ebme.marine.rutgers.edu paper…  · web viewgiven the widespread influence of lateral gene...

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Dr. Kay D. Bidle Assistant Professor x 393 Fax: 732-932-4083 [email protected] H. Jesse Smith Senior Editor Science 1200 New York Avenue NW Washington, DC 20005 202-326-6556 17 July 2006 Dear Dr. Smith, Enclosed please find a manuscript entitled “Fossil Genes and Microbes Entombed in the Oldest Ice on Earth” by Lee et al. for consideration for publication in Nature. It reports our metabolic and genetic characterization of microbes and DNA encased in extremely slow-moving debris-covered glacier ice from the Dry Valleys region of the Transantarctic Mountains. The Antarctic continent offers unique environments for understanding the limits to geological and biological preservation of life and genetic material in immobilized dormant states. We have discovered that metabolic activity and cell viability have been retained in buried ice samples spanning an ~8 million year time transect and including the oldest known ice on Earth, although they were critically compromised with age. Our molecular analyses further revealed dramatic differences in DNA integrity between these ice samples, indicating that the average DNA size declines exponentially with time with a half-life of ~2.5 million years. These data provide unprecedented insight into the preservation of environmental DNA in ice. Interestingly, our metagenomic analysis of preserved community DNA from these ancient ice samples found diverse orthologs to extant metabolic genes, making them literal “gene banks”, with deposits made when the ices formed 0.1 to ~ 8.1 My. Given the widespread influence of lateral gene transfer within microbial populations and its putative influence on the tempo of microbial evolution, one can envision pulsed periods of gene availability in environments that experience episodic periods of melting and freezing, like glaciers and pack ice, or snowball events. Hence, community DNA immobilized in Antarctic ice can be viewed as a “gene popsicle” that potentially can be acquired repaired, incorporated and used by viable microbes upon thawing. This means that such events may provide an opportunity for massive microbial gene transfers that alter metabolic potential, a R U T G E R S, T H E S T A T E U N I V E R S I T Y O F N E W J E R S E Y INSTITUTE OF MARINE & COASTAL SCIENCES 71 DUDLEY ROAD • NEW BRUNSWICK • NEW JERSEY • 08901-8521 TEL: 732-932-6555 • FAX: 732 932-8578 • URL: http://marine.rutgers.edu

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Page 1: ebme.marine.rutgers.edu Paper…  · Web viewGiven the widespread influence of lateral gene transfer within microbial populations and its putative influence on the tempo of microbial

Dr. Kay D. BidleAssistant Professor x 393Fax: [email protected]

H. Jesse SmithSenior EditorScience 1200 New York Avenue NWWashington, DC 20005202-326-6556 17 July 2006

Dear Dr. Smith,

Enclosed please find a manuscript entitled “Fossil Genes and Microbes Entombed in the Oldest Ice on Earth” by Lee et al. for consideration for publication in Nature. It reports our metabolic and genetic characterization of microbes and DNA encased in extremely slow-moving debris-covered glacier ice from the Dry Valleys region of the Transantarctic Mountains. The Antarctic continent offers unique environments for understanding the limits to geological and biological preservation of life and genetic material in immobilized dormant states. We have discovered that metabolic activity and cell viability have been retained in buried ice samples spanning an ~8 million year time transect and including the oldest known ice on Earth, although they were critically compromised with age. Our molecular analyses further revealed dramatic differences in DNA integrity between these ice samples, indicating that the average DNA size declines exponentially with time with a half-life of ~2.5 million years. These data provide unprecedented insight into the preservation of environmental DNA in ice.

Interestingly, our metagenomic analysis of preserved community DNA from these ancient ice samples found diverse orthologs to extant metabolic genes, making them literal “gene banks”, with deposits made when the ices formed 0.1 to ~ 8.1 My. Given the widespread influence of lateral gene transfer within microbial populations and its putative influence on the tempo of microbial evolution, one can envision pulsed periods of gene availability in environments that experience episodic periods of melting and freezing, like glaciers and pack ice, or snowball events. Hence, community DNA immobilized in Antarctic ice can be viewed as a “gene popsicle” that potentially can be acquired repaired, incorporated and used by viable microbes upon thawing. This means that such events may provide an opportunity for massive microbial gene transfers that alter metabolic potential, a prescient scenario given the current trends in climate change and global warming. Such events could have potentially “scrambled” microbial phylogenies several times in Earth’s history, and potentially accelerated the tempo of evolution.

Given that our results help to constrain the possible exchange of genetic material to the oceans, as well as the ability of viable microbes to traverse the solar system in comets as a potential mechanism of seeding habitable planets with life, we believe that our results will be of broad interest to Nature’s readership, including microbial ecologists, molecular biologists, geologists, and astrobiologists. Along with our on-line submission of the manuscript (~2500 words, Microsoft Word format) are: 5 figures (comprising 19 separate panels, Powerpoint format); Supplementary Information (comprising 4 tables, Tables S1-S4; Powerpoint format); and 2 supporting manuscripts in press (Levy et al. and Kowalewski et al.; PDF format), both of which are referenced in our paper. In addition, we have provided a list of suggested reviewers (below), none of who has seen this manuscript. On behalf of my co-authors and myself, I thank you for your consideration and look forward to hearing from you. Sincerely,

Kay Bidle

R U T G E R S, T H E S T A T E U N I V E R S I T Y O F N E W J E R S E Y

INSTITUTE OF MARINE & COASTAL SCIENCES 71 DUDLEY ROAD • NEW BRUNSWICK • NEW JERSEY • 08901-8521TEL: 732-932-6555 • FAX: 732 932-8578 • URL: http: //marine.rutgers.edu

Page 2: ebme.marine.rutgers.edu Paper…  · Web viewGiven the widespread influence of lateral gene transfer within microbial populations and its putative influence on the tempo of microbial

Suggested Reviewers:

Edward F. DeLongDepartment of Civil and Environmental Engineering77 Massachusetts Ave; 1-290Cambridge, MA 02139Office: 48-427Phone: (617) 253-5271email: [email protected]

David M. KarlDepartment of Oceanography1000 Pope Rd.  MSB 629University of HawaiiHonolulu, HI  96822  Phone: (808) 956-8964 Fax: (808) 956-5059e-mail:  [email protected]

Farooq AzamScripps Institution of Oceanography, UCSD9500 Gilman DriveLa Jolla CA, 92093-0202Phone: (858) 534-6850Fax: (858) 534-7313email: [email protected]

Bess B. WardDepartment of Ecology and Evolutionary BiologyPrinceton University, Princeton, NJ 08544-100Phone: (609) 258-5150Fax: 609.258.0796email: [email protected] Douglas CaponeDept. Marine Biology, AHF106University of Southern CaliforniaLos Angeles, California, 90089-0371Phone: 213-740-2772Fax: 213-740-6720email: [email protected]  David SugdenSchool of GeosciencesThe University of EdinburghGrant InstituteThe King's BuildingsWest Mains RoadEDINBURGH EH9 3JWPhone: +44 (0) 131 650 7542Fax: +44 (0) 131 668 3184email: [email protected] 

R U T G E R S, T H E S T A T E U N I V E R S I T Y O F N E W J E R S E Y