Note to users. If you're seeing this message, it means that your browser cannot find this page's style/presentation instructions -- or possibly that you are using a browser that does not support current Web standards. Find out more about why this message is appearing, and what you can do to make your experience of our site the best it can be.
A Serpentinite-Hosted Ecosystem: The Lost City Hydrothermal Field
Deborah S. Kelley,1*Jeffrey A. Karson,2Gretchen L. Früh-Green,3Dana R. Yoerger,4Timothy M. Shank,4David A. Butterfield,5John M. Hayes,4Matthew O. Schrenk,1Eric J. Olson,1Giora Proskurowski,1Mike Jakuba,6Al Bradley,4Ben Larson,1Kristin Ludwig,1Deborah Glickson,1Kate Buckman,4Alexander S. Bradley,7William J. Brazelton,1Kevin Roe,5Mitch J. Elend,1Adélie Delacour,3Stefano M. Bernasconi,3Marvin D. Lilley,1John A. Baross,1Roger E. Summons,7Sean P. Sylva4
The serpentinite-hosted Lost City hydrothermal field is a remarkablesubmarine ecosystem in which geological, chemical, and biologicalprocesses are intimately interlinked. Reactions between seawaterand upper mantle peridotite produce methane- and hydrogen-richfluids, with temperatures ranging from <40° to 90°Cat pH 9 to 11, and carbonate chimneys 30 to 60 meters tall.A low diversity of microorganisms related to methane-cyclingArchaea thrive in the warm porous interiors of the edifices.Macrofaunal communities show a degree of species diversity atleast as high as that of black smoker vent sites along the Mid-AtlanticRidge, but they lack the high biomasses of chemosynthetic organismsthat are typical of volcanically driven systems.
1 School of Oceanography, University of Washington, Seattle, WA 98195, USA. 2 Division of Earth and Ocean Sciences, Duke University, Durham, NC 27708, USA. 3 Department of Earth Sciences, ETH-Zentrum, Zurich, Switzerland. 4 Woods Hole Oceanographic Institution (WHOI), Woods Hole, MA 02543, USA. 5 Joint Institute for the Study of the Atmosphere and Ocean, University of Washington, and National Oceanic and Atmospheric Administration Pacific Marine Environmental Laboratory, Seattle WA 98115, USA. 6 MIT/WHOI Joint Program, WHOI, Woods Hole MA 02543, USA. 7 Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge MA 02139, USA.
* To whom correspondence should be addressed. E-mail: kelley{at}ocean.washington.edu
The editors suggest the following Related Resources on Science sites:
In Science Magazine
PERSPECTIVES
Antje Boetius (4 March 2005) Science307 (5714), 1420.
[DOI: 10.1126/science.1109849] |Summary »|Full Text »|PDF »
THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
Genome beginnings: rooting the tree of life.
J. A. Lake, R. G. Skophammer, C. W. Herbold, and J. A. Servin (2009)
Phil Trans R Soc B
364, 2177-2185
|Abstract »|Full Text »|PDF »
Strong Release of Methane on Mars in Northern Summer 2003.
M. J. Mumma, G. L. Villanueva, R. E. Novak, T. Hewagama, B. P. Bonev, M. A. DiSanti, A. M. Mandell, and M. D. Smith (2009)
Science
323, 1041-1045
|Abstract »|Full Text »|PDF »
Fe-Ni-Co-O-S Phase Relations in Peridotite-Seawater Interactions.
Formation of replacement dolomite in the Latemar carbonate buildup, Dolomites, northern Italy: Part 2. Origin of the dolomitizing fluid and the amount and duration of fluid flow.
Abiogenic Hydrocarbon Production at Lost City Hydrothermal Field.
G. Proskurowski, M. D. Lilley, J. S. Seewald, G. L. Fruh-Green, E. J. Olson, J. E. Lupton, S. P. Sylva, and D. S. Kelley (2008)
Science
319, 604-607
|Abstract »|Full Text »|PDF »
On the origin of biochemistry at an alkaline hydrothermal vent.
From the Cover: Extreme accumulation of nucleotides in simulated hydrothermal pore systems.
P. Baaske, F. M. Weinert, S. Duhr, K. H. Lemke, M. J. Russell, and D. Braun (2007)
PNAS
104, 9346-9351
|Abstract »|Full Text »|PDF »
Techniques for Deep Sea Near Bottom Survey Using an Autonomous Underwater Vehicle.
D. R. Yoerger, M. Jakuba, A. M. Bradley, and B. Bingham (2007)
The International Journal of Robotics Research
26, 41-54
|Abstract »|PDF »
Inaugural Article: Organic haze on Titan and the early Earth.
M. G. Trainer, A. A. Pavlov, H. L. DeWitt, J. L. Jimenez, C. P. McKay, O. B. Toon, and M. A. Tolbert (2006)
PNAS
103, 18035-18042
|Abstract »|Full Text »|PDF »
Methane- and Sulfur-Metabolizing Microbial Communities Dominate the Lost City Hydrothermal Field Ecosystem.
W. J. Brazelton, M. O. Schrenk, D. S. Kelley, and J. A. Baross (2006)
Appl. Envir. Microbiol.
72, 6257-6270
|Abstract »|Full Text »|PDF »
Evidence that the Root of the Tree of Life Is Not within the Archaea.
R. G. Skophammer, C. W. Herbold, M. C. Rivera, J. A. Servin, and J. A. Lake (2006)
Mol. Biol. Evol.
23, 1648-1651
|Abstract »|Full Text »|PDF »
M. J. Russell and A. J. Hall (2006)
Geological Society of America Memoirs
198, 1-32
|Abstract »|Full Text »|PDF »
Desulfotomaculum and Methanobacterium spp. Dominate a 4- to 5-Kilometer-Deep Fault.
D. P. Moser, T. M. Gihring, F. J. Brockman, J. K. Fredrickson, D. L. Balkwill, M. E. Dollhopf, B. S. Lollar, L. M. Pratt, E. Boice, G. Southam, et al. (2005)
Appl. Envir. Microbiol.
71, 8773-8783
|Abstract »|Full Text »|PDF »
Building the Biomarker Tree of Life.
J. J. Brocks and A. Pearson (2005)
Reviews in Mineralogy and Geochemistry
59, 233-258
|Full Text »|PDF »