Different Directions

Different Directions

The New Frontier

As a child I grew up seeing the standard Geologic Chart, and as a child, not really understanding it. But I did get a sense of the great stretch of time the Earth had existed through, as well as a sense of the layers of geologic periods, stacked on top of one another like books in a pile - each containing a story about life.

And now, in the year of Darwin's 200th anniversary, I begin to clarify and again to learn.

As with all science, everything is in flux; everything is open to change, and the Geologic Chart that I grew up with is gone. And a new chart is coming into being....

When Charles Darwin wrote On the Origin of Species, he and most paleontologists believed that the oldest animal fossils were the trilobites and brachiopods of the Cambrian Period, now known to be about 540 million years old.

Many paleontologists believed that simpler forms of life must have existed before this but that they left no fossils. A few believed that the Cambrian fossils represented the moment of God's creation of animals, or the first deposits laid down by the biblical Flood.

Darwin wrote, "the difficulty of assigning any good reason for the absence of vast piles of strata rich in fossils beneath the Cambrian system is very great," yet he expressed hope that such fossils would be found, noting that "only a small portion of the world is known with accuracy."

That was 200 years ago.

Since Darwin's time, the fossil history of life on Earth has been pushed back to 3.5 billion years before the present.

In The Precambrian Eon

MYA

Periods

Major Events

543

Neoproterozoic

Oldest animal fossils

900

Mesoproterozoic

 

1600

Paleoproterozoic

Approximate origin of Eukaryotes

Transition to Oxygen Atmosphere

2500

Archaean

Oldest known fossils

Oldest known rocks

3800

Hadean

 

4500

     

Most of the fossils found there are microscopic bacteria and algae. However, in the latest Proterozoic -- in a time period now called the Vendian (see below) -- macroscopic fossils of soft-bodied organisms can be found in localities around the world, and now confirm Darwin's expectations.

So, let's look at this new frontier of knowledge, the expanding Proterozoic and how its new Vendian Period fits in.

The Proterozoic Era

Many of the most exciting events in the history of the Earth and of life occurred during the Proterozoic -- stable continents first appeared and began to grow (accrete) in a long process that took about a billion years.

Also coming from this time are the first abundant fossils of living organisms,

  • Bacteria
  • Archaeans
  • Eukaryotic cells

Here's a few words about each of these groups.

Bacteria

Bacteria are often maligned as the causes of human and animal disease ( like the one shown below: Often airborne in hospitals, schools, and other public places, Streptococcus bacteria are responsible for infections such as strep throat, scarlet fever, and some types of pneumonia ).


However, certain bacteria, produce antibiotics such as streptomycin and nocardicin, while others live symbiotically in the guts of animals (including humans) or elsewhere in their bodies, or on the roots of certain plants, converting nitrogen into a usable form.

For example, Bacteria put the tang in yogurt, the sour in sourdough bread, and they help to break down dead organic matter; bacteria make up the base of the food web in many environments.

Bacteria are of such immense importance because of their extreme flexibility, capacity for rapid growth and reproduction, and great age - the oldest fossils known, nearly 3.5 billion years old, are fossils of bacteria-like organisms.


Fossilized Bacteria

Archaea

                   Life's extremists. . .

The Domain Archaea wasn't recognized as a major domain of life until quite recently.

Until the 20th century, most biologists considered all living things to be classifiable as either a plant or an animal. But in the 1950s and 1960s, most biologists came to the realization that this system failed to accommodate the fungi, protists, and bacteria.

By the 1970s, a system of Five Kingdoms had come to be accepted as the model by which all living things could be classified. At a more fundamental level, a distinction was made between the prokaryotic bacteria and the four eukaryotic kingdoms (plants, animals, fungi, & protists).

The distinction recognizes the common traits that eukaryotic organisms share, such as nuclei, cytoskeletons, and internal membranes.

However, the scientific community was shocked in the late 1970s by the discovery of an entirely new group of organisms -- the Archaea.

Dr. Carl Woese and his colleagues at the University of Illinois were studying relationships among the prokaryotes using DNA sequences, and found that there were two distinctly different groups.

Those "bacteria" that lived at high temperatures or produced methane clustered together as a group well away from the usual bacteria and the eukaryotes.

Because of this vast difference in genetic makeup, Woese proposed that life be divided into three domains:

 

  • Eukaryota,
  • Bacteria, and
  • Archaea.

The three domains are shown in the illustration to the right, which illustrates also that each group is very different from the others.

Further work has revealed additional surprises. Most archaeans don't look that different from bacteria under the microscope.

However, biochemically and genetically, they are as different from bacteria as you are.

http://www.ucmp.berkeley.edu/archaea/NRPoctopussprsm.jpgFinding Archaea : The hot springs of Yellowstone National Park, USA, were among the first places Archaea were discovered. At left is Octopus Spring, and at right is Obsidian Pool. Each pool has slightly different mineral content, temperature, salinity, etc., so different pools may contain different communities of archaeans and other microbes. The biologists pictured above are immersing microscope slides in the boiling pool onto which some archaeans might be captured for study.

http://www.ucmp.berkeley.edu/archaea/NRPobsidianpoolsm.jpg

Archaeans inhabit some of the most extreme environments on the planet. Some live near rift vents in the deep sea at temperatures well over 100 degrees Centigrade. Others live in hot springs (such as the ones pictured above), or in extremely alkaline or acid waters.

They have been found thriving inside the digestive tracts of cows, termites, and marine life where they produce methane. They live in the anoxic muds of marshes and at the bottom of the ocean, and even thrive in petroleum deposits deep underground.

Some archaeans can survive the effects of extremely salty water.

However, archaeans are not restricted to extreme environments; new research is showing that archaeans are also quite abundant in the plankton of the open sea. Much is still to be learned about these microbes, but it is clear that the Archaea is a remarkably diverse and successful group of organisms.

      Eukaryota


The Eukaryota include the organisms that most people are most familiar with

  • Animals,
  • Plants,
  • Fungi, and
  • Protists ( Amoeba, Paramecium, protozoa, algae, slime and water molds, etc. ).

Eukaryota also include the vast majority of the organisms that paleontologists work with.

Although they show unbelievable diversity in form, they share fundamental characteristics of cellular organization, biochemistry, and molecular biology.

Besides these groups of life, with the beginning of the Middle Proterozoic comes the first evidence of oxygen build-up in the atmosphere. This turned out to be good for us much later on, but at the time quite deathly for some of the earlier forms of life.

For example, this global catastrophe spelled doom for many bacterial groups, but made possible the explosion of eukaryotic forms. These include multicellular algae, and toward the end of the Proterozoic, the first animals.

So, let's look at the newest period on the Geologic Chart, the Vendian Period.

Paleo Fun

Pages

The Charles William Collection

The Processes of the Earth
Geologic Time Scale
    New Frontier
        Vendian
        Vendian Gallery
    Carboniferous
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Looking At Crusts
Volcanoes
    Olivine Bombs
Earthquakes
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Geodes
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A Beginning Guide To Fossils
The Earliest Life
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Brachipods
Trilobites
Bryozoans
Dinosaurs And Birds
Eurypterids
Echinoderms
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Keichousaurus

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