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Electroneurobiología

ISSN: ONLINE 1850-1826 - PRINT 0328-0446

 

 

Modern Myths Concerning Life on Mars

 

by

 

 

Gilbert V. Levin*

BioSpherix Division, Spherix Incorporated, Annapolis, MD 21401, USA

Contact: glevin@spherix.com; phone 410-224-3319; fax 410-224-3010

 

 

Electroneurobiología 2006; 14 (5), pp. 3-25; URL <http://electroneubio.secyt.gov.ar/index2.htm>

 

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Table of Contents

1. Introduction

2. The Standard Model

3. The Viking Labeled Release Experiment

4. The LR Pedigree

5. The LR on Mars

6. The Standard Model Specific Obstacles Raised and Rebuttals

7. The Present Situation

8. Future Life Detection Experiments

9. Recommendations

 

 

ABSTRACT: July 30, 2006 was the 30th anniversary of the Viking Mission’s first Labeled Release (LR) life detection experiment on Mars.  The strong response, together with supporting results from eight additional LR tests of Martian soil, established the presence of an active agent that was inhibited by heating.  The data satisfied the pre-mission criteria for the detection of living microorganisms.  However, the scientific community reacted cautiously, generally concluding that the activity in the soil was caused by chemistry or physics.

Over the last three decades, investigation of Mars has greatly increased.  Soil, rock, and atmospheric analyses have been made.  Multi-spectral observations have been made from Mars and Earth orbits and from Earth-based telescopes.  Knowledge of extreme habitats on Earth and bizarre life forms that populate them has increased dramatically. However, this vast amount of new astrobiological information has yet to be integrated into an objective scientific evaluation of the LR results and the possibilities for life on Mars.  Indeed, in part upon misinterpretations of the new findings, myths have been embedded into the scientific literature of Mars.

Based on these myths as key ingredients, a false “standard model” of Martian life potential has been developed.  It has been accepted by much of the astrobiological community, and, through its endorsement, the world at large.  This paper attempts to bring the supportable facts together in calling for a revision of the current consensus regarding life on Mars.  It recommends actions to facilitate the paradigm change.

 

Key words: Life on Mars, astrobiology, extreme habitats, Viking mission Labeled Release experiment, Martian environment, water on Mars

 

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1.  INTRODUCTION

July 30, 2006 marked the 30th anniversary of the Viking Mission’s first Labeled Release (LR) life detection experiment on Mars.  Its strongly positive response established the presence of an active agent(s) in the Martian soil.  In subsequent runs, the response from the soil was shown to be eliminated or substantially reduced by heating or by months-long storage in the dark at about 10o C, within the Martian ambient surface temperature.[1]  Similar responses were obtained at the two Viking landing sites some 4,000 miles apart.  The data satisfied and, through improvised additional LR sequences, exceeded the pre-mission criteria set for the detection of living microorganisms.  However, the results were treated very cautiously, and the general scientific community concluded that the activity in the soil was chemical or physical, rather than biological.

Over the last three decades, the scientific investigation of Mars has greatly increased.  Soil, rock and atmospheric analyses have been made on Mars.  Multi-spectral observations have been made from orbit, and telescopic observations made from Earth.  Our knowledge concerning extreme habitats on Earth and bizarre life forms that inhabit them has increased dramatically.  However, this vast amount of new astrobiological information has yet to be integrated into a scientific evaluation of the possibilities and prospects for life on Mars.  Indeed, despite these recent findings, and, in part, based upon their misinterpretations, a demonstrably erroneous “standard model” for Martian life has been developed.  The model has been accepted by much of the astrobiological community, and, through its endorsement, the world at large.  This paper attempts to bring together the relevant discrete findings about life on Mars, and justify a revision of the current consensus.

 

 

2.  THE STANDARD MODEL

The generally accepted “standard model” for life on Mars postulates:

·         The surface of Mars is inimical to extant life because of the absence of liquid water, the intense UV flux and an ubiquitous layer of highly oxidizing chemical(s).

·         The absence of organic matter in the surface material is proof of the oxidizing layer and/or the effect of the UV flux, and of the absence of life.

·         Life may have existed on the surface in the geological past when conditions were more hospitable.

·         Extant life may inhabit underground oases where there is liquid water and environmental conditions provide a favorable habitat.

Any claim to the detection of life on Mars must deal with each of the obstacles posed by this model and relevant corollaries resulting there from.  This paper will attempt to show that the Standard Model and its corollaries, comprising the “Modern Myths of Mars,” are not supported in fact.

 

3.  THE VIKING LABELED RELEASE EXPERIMENT

 

Because life is the most complex phenomenon, the detection of any chemical on Mars is unlikely to be accepted as proof of life.  Therefore, the demonstration of active metabolism was the basis of the LR life detection experiment.  A simple diagram of the experiment is shown in Figure 1.

 

FIGURE 1.  Schematic of the Viking Labeled Release experiment

 

The nutrients were selected for the LR based on theory and experiment.  All the nutrients, or substrates, were simple Miller-Urey molecular compounds believed to have formed early on primitive Earth and, therefore, likely to have been incorporated into the earliest life forms, and probably retained throughout their evolutionary process.  Each candidate nutrient was uniformly tagged with 14C.  Those nutrients having optical isomers were included as racemic mixtures to make either stereoisomer available to potential Martian life.  The nutrients were used in minimal concentrations in pure aqueous solution to preclude possible toxicity as sometimes occurs when microorganisms are overly dosed with organic and/or inorganic matter.  Table 1 presents the LR nutrients showing their concentrations and activities.

 

TABLE 1.  Labeled Release Nutrients


Substrate

Structure and
label position (*)


Concentration


µCi ML-1*

Specific Activity
(Ci/Mole)

14C-glycine
14C-DL-alanine
14C-sodium formate
14C-DL-sodium lactate
14C-calcium glycolate

NH3·*CH2·*COOH
*CH3·*CH(NH3)·*COOH
H*COONa
*CH3·*CHOH·*COONa
(*CH2OH·*COO)2Ca

2.5 × 10-4M
5.0 × 10-4M
2.5 × 10-4M
5.0 × 10-4M
2.5 × 10-4M

4
12
2
12
4

16
48
8
48
16

 

*Total = 34 μCi, which yields 6.8 × 107 dpm ml-1

 

 

Thousands of tests were made on microbial species, covering all types available: pure cultures, mixed cultures and soils; and many field tests of soils were conducted over a wide range of environments during the twenty years of development of the LR.  Examples of field tests made with the early “sticky string” version of the instrument, which ejected and reeled in a silicone-covered string to collect its sample, are shown in Figures 2 to 4.  False positives were never obtained from sterilized samples.  Certainty of response from living organisms, sensitivity[2] (to as little as ~30 cells/g), and rapidity of response provided a high level of confidence in the experiment.

 

FIGURE 2.  LR Test at 12,000 Ft. (above timberline) on White Mountain, CA

 

 

 

FIGURE 3 (left).  LR test on Death Valley sand dune

 

FIGURE 4 (right). LR “Sticky String” test on Salton Sea desert flats

4.  THE LR PEDIGREE

An unsolicited proposal to develop the LR (originally “Gulliver”) experiment was submitted to NASA in 1958.  After extensive review, the proposal was funded in 1959.  The experiment immediately showed promise.  This was detailed in quarterly and annual reports submitted to NASA.  A new proposal for continuation had to be submitted to NASA annually for review for continuation.  There was constant interaction with NASA throughout the project.  The Viking Project was formed in 1969, and NASA invited competition for life detection experiments.  Many proposals were submitted, including that for the LR, which again underwent the evaluation process.  The LR experiment was selected by the four review committees established by NASA.  Members included personnel from NASA, NSF, NIH and academia.  They all accepted LR’s criteria for life:  evolution of 14C-labeled gas, followed by a heat-treated control producing little or no gas.  Intensive reviews, scheduled and unscheduled, of the LR were performed frequently by NASA and Viking Project committees and “tiger teams” during the additional ten years of development, all of which further increased the high level of confidence in which its many reviewers held the LR experiment.

 

5.  THE LR ON MARS

After its flawless landing, Viking 1 performed the first LR experiment on July 30, 1976.  The soil tested had been taken by the sampling arm from the surface to a depth of about four cm., placed in the distribution box and then dispensed to the LR.  Immediately upon injection of nutrient, 14C-labeled gas began evolving.  After about three days, the volume of the accumulating gas approached a plateau, but continued to show a very slight increase.  At the end of the eight-sol Cycle 1 test, a second injection of nutrient was made.  A sharp decrease in headspace gas occurred until about 20 % of it was re-adsorbed by the sample, after which a slow re-evolution of gas over the eight sols of Cycle 2 restored the full amplitude of Cycle 1.  The protocol called for a control in the event of a positive response.  Accordingly, a duplicate soil sample was inserted into a fresh cell, heated for three hours at 160o C to sterilize it (the control procedure established for all Viking biology experiments), allowed to cool and then was tested.  It produced virtually no response, thus completing the pre-mission criteria for the detection of microbial life.  Those criteria did not require a positive response to a second injection.  Further, the LR tests showed that, isolated in the dark sample distribution box and held at ~ 10o C, the soil lost its activity over a period of two to three months.  However, the positive responses had been obtained from soil samples that, prior to nutrient injection, had been