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PubMed1989

Life on Mars: how it disappeared (if it was ever there).

The cryptoendolithic microbial community in the Ross Desert (McMurdo Dry Valleys) of Antarctica exists at temperatures significantly below the temperature optima of the primary producers. Surviving near the limit of their physiological adaptability, the organisms are under severe environmental stress, so further deterioration in the environment results in cell damage and death. The sequence of events leading to extinction is considered to be a terrestrial analog for disappearance of possible life on early Mars. Progressive stages of cell damage and death in the Ross Desert material are documented with transmission electron microscopy.

Antarctic Regions↗

PubMed1992

Testing a Mars science outpost in the Antarctic dry valleys.

Field research conducted in the Antarctic has been providing insights about the nature of Mars in the science disciplines of exobiology and geology. Located in the McMurdo Dry Valleys of southern Victoria Land (160 degrees and 164 degrees E longitude and 76 degrees 30' and 78 degrees 30' S latitude), research outposts are inhabited by teams of 4-6 scientists. We propose that the design of these outposts be expanded to enable meaningful tests of many of the systems that will be needed for the successful conduct of exploration activities on Mars. Although there are some important differences between the environment in the Antarctic dry valleys and on Mars, the many similarities and particularly the field science activities, make the dry valleys a useful terrestrial analog to conditions on Mars. Three areas have been identified for testing at a small science outpost in the dry valleys; 1) studying human factors and physiology in an isolated environment; 2) testing emerging technologies (e.g., innovative power management systems, advanced life support facilities including partial bioregenerative life support systems for water recycling and food growth, telerobotics, etc.); and 3) conducting basic scientific research that will enhance our understanding of Mars while contributing to the planning for human exploration. We suggest that an important early result of a Mars habitat program will be the experience gained by interfacing humans and their supporting technology in a remote and stressful environment.

Antarctic Regions↗

PubMed1992

History of water on Mars: a biological perspective.

We divide the history of water on the Martian surface into four epochs based upon the atmospheric temperature and pressure. In Epoch 1, during which a primordial CO2 atmosphere was actively maintained by impact and volcanic recycling, we presume the mean annual temperature to have been above freezing, the pressure to have exceeded one atmosphere, and liquid water to have been widespread. Under such conditions, similar to early Earth, life could have arisen and become abundant. After this initial period of recycling, atmospheric CO2 was irreversibly lost due to carbonate formation and the pressure and temperature declined. In Epoch II, the mean annual temperature fell below freezing but peak temperatures would have exceeded freezing. Ice covered lakes, similar to those in the McMurdo Dry Valleys of Antarctica could have provided a habitat for life. In Epoch III, the mean and peak temperatures were below freezing and there would have been only transient liquid water. Microbial ecosystems living in endolithic rock "greenhouses" could have continued to survive. Finally, in Epoch IV, the pressure dropped to near the triple point pressure of water and liquid water could no longer have existed on the surface and life on the surface would have become extinct.

Antarctic Regions↗

PubMed1992

Long-term preservation of microbial ecosystems in permafrost.

It has been established that significant numbers (up to 10 million cells per gram of sample) of living microorganisms of various ecological and morphological groups have been preserved under permafrost conditions, at temperatures ranging from -9 to -13 degrees C and depths of up to 100 m, for thousands and sometimes millions of years. Preserved since the formation of permafrost in sand-clay sediments of the Pliocene-Quaternary period and in paleosols and peats buried among them, these cells art the only living organisms that have survived for a geologically significant period of time. The complexity of the microbial community preserved varies with the age of the permafrost. Eukaryotes are found only in Holocene sediments; while prokaryotes are found to greater ages, i.e., Pliocene and Pleistocene. The diversity of microorganisms decreases with increasing age of sediments, and as a result cocci and corynebacteria are predominant. Enzyme activity (catalase and hydrolytic enzymes) and photosynthetic pigments (chlorophyll and pheophytin have also been detected in permafrost sediments. These results permit us to outline some approaches to the search for traces of life in the permafrost of Martian sediments by borehole core sampling. It is in the deep horizons (and not on the planet surface), isolated by permafrost from the external conditions, that results similar to those obtained on Earth can be expected.

Bacteria↗

PubMed1987

Behind shamanism: changing voices of Siberian Khanty cosmology and politics.

Siberian shamanism has roots in hunting traditions, kinship organization and soul beliefs which have changed under Soviet rule. Aspects of shamanic epistemology and curing survive, although native medical logic sometimes clashes with modern positivist medicine. Assumptions behind Siberian, particularly Khanty, shamanism are examined through analysis of training, seances and cosmology. The changing social context of shamanism is explored in a framework of Soviet pressure to reject shamanic 'superstitution' and 'exploration.' Shamans themselves have adapted their politics, diagnoses and symbolic actions to an increasingly cold social climate. Data results from ethno-historical and field research, including a summer 1975 trip to the Ob-Ugrian Khanty (Ostiak).

Ethnicity↗

PubMed1992

Going to extremes: the cultural context of stress, illness and coping in Antarctica.

The question of whether the concept of adaptation remains useful in medical anthropology is examined in the context of the human experience in Antarctica. This experience is characterized by prolonged isolation, confinement, and exposure to extreme environmental conditions. Men and women who winter-over at scientific research stations often exhibit a complex of psychophysiological symptoms in response to these stressors. However, this experience also appears to provide long-term health benefits. It is argued that the psychological symptoms are themselves part of the process of coping and do not necessarily represent an inability to adapt to the extreme environment. Coping is viewed as a process of negotiation leading to a compromise between individual and group needs. The cultural systems of Antarctic research stations are both a product of this negotiation and a set of normative and pragmatic rules regulating this process. Further, this process fosters the acquisition of new strategies or resources for coping with subsequent stressful experiences.

Adaptation, Psychological↗

PubMed1988

Substances with affinity to a monoclonal aflatoxin B1 antibody in Danish urine samples.

Using a competitive enzyme immunoassay, one or more substances recognized by a monoclonal antibody against aflatoxin B1 were detected in human urine samples collected in Denmark. The concentration of urinary aflatoxin-like substances was equivalent to 0.0-6.5 ng aflatoxin B1/mg creatinine. A truly competitive interaction in the immunoassay was found between aflatoxin-like substances and aflatoxin B1. Aflatoxin-like substances could be isolated in small quantities from urine by affinity chromatography. The quantity of urinary aflatoxin-like compounds in the samples collected showed a skewed normal distribution (80 individuals). In order to explain the seemingly high level of aflatoxin-like material in urine samples from people living in a cold temperate climate, the source of aflatoxin-like compounds was investigated. In a dietary restriction study, potential dietary factors leading to excretion of aflatoxin-like compounds were investigated. Our data indicate that the excretion of these compounds by healthy Danes depends mainly on the food ingested 24-48 hr before urine samples were collected. In particular, the excretion of aflatoxin-like substances was increased when diets include beer, dairy products or meat. A map of the epitope recognized by the antibody was constructed from the results of competition studies with several AFB1 analogues. The epitope map was used to draw chemical structures representing the minimal requirements for antibody recognition. An on-line search was conducted among the 98.2 x 10(6) structures in the Chemical Abstracts and Registry Databases (STN, Columbus, OH) and provided strong evidence that only aflatoxins or aflatoxin derivatives are recognized by the antibody. The possible chemical structures of the aflatoxin-like substances are discussed.

Aflatoxin B1↗

PubMed1971