Geology

Geology
The 366 daily episodes in 2014 were chronological snapshots of earth history, beginning with the Precambrian in January and on to the Cenozoic in December. You can find them all in the index in the right sidebar. In 2015, the daily episodes for each month were assembled into monthly packages (link in index at right), and a few new episodes were posted from 2015-18. You may be interested in a continuation of this blog on Substack at this location. Thanks for your interest!

Thursday, February 20, 2014

February 20. Calcareous algae




We’ve talked about the Cambrian explosion and some of the cool critters that evolved during it, like trilobites and brachiopods. But the less obvious life was still around, if not thriving. That included blue-green algae, or cyanobacteria. Those little guys way back in the Precambrian were the primary builders of our oxygen-rich atmosphere. But during the Cambrian, calcareous algae, that is those that could create fine layers of calcite, calcium carbonate, were still abundant enough to make small reefs in the Cambrian rocks near Saratoga, New York, at Jackson, Wyoming, and elsewhere.

Cambrian stromatolites near Saratoga Springs, NY.
Photo by Michael C. Rygel, via Wikipedia
under Creative Commons Attribution Share Alike unported license
It’s fair to call these things stromatolites, just as we did during the Precambrian. Stromatolites have survived to the present, but they have declined from their peak in the Precambrian. Some scientists think they suffered from the Cambrian proliferation of new grazing animals like trilobites, which might have roamed the surfaces of stromatolites, scraping the living algae off as food. This seems reasonable, and there is also a well-documented example from the Ordovician of stromatolites increasing in abundance during extinction events that killed off marine animals. Conversely, stromatolites decreased as animal life recovered from the extinctions.

Should we care about ancient algae? Well, ancient algae and other plants are the biggest sources of organic matter that becomes oil and natural gas. You decide whether or not to care about them.


Two noteworthy geologists were born on this day. Nathaniel Southgate Shaler was born February 20, 1841, in Newport, Kentucky. He became a fixture in the paleontology and geology departments at Harvard University. Ray C. Moore was also born today, in 1892, in Roslyn, Washington. He worked for the US Geological Survey and the University of Kansas, and he initiated the massive Treatise on Invertebrate Paleontology, 50 volumes, still in progress, and the definitive encyclopedia on invertebrate fossils. And on this day in 1962, John Glenn orbited planet earth.
—Richard I. Gibson


Photo by Michael C. Rygel, via Wikipedia under Creative Commons Attribution Share Alike unported license.

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