(Reprrnred frm Nature, Vol. 207. No. 4992, pp. 9-13, 3uly 3, 1965) SIGNS OF LIFE CRITERION-SYSTEM OF EXOBIOLOGY By PROF. JOSHUA LEDERBERG Department of Genetics, Stanford University School of Medicine, Palo Alto, California T HE imminence of interplanetary. traffic calls for systematic criticism of the theoretical basis and operational methods of `exobiology', t,he init,ial search for and continual investigation of the life it might en- counter. Very little science is totally irrelevant to it, and the policy-maker must face a riot of potential approaches to space flight experiments. By every stand- ard, this is an epochal enterprisa: a unique event in the history of the solar system and of the human species, and the focus of an enormous dedication of cost and offort. It, requires a new perspective in experimental policy. The broader interfaces of eso-(Earth's own) biology, by cont,rast, permit it,s fruitful growth within the context of methodologies and instruments that can lag behind broadly established needs and imaginative possibilities. A system for orderly appraisal of the problem would rationalize the partition of labour, our only means of managing a complex problem. Mars is our prior t,arget. Our premissed information is only: (1) terrestrial observation: osobiochemistry ; (2) the implications of Mars being a `terrestrial planet'; (3) a very small body of definite observational results. The choice of our first experiments must take account of a wide range of theoretical possibilities not yet narrowed by the experimental process. Over this broad reach, logical necessity rarely coincides with logical sufficiency. The most compelling inferences might stem from the least likely event. Our speculation will be narrowed and policy simplified by t,angible information about any aspect of Mars, especially if it encompasses the varia- bility of the planet's fcat,ures in space and time. Evolutionary Stages and the Definition of `Life' Fundamental to all biological theory, eso- or exo-, is the evolutionary principle. As is now commonplace, we recognize the following stages in the Earth's history: (A) Chemogeny (orgo& chemislr?/). The production of complex organic compounds by a variety of non-replica- t,ive mechanisms-the primitive cosmic aggregation, photochemistry of isolated atmospheres, thermal and spontaneous reactions of inorganically catalysad, previ- ously formed reagents. (B) Biogeny (biology). The replication of a specifically ordered polymer, DNA being the terrestrial example, which specifies the sequence of its own replicas, and of the working materials, like RNA and proteins, from which cells and organisms are fashioned. Random experiments of error in replication, and natural selection of their developmental consequences, result in the panoply of terrestrial life. (C) Cognogeray (history). The evolution of the mechan- isms of perception, computation, and symbolic expression and interpersonal communication, whereby t,radition can accumulate, culture unfold. Mars must be supposed to have had an initial history similar to Earth. To ask whether Mars has life is to ask how far has its chemogeny gone; how like and how unlike the Earth's; has its evolution passed through the biogenic (ordered macromolecular) stage ? Then through the cognogenic ? In evaluating a complex set of possibilities it is helpful to &d classifying parameters which can be scanned systematically, if sometimes only implicitly, to generate a probabilitv space. In this case, the evolutionary principle furnish& the parameter : chemical complexity: The initial planetogeny and the consequent differences in physical and chemical environment determine the possibie points of departure of the evolutionary processes. On these grounds, Jupiter must have special interest for comparative cosmochemistry; but it is still much less accessible to close investigation, and we have even less of a basis to predicate a homologous chemogeny there than we do for Mars. In so far as Mars does retain some environmental analogies to Earth we might at least predicate, for one branch of our analvsis, that any Martian iife is based on chemical linkkges, predominantly -C-C-, -C-O-, -C-N- and -O-P-, which are barely stable in aqueous medium. We leave to hypothesis the extent to which the constructions from thoso and other radicals emulate terrestrial biochemistry at each level of complexity. The cosmic abundance of these elements is relatively high, and there is every reason to believe that Mars is at least as richly endowed as Earth in them. If the initial budget of carbon has not, like that of the Earth's crust, been completely requisitioned by life, then what form will we find it in ? Chemogeny generates a vast mixture of products through the level of random macromolecules. Mars must have nurtured such chemistry, whether or not it had progressed to biogeny. A negative assay for organic materials would preclude biology, but could we believe such a result ? It would properly be blamed on defici- encios in the particular sample. The positive assay, if it told something of t,he concentration and composition of organic molecules, would add t,o our uuderst'anding of Mars's development'. and would contribute to our judg- ment of the life-detection problem. But it would not answer it. On the other hand, onto life has appeared on a planet, it would dominate its organic chemistry-most carbon compounds would bo witnesses of biogenic (or cognogenic) specificity. The cataloguing of organic molecules is a description of the consequences of evolution and must make up a large part of our effort. The Chemical Scan To promise an actual complete scau of hypotheses of molecular complexity would be pretentious and witless, notwithstandirig that a computer can now bc programmed to visualize all the possibilities. However, the fantasy of such a scan is a constructive exercise in evalua- tion of evidence for life. For each chemical species the imagination of the specialist might be challenged to ask: (a) is there any information concerning t,he existence of this it,em relevarit to scientific inferollce in exobiology; (b) what are my prior expectations on the distribution of this species, with and without life; (c) what other data could contribute; (d) how would the observation be inter- preted from a t,errestrial foray; (e) what special methods are available or could be devised to detect the species ? We might nurture a hope of turning up a special treasure, a rare example of a molecule which would reveal something about the evolution of the planet and help narrow our choices among the confusing array of pqssible targets. In practice this advantage does not materialize so easily, for the hope is false. Not that no chemical M B C LF Fig. 1. Contingency ~pxe. `l'lie rmivcrse of possible observations I includes the overlapping domains II and C, the predictions of biogeny and chemogeny, respectiwly. Tlw remainder is N, contradictions of these models, and possible cons~~~~nc~s of cognogeny. Should this also I,l~ bourdYl `) species is potentially informative; paradoxically, every one is. Consider hydrogen. In term.5 of tho simple Venn diagram (Fig. l), most expected observations would fall in the region (B4"), that is, would be consist,ent with biogeny but not imply it. However, the sensible absence of hydrogen from Mars' surface would fall in region (--H.G), that is, virtually preclude life. But if we could produce no plausible physical model for the disappearance of hydrogen, we would have to reconsider the region (I.-C), t,hat is, to ask whct,her the anomaly implies a bio- gonic or cognogenic sequestration of the element. On the other hand, certain microscopic distributions of H are hard t,o reconcile wit,h any chemogenic model, and point to tho region (U.--C), t)hat is, an inference in favour of biogeny. This verges on morphology, but can still bn formulated as molecular statistics. On another tack, suppose a specimen consisted of pure protium, 1H, to the exclusion of deut'crium, 2H. Tll0 price of pure prot,ium on thn t,errcstrial market hints at, the obstacles to a chomogenic model. Apart from cogno- genie activity, if a biogenic q;stem were exqisitcly sensitive to deutsrium-tosicit,y it might evolve a dis- crimination against it,. The arguments have been laboured, but are rluite typical of those that. discovery of any other species would arouse. Entropy or Unlikelihood ? Given the evolutionary continuity of lifo and our understanding of the organism as a chemical machine. there can be no absolutely distinctive signature of lift. Some conjunctions-like a planetary depot of protium- would be so unaccountable to our present model of chemi- cal behaviour that we would feel obligated to postulate the operation of a goal-directed system (biogeny or cognogeny) rather than accept tho improbability of such a conjunction by chance. This choice plainly depends on our freedom of choice of models. For example, OUI present knowledge of chemogeny permits a wide latit'udc of hypotheses as to the range of molecular species that atmospheric photochemistry might generate. Further developments in our knowledge of chemogeny or of the available chemical and physical resources of Mars might confer useful constraints on the data that might now be `explained away' as chemogeny, and thus cannot yet make a crucial contribution t,o our search. From terrestrial ospcrienco we judge that the occur- rence of any of a number of compounds in high purity is a sign of life. Such deposits at a macroscopic level tend to signify cognogeny-a smelter, a chemical laboratory, a communications cablo, rather t~ha.n biogmy-organic structure usually being built of microscopically dcfincd components. Kegentropy is a noccssar~, but not sufficient', sign of life. However, it can help filter out the most promising situations. Then only the details of exparicnco or confident USC of available theory can decide whothcl tho eddy has a chemical-kinetic explan&ion or a bio- 01 cogno-genie one. Lacking our oxperienco, a Martian visitor might credit diamantane carbon to some mysteri- ous biogenic function, inhibit'ed by I' chromosomes; if hc: were cleverer, to the General Electric Co. He would noed vory special knowledge of the Earth to predict t,het diamonds would be found in the ground (and even more to understand lvhy mon dig them up, only so t,hat womc'n will wear them). Kinetic instability in the context of local chemical anal physical conditions is another clue: For example, cove1 of photosensitive pigments (witness terrestrial chloro- phyll) recluires special att.ention to the magnitude of plausible synthetic processes, atmospheric-chemical versus biogenic, by which their st'eatly-state concentrat,ion could be maintained. dnalogous reasoning would apply to compounds which are thermolabile in relation to thr ambient tcmpcrature, or chemically unstable species \vhich should reach equilibrium with coexistent, oxidant. Do we see a forest fire . `p Then wo must, think of tho efficient system of photosynthesis which will restore the steady-state vegetation. Top-heavy structures, which high-altitude reconnaissance could perceive even without resolving single trees, houses, or bipeds, likewise tell of kinematic instability, and in turn, some process to re- raise what must some time fall. But geophysics competes with biophysics, and we have to discriminate life from vulcanism and orogeny. In sum, unlikelihood in terms of the chemogenic model gives weight to any finding as a datum for exobiology. It, should be possible to quantitate chcmogenic likelihood, essential if a datum is to be given a measured value in any decision-making programmc. Tho resolut,ion of the Ineasurement need not be very high. to make it still very useful in comparing disparate approaches. In more general terms, biota have a high `density of' internal information: the root of our conceptual distmc- tion bctwocn matter and life is the rich story tha.t lifo can tell about itself, a plot, tho details of which wo ca.n scarcely deduce from our simple knowledge of the initial conditions. But there must bo a plot, that is, tho informe- tion must have some interesting pattern, or we would not. distinguish a cell from the dislocations in a snowflake. Optical Activity ?ileny molecular species can contribute in an important \vay to our appreciation of life. A ~Aori, WC have a very .? limited basis to predict which species will be most cogent. We should, of course, give high, but not exclusive, priorit,v t,o terrest,rial prototypes like amino-acids and nucleotidcs. Fortunately, there is a generic classificat,ion of compounds which is relatively independent of detail of struct,ure, yet should pervade a biogenic chemistry. This is optical act'ivity. The argument for logical necessity of net optical activity has nothing to do with optical rotation. It depends on the crucial role of t,he informational macromolecule in a definition of life. JVhen tetravalent carbon is incorpor- ated into macromolecular structure, each carbon stands a reasonable risk of being an asymmetric centro, of having a distinctive substituent on each of its four valences. Such an atom is subject to stereo-(optical) isomerism, and its Ori0nt&iOn, D- or L-, must be specified if the macro- molecule is to be fully ordered, more concretely, if it is t,o have a ndl-defined t,hree-dimensional shape. Con- versely, biogenic macromolecules, having ordered asym- metric centres, have the necessary information to dis- criminate among the isomers of monomeric substrates. i)n Earth, where biogeny has dominated the st,atistics of organic molecules. n-c find that the ratio of D- to L-glucose residues is at least 1O'j : 1. Logical sufficiency can also be argued. Chemical en- antiomorphs should be generated in equa,l proportions except under the influencn of a catalytic system which is already asymmetrically organized. The global organiza- tion of a planet int'o one catal~t~ic system of particular orientation is a catastrophe of :L magnitude unique to biogeny. Spont,aneous &solution miiht occur locally. Hence this criterion has its great<& weight when annlied to a species which Rows thro