Union [U]

U44A Marriott:salon 7 Thursday 1600h

Big Bang to You and Me II

Presiding:J B Plescia, Applied Physics Laboratory, Johns Hopkins University; K Nealson, University of Southern California

U44A-01 INVITED 16:00h

Biologic History and the Cardinal Rule of Life

* Schopf, J W (schopf@ess.ucla.edu) , Earth and Space Sciences, University of California, Los Angeles, Los Angeles, CA 99095 United States

In broad perspective, the history of life is remarkably static -- once set, a system that has changed little over all of geological time. The basic chemistry of living systems (CHONSP, and the monomers and polymers they compose), the genetics and cellular structure of life, even the ecologic division of the biologic world into "eaters" (heterotrophs) and "eatees" (autotrophs), are innovations all dating from the Archean that have carried over to the present. Throughout Earth history, biology has followed the Cardinal Rule of Life -- avoid change, never evolve at all! Biology maintains the status quo, opportunistically responding only if conditions change. Life's credo might well be "if it ain't broken, don't fix it." Of course, biomolecules do get "broken," by mutations, but living systems have many biochemical repair mechanisms. Evolution is a result of small changes that slip through unfixed. We see the results of evolution in the fossil record only because of the vastness, the true enormity, of geological time. What events punctuated this static underpinning to produce the modern living world? Only three, each in its own way shaping the course of life's history. The earliest, photosynthesis, freed life from dependence on foodstuffs made by nonbiologic processes. The advent of the advanced form of this process, oxygenic ("green plant") photosynthesis -- also an Archean innovation -- pumped oxygen into the environment (markedly increasing energy yields), "rusted the Earth" (evidenced by banded iron-formations), and, by $\sim$2,300 Ma ago, led to establishment of an aerobic-anaerobic ecosystem like that today. Not surprisingly, given the Cardinal Rule of Life, the inventors of this innovation, microbial cyanobacteria, evolved little over billions of years. The second major innovation was sex. In the modern world, this reproductive process is exhibited only by nucleated (eukaryotic) cells, derived from non-sexual eukaryotic ancestors. Although eukaryotes date from $\sim$2,000 Ma ago, they first evolved slowly -- following the Cardinal Rule of Life -- until $\sim$1,000 Ma ago when sexual reproduction took over. This development markedly speeded the development of new species that could compete, and eventually dominate, in habitats previously owned by their non-sexual prokaryotic ancestors, as evidenced both in the fossil record and by molecular biology-based rRNA phylogenetic trees. The third innovation was cellular differentiation and multicelluarity. Although the "Cambrian Explosion" -- the great radiation of animal life during the Cambrian Period beginning $\sim$550 Ma ago -- is commonly viewed as reflecting this event, it seems more a continuum than a step-function change. Evolution speeded in the half-billion years between 1,000 Ma ago and the beginning of the Cambrian: phytoplankton gave rise to multicellular seaweeds by $\sim$850 Ma; and primitive protozoans, present as early as $\sim$950 Ma, had by $\sim$600 Ma given rise to soft-bodied multicelled animals. Soon thereafter, animals developed shelly protective armor -- marking the beginning of the Cambrian Period, and thus of the Phanerozoic Eon. The Phanerozoic history of life is familiar to all, from spore-producing to seed-producing to flowering plants, from animals without backbones to fish, land-dwelling vertebrates, then birds and mammals. Plants ("eatees") and animals ("eaters") co-evolved in sequence. Again, life followed the Cardinal Rule, changing little, then evolving rapidly, as new ecologic opportunities became available.

U44A-02 INVITED 16:30h

The Path of Human Evolution

* Feibel, C S (feibel@rci.rutgers.edu) , Department of Anthropology Rutgers University, 131 George Street, New Brunswick, NJ 08901

A complex series of evolutionary steps, contingent upon a dynamic environmental context and a long biological heritage, have led to the ascent of {\it Homo sapiens} as a dominant component of the modern biosphere. In a field where missing links still abound and new discoveries regularly overturn theoretical paradigms, our understanding of the path of human evolution has made tremendous advances in recent years. Two major trends characterize the development of the hominin clade subsequent to its origins with the advent of upright bipedalism in the Late Miocene of Africa. One is a diversification into two prominent morphological branches, each with a series of 'twigs' representing evolutionary experimentation at the species or subspecies level. The second important trend, which in its earliest manifestations cannot clearly be ascribed to one or the other branch, is the behavioral complexity of an increasing reliance on technology to expand upon limited inherent morphological specializations and to buffer the organism from its environment. This technological dependence is directly associated with the expansion of hominin range outside Africa by the genus {\it Homo}, and is accelerated in the sole extant form {\it Homo sapiens} through the last 100 Ka. There are interesting correlates between the evolutionary and behavioral patterns seen in the hominin clade and environmental dynamics of the Neogene. In particular, the tempo of morphological and behavioral innovation may be tracking major events in Neogene climatic development as well as reflecting intervals of variability or stability. Major improvements in analytical techniques, coupled with important new collections and a growing body of contextual data are now making possible the integration of global, regional and local environmental archives with an improved biological understanding of the hominin clade to address questions of coincidence and causality.

U44A-03 INVITED 17:00h

Human Population Influence on the Planet

* Pimentel, D (dp18@cornell.edu) , College of Agriculture and Life Sciences, Cornell University, Ithaca, NY 14853 United States

The continued expansion of the human population, now at 6.3 billion projected to reach 12 billion by 2050, is using, destroying, and polluting the very Earth's resources that support human life. Currently the World Health Organization reports that more than 3 billion people are malnourished - largest number ever. Contributing to the malnourishment problem is soil erosion that results in the loss of about 75 billion tons of soil from agriculture each year. More than 99% of all food for the world comes from the land - less than 1% from the oceans and other aquatic ecosystems. Yet agricultural cropland is being abandoned because of soil erosion and salinization and the rapid spread of human settlements. Water is essential for all life and agriculture is the major consumer accounting for more than 70% of freshwater used. Already water shortages are critical in the U.S. and worldwide. Thus far, abundant fossil fuels are supporting the expansion of agricultural productivity as well as industry and transport growth. Yet credible evidence suggests that the supplies of oil and natural gas especially are rapidly diminishing. The development of renewable energy is behind schedule and when developed will only supply only about half of current energy used. If we do not work towards a relative balance between human numbers and essential natural resources, humans will suffer. Human health, productivity and well being, now and for future generations, require the continued availability of our basic resources - soil, water, foods, and energy.