Skip to main content Accessibility help
×
Hostname: page-component-cd9895bd7-8ctnn Total loading time: 0 Render date: 2024-12-26T01:19:08.097Z Has data issue: false hasContentIssue false

7 - The biogeochemistry and hydrology of McMurdo Dry Valley glaciers: is there life on martian ice now?

Published online by Cambridge University Press:  06 July 2010

Peter T. Doran
Affiliation:
University of Illinois, Chicago
W. Berry Lyons
Affiliation:
Ohio State University
Diane M. McKnight
Affiliation:
University of Colorado, Boulder
Get access

Summary

Introduction

Microbial life on Earth usually requires at least five prerequisites: innoculi, liquid water, and sources of energy, carbon, and nutrients (Rothschild and Manicelli,2001). One of the major advances in the cryospheric sciences during the last decade is the realization that microbial life or innoculi are found in a whole spectrum of environments throughout glacier ice masses of all scales, from the snow cover, through ice surface (or supraglacial) environments, within ice (or englacial) environments through to ice bed (or subglacial) environments (Hodson et al., 2008). A remarkable observation is that apparently viable microbes can be found throughout the whole 4 km of ice column found near the center of the East Antarctic Ice Sheet above subglacial Lake Vostok (Priscu et al., 2008). Hence, glaciers on Earth can now be regarded as biomes or ecotomes, and the question arises whether or not glaciers on other celestial bodies have the potential to act as ecotomes. This chapter begins to provide an answer by first describing how microbial life exists in the cold glaciers of the McMurdo Dry Valleys, and second, by speculating on whether or not there is the chance of life in the glaciers and ice caps of Mars. We make the assumption that potential microbial life on Mars is carbon based and requires the same five prerequisites for microbial life as on Earth (Rothschild and Manicelli, 2001).

Type
Chapter
Information
Life in Antarctic Deserts and other Cold Dry Environments
Astrobiological Analogs
, pp. 195 - 220
Publisher: Cambridge University Press
Print publication year: 2010

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Andrews-Hanna, J. C., Zuber, M. T., and Banerdt, W. B. (2008). The Borealis basin and the origin of the martian crustal dichotomy, Nature, 453, 1212–1215.CrossRefGoogle ScholarPubMed
Bagshaw, E., Tranter, M., Fountain, A., et al. (2007). The biogeochemical evolution of cryoconite holes on Canada Glacier, Taylor Valley, Antarctica. Journal of Geophysical Research, 112, G04S35, doi: 10.1029/2007JG000442.CrossRefGoogle Scholar
Bardgett, R. D. and Walker, L. R. (2004). Impact of coloniser plant species on the development of decomposer microbial communities following deglaciation. Soil Biology and Biochemistry, 36, 555–559.CrossRefGoogle Scholar
Byrne, S. and Ingersoll, A. P. (2003). A sublimation model for Martian south polar ice features. Science, 299, 1051–1053.CrossRefGoogle ScholarPubMed
Cowan, D. A. and Tow, L. A. (2004). Endangered Antarctic environments. Annual Review of Microbiology, 58, 649–690.CrossRefGoogle ScholarPubMed
Doran, P. T., McKay, C. P., Clow, G. D., et al. (2002). Valley floor climate observations from the McMurdo Dry Valleys, Antarctica, 1986–2000. Journal of Geophysical Research, Atmospheres, 107, D24.CrossRefGoogle Scholar
Foreman, C. M., Wolf, C. F., and Priscu, J. C. (2004). Impact of episodic warming events on the physical, chemical and biological relationships of lakes in the McMurdo Dry Valleys, Antarctica, Aquatic Geochemistry, 10(3), 239–268.CrossRefGoogle Scholar
Foreman, C. M., Sattler, B., Mikucki, J. A., Porazinska, D. L., and Priscu, J. C. (2007). Metabolic activity and diversity of cryoconites in the Taylor Valley, Antarctica. Journal of Geophysical Research, 112, G04S32, doi: 10.1029/2006JG000358.CrossRefGoogle Scholar
Forget, F., Haberle, R. M., Montmessin, F., Levrard, B., and Head, J. W. (2006). Formation of glaciers on Mars by atmospheric precipitation at high obliquity. Science, 311, 368–371.CrossRefGoogle ScholarPubMed
Fountain, A. G., Dana, G. L., Lewis, K. J., Vaughn, B. H., and McKnight, D. (1998). Glaciers of the McMurdo Dry Valleys, Southern Victoria Land, Antarctica. In Ecosystem Dynamics in a Polar Desert: The McMurdo Dry Valleys, Antarctica, ed. Priscu, J. C.. Antarctic Research Series 72. Washington, D.C.: American Geophysical Union, pp. 65–75.Google Scholar
Fountain, A. G., Lyons, W. B., Burkins, M. B., et al. (1999). Physical controls on the Taylor Valley ecosystem, Antarctica. BioScience, 49(12), 961–971.CrossRefGoogle Scholar
Fountain, A. G., Tranter, M., Nylen, T. H., Lewis, K. J., and Mueller, D. R. (2004). Evolution of cryoconite holes and their contribution to meltwater runoff from glaciers in the McMurdo Dry Valleys, Antarctica. Journal of Glaciology, 50(168), 35–45.CrossRefGoogle Scholar
Fountain, A. G., Nylen, T. H., Tranter, M., and Bagshaw, E. (2008). Temporal variations in physical and chemical features of cryoconite holes on Canada Glacier, McMurdo Dry Valleys, Antarctica. Journal of Geophysical Research, 113, G01S92, doi: 10.1029/2007JG000430.CrossRefGoogle Scholar
Goetz, W. and 19 others (2005). Indication of drier periods on Mars from the chemistry and mineralogy of atmospheric dust. Nature, 436, 62–65.CrossRefGoogle ScholarPubMed
Gribbon, P. W. (1979). Cryoconite holes on Sermikaysak, West Greenland. Journal of Glaciology, 22, 177–181.CrossRefGoogle Scholar
Head, J. W. (2007). The geology of Mars: new insights and outstanding questions. In The Geology of Mars: Evidence from Earth-Based Analogs, ed. Chapman, M.. Cambridge, UK: Cambridge University Press, pp. 1–46.Google Scholar
Head, J. W. and Marchant, D. R. (2003). Cold-based mountain glaciers on Mars: Western Arsia Mons. Geology, 31, 641–644.2.0.CO;2>CrossRefGoogle Scholar
Head, J. W. and Wilson, L. (2007). Heat transfer in volcano–ice interactions on Mars: synthesis of environments and implications for processes and landforms. Annals of Glaciology, 45, 1–13.CrossRefGoogle Scholar
Head, J. W., Mustard, J. F., Kreslavsky, M. A., Milliken, R. E., and Marchant, D. R. (2003). Recent ice ages on Mars. Nature, 426, 797–802.CrossRefGoogle ScholarPubMed
Hodson, A., Tranter, M., Anesio, A. M., et al. (2008). Glacial ecosystems. Ecological Monographs, 78, 41–68.CrossRefGoogle Scholar
Kennedy, A. D. (1993). Water as a limiting factor in the Antarctic terrestrial environment: a biogeographical synthesis. Arctic and Alpine Research, 25, 308–315.CrossRefGoogle Scholar
Kieffer, H. H., Christensen, P. R., and Titus, T. T. (2006). CO2 jets formed by sublimation beneath translucent slab ice in Mars' seasonal south polar ice cap. Nature, 442, 793–796.CrossRefGoogle ScholarPubMed
Killawee, J. A., Fairchild, I. J., Tison, J. -L., Janssens, L., and Lorrain, R. (1998). Segregation of solutes and gases in experimental freezing of dilute solutions: implications for natural glacial systems. Geochimica et Cosmochimica Acta, 62, 3637–3655.CrossRefGoogle Scholar
Lancaster, N. (2002). Flux of eolian sediment in the McMurdo Dry Valleys, Antarctica: a preliminary assessment. Arctic Antarctic and Alpine Research, 34, 318–323.CrossRefGoogle Scholar
Langevin, Y., Poulet, F., Bibring, J.-P., Schmitt, B., Doute, S., and Gondet, B. (2005). Summer evolution of the north polar cap of Mars as observed by OMEGA/Mars Express. Science, 307, 1581–1584.CrossRefGoogle Scholar
Lewis, K. J., Fountain, A. G., and Dana, G. L. (1999). How important is terminus cliff melt?: a study of the Canada Glacier terminus, Taylor Valley, Antarctica. Global and Planetary Change, 22(1–4), 105–115.CrossRefGoogle Scholar
Lyons, W. B., Welch, K. A., Fountain, A. G., et al. (2003). Surface glaciochemistry of Taylor Valley, southern Victoria Land, Antarctica and its relationship to stream chemistry. Hydrological Processes, 17(1), 115–130.CrossRefGoogle Scholar
Marinova, M. M., Aharonson, O., and Asphaug, E. (2008). Mega-impact formation of Mars hemispheric dichotomy. Nature, 453, 1216–1219.CrossRefGoogle ScholarPubMed
McKay, C. H., Anderson, D. T., Pollard, W. H., et al. (2005). Polar lakes, streams and springs as analogs for hydrological cycles on Mars. In Water on Mars and Life, ed. Tokano, T.. Advances in Astrobiology and Biogeophysics. Berlin: Springer-Verlag, pp. 219–233.Google Scholar
Melosh, J. H. (2008). Did an impact blast away half of the martian crust?Nature Geosciences, 1, 412–414.CrossRefGoogle Scholar
,MEPAG (Mars Exploration Program Analysis Group) (2006). Findings of the Mars Special Regions Science Analysis Group. Astrobiology, 6, 677–732.CrossRefGoogle Scholar
Mikucki, J. A. and Priscu, J. C. (2007). Bacterial diversity associated with Blood Falls, a subglacial outflow from the Taylor Glacier, Antarctica. Applied and Environmental Microbiology, 73, 4029–4039.CrossRefGoogle ScholarPubMed
Mikucki, J. A., Foreman, C. H., Sattler, B., Lyons, W. B., and Priscu, J. A. (2004). Geomicrobiology of Blood Falls: an iron rich saline discharge at the terminus of Taylor Glacier, Antarctica. Aquatic Chemistry, 10, 199–220.Google Scholar
Mindl, B., Anesio, A. M., Meirer, K., et al. (2007). Factors influencing bacterial dynamics along a transect from supraglacial runoff to proglacial lakes of a high Arctic glacier. FEMS Microbiol Ecology, 59, 307–317.CrossRefGoogle ScholarPubMed
Mueller, D. R. and Pollard, W. H. (2004). Gradient analysis of cryoconite ecosystems from two polar glaciers. Polar Biology, 27(2), 66–74.CrossRefGoogle Scholar
Muir, , H. (2008). Phoenix lander uncovers ice on Mars. New Scientist. www.newscientist.com/article/dn14143.
Nimmo, F., Hart, S. D., Korycansky, D. G., and Agnor, C. B. (2008). Implications of an impact origin for the martian hemispheric dichotomy. Nature, 453, 1220–1223.CrossRefGoogle ScholarPubMed
Nkem, J. N., Wall, D. H., Virginia, R. A., et al. (2006). Wind dispersal of soil invertebrates in the McMurdo Dry Valleys, Antarctica. Polar Biology, 29(4), 346–352.CrossRefGoogle Scholar
Nylen, T. H., Fountain, A. G., and Doran, P. T. (2004). Climatology of katabatic winds in the McMurdo dry valleys, southern Victoria Land, Antarctica. Journal of Geophysical Research, Atmospheres, 109, D3.CrossRefGoogle Scholar
Paerl, H. W. and Priscu, J. C. (1998). Microbial phototrophic, heterotrophic, and diazotrophic activities associated with aggregates in the permanent ice cover of Lake Bonney, Antarctica. Microbial Ecology, 36, 221–230.CrossRefGoogle ScholarPubMed
Plaut, J. J. and 23 others (2007). Subsurface radar sounding of the south polar layered deposits of Mars. Science, 316, 92–95.CrossRefGoogle ScholarPubMed
Porazinska, D. L., Fountain, A. G., Nylen, T. H., et al. (2004). The biodiversity and biogeochemistry of cryoconite holes from McMurdo Dry Valley glaciers, Antarctica. Arctic Antarctic and Alpine Research, 36(1), 84–91.CrossRefGoogle Scholar
Priscu, J. C. and Christner, B. C. (2002). Earth's icy biosphere. In Microbial Biodiversity and Microprospecting, ed. Bull, A.. Washington, D.C.: ASM Press, pp. 130–145.Google Scholar
Priscu, J. C., Tulaczyk, S., Studinger, M., et al. (2008). Antarctic subglacial water: origin, evolution and microbial ecology. In Polar Lakes and Rivers: Limnology of Arctic and Antarctic Aquatic Ecosystems, ed. Vincent, W. and Laybourn-Parry, J.. Oxford, UK: Oxford University Press, pp. 119–135.CrossRefGoogle Scholar
Rothschild, L. J. and Manicelli, R. L. (2001). Life in extreme environments. Nature, 409, 1092–1101.CrossRefGoogle ScholarPubMed
Säwström, C., Granéli, W., Laybourn-Parry, J., and Anesio, A. M. (2007). High viral infection rates in Antarctic and Arctic bacterioplankton. Environmental Microbiology, 9, 250–255.CrossRefGoogle ScholarPubMed
Schorghofer, N. (2007). Dynamics of ice ages on Mars. Nature, 449, 192–194.CrossRefGoogle ScholarPubMed
Stibal, M., Tranter, M., Benning, L. G., and Řehák, J. (2008). Microbial primary production on an Arctic glacier is insignificant in comparison to allochthonous organic carbon input. Environmental Microbiology, doi: 10.1111/j.1462–2920.2008.01620.CrossRef
Titus, T. N., Kieffer, H. H., and Christensen, P. R. (2003). Exposed water ice discovered near the south pole of Mars. Science, 299, 1048–1051.CrossRefGoogle ScholarPubMed
Tranter, M., Fountain, A. G., Fritsen, C. H., et al. (2004). Extreme hydrochemical conditions in natural microcosms entombed within Antarctic ice. Hydrological Processes, 18(2), 379–387.CrossRefGoogle Scholar
Tranter, M., Fountain, A. G., Lyons, W. B., Nylen, T. H., and Welch, K. A. (2005). The chemical composition of runoff from Canada Glacier, Antarctica: implications for glacier hydrology during a cool summer. Annals of Glaciology, 40, 15–19.CrossRefGoogle Scholar
Wharton, R. A., McKay, C. P., Simmons, G. M., and Parker, B. C. (1985). Cryoconite holes on glaciers. BioScience, 35(8), 499–503.CrossRefGoogle ScholarPubMed

Save book to Kindle

To save this book to your Kindle, first ensure [email protected] is added to your Approved Personal Document E-mail List under your Personal Document Settings on the Manage Your Content and Devices page of your Amazon account. Then enter the ‘name’ part of your Kindle email address below. Find out more about saving to your Kindle.

Note you can select to save to either the @free.kindle.com or @kindle.com variations. ‘@free.kindle.com’ emails are free but can only be saved to your device when it is connected to wi-fi. ‘@kindle.com’ emails can be delivered even when you are not connected to wi-fi, but note that service fees apply.

Find out more about the Kindle Personal Document Service.

Available formats
×

Save book to Dropbox

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Dropbox.

Available formats
×

Save book to Google Drive

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Google Drive.

Available formats
×