifiers

dc:identifier.*
Handle dc:identifier.uri
http://hdl.handle.net/1721.1/38202
OAI identifier oai:identifier
oai:dspace.mit.edu:1721.1/38202

Chain of custody

source
Harvested from
MIT
Base URL
dspace.mit.edu/oai/request
Last updated
2026-07-22
Source record
OAI-PMH GetRecord
citation

Canovas, Peter A. The redox and iron-sulfide geochemistry of Salt Pond and the thermodynamic constraints on native magnetotactic bacteria. Massachusetts Institute of Technology, 2006. http://hdl.handle.net/1721.1/38202