Stephen P. Broker
Because evolution is a subject that involves the passage of time, it is essential that the student have an understanding of the magnitude of geological time. Humans measure time on the basis of years and, at most, decades. The average lifespan of Western man is approximately seven decades. More immediate events in our lifetimes are measured in days, hours, and minutes, The concept “one million” is very much beyond our full comprehension, and yet one million years is an extremely short period of time in geological terms. The earliest known forms of life date back three thousand million years, “Molecular fossils” which resemble living cells have recently been found in Greenland, and they have been estimated to be 3.8 billion years old. Mammalian evolution has been taking place for 200 million years, and there are ancestral primates known to have lived 70 million years ago. How, then, does one acquire some appreciation for the magnitude of time?
In the 1950s a book entitled
Cosmic View: The Universe in Forty Jumps
took a very interesting approach to the study of space, a concept equally as difficult to grasp as that of time. Beginning with a drawing of a young girl sitting in a rocking chair, the author moved a step at a time, by powers of ten, outward from the girl, and then inward. Each succeeding drawing took the observer ten times farther away from, or closer to the girl. Within the first few jumps outward, the observer realizes that the girl is sitting in a school yard, that the school is located in a farming region, that the farmlands are in western Europe, that the earth’s northern hemisphere is being represented. Each jump of a factor of ten develops a feeling for the magnitude of self, region, continent, hemisphere, earth, solar system, galaxy, and known expanse of the universe. In the reverse direction, moving from our most familiar frame of reference to smaller objects, the imaginary camera, now installed on a microscope rather than a telescope, focuses on skin tissue, cells, cellular organelles, molecules, atoms, and subatomic particles. Forty different frames of reference were required in this book to span the magnitude of the universe known to man.
More recently and in a similar approach, the astronomer and writer Carl Sagan has refined an effective method for the study of time. Taking the history of the universe from the time of the Big Bang, currently estimated as having occurred fifteen billion years ago, up to the present, and condensing this time into one imaginary calendar year, January 1 through December 31, one can develop a “cosmic calendar.” January 1 marks the occurrence of the Big Bang, that “moment” when all of the coalesced matter of the universe exploded outward and began its migration away from the center. The last tick of this geological clock, on December 31 as 11:59.59 passes by, marks the approach to the present. One can then mark notable events on this calendar, such as the formation of our solar system, the cooling of the earth’s crust, the first appearance of life on earth, and the appearance of man’s progenitors. Such a calendar is easily adapted for the study of hominid evolution.
In preparing his own cosmic calendar, the student learns that life on earth has had an enormous amount of time in which to change. With an estimated 4.5 billion year age of the earth (early September on our calendar), and with life first appearing at least 3 billion years ago (the first week in October), one begins to get the feeling that it would be far less likely that life would remain continuous and unchanged for such vast periods of time. At the same time, one realizes that our residence on this planet has been relatively brief: the first m~mals appear on the cosmic calendar on December 26, and the first primates do not make an appearance until December 29* Those forms that we call hominids appear late in the day on December 31. Our calendar. which is more detailed for the final days and hours of December, is developed to reflect the appearance of life forms now extinct: early pongids (apes); dryopithecids (Miocene apes); ramapithecids (the first ape like inhabitants of open grasslands); australopithecids (close relatives of
Homo
).
Homo sapiens
(modern man) appears at approximately 11:59 p.m. On the last day of this imaginary year. Although we can never fully grasp the magnitude of vast periods of time, the calendar does give some perspective on the length of time during which evolutionary change has taken place.
It is also helpful to look at generation time in comparison with geological time. Different organisms are capable of reproducing at different rates. Bacteria growing under optimal conditions can reproduce asexually every 20 minutes. If it were possible for bacteria to divide at this maximum rate over an extended period of time, 72 generations of bacteria would be produced in 24 hours. More than 26,000 generations would follow in the first year. Obviously, all bacteria don’t reproduce unchecked, but their overall generation time is very short.
Generation time in humans varies widely, with the capability for reproduction ranging from 12 to 18 years. Assuming an average generation time of 20 years, there have been 10 generations that intervene between us and time of the American Revolution; 100 generations since the time of Jesus; at least 15,000 generations since Peking Man; 50,000 generations in the past 1 million years. Similarly, each of us has had 210=1024 ancestors since the American Revolution; 250,000 ancestors since 1 million years B.P. That is a lot of generations and a lot of ancestors. (B.P. = before present).
The geological epochs during which hominids and nearhominids have evolved are the Miocene, Pliocene, and Pleistocene Epochs. These epochs are referred to in Section IV of this narrative, dealing with the fossil record. The Miocene spans the period of time from 25 million to 12 million years B.P.* A number of ape species were present in Africa, southern Europe and Asia during the Miocene, including the great ape
Dryopithecus
and the lesser ape
Limnopithecus
. (See slides.)
During the Pliocene Epoch, approximately 12 million to 3 million years ago, tropical forests of the Old World increasingly gave way to open grasslands and savannas. The first arboreal/terrestrial primates to exploit these habitats were the ramapithecines, including
Kenyapithecus
,
Gigantopithecus
, and
Ramapithecus
. Toward the end of the Pliocene the first hominids, the australopithecine, appeared in East Africa and South Africa. The Pleistocene Epoch, 3 million to 10,000 years ago, was characterized by great changes in climate and by extensive glaciation. A number of mammals, including the once diverse hominid lines, became extinct. One hominid line, that of man, emerged.
*The symbol is used for “approximately” throughout this paper.