Showing posts with label earth. Show all posts
Showing posts with label earth. Show all posts

Wednesday, April 28, 2010

Transgressions of a different sort


Before fossils were understood to be the actual remains of once-living plants and animals, they were regarded in some quarters as tricks of the devil, planted by the fallen one to test the fidelity of the faithful.

After all, fossils of animals that clearly lived in the ocean were found far from any modern ocean (like those fossil clams in Nebraska mentioned in an earlier post) and even on the tops of mountains.

At a time when the Earth and everything in it was understood to be unchanged from its original creation, fossils of marine invertebrates on mountain tops were problematic, and a divinely sent global flood was an explanation that conformed both to the observations and to the philosophical framework of the time.

We now understand the dynamic nature of the Earth and can explain these observations in terms of mechanisms like plate tectonics and glaciation.

Illustration: The last major transgression of the sea over North America formed a seaway that reached from the Gulf of Mexico to the Arctic during the Cretaceous Period (144-65 million years ago). From http://www.emporia.edu/earthsci/student/mcgee2/hipln005.jpg


Friday, April 16, 2010

Shields up, Scotty


Early Earth was a rough place for life to gain a foothold.

One of the questions facing scientists is just when the earth’s protective magnetic field was strong enough to shield its inhabitants from harmful cosmic radiation.

Ancient rocks from South Africa indicate that a magnetic field 50-70 percent the strength of today’s magnetic field was in place by 3.4 billion years ago.

The evidence comes from nanometer-sized crystals of the mineral magnetite embedded in millimeter-sized quartz crystals. Quartz is the most stable mineral in the Earth’s crust and a good time capsule for the included magnetite. A magnetometer is used to detect the magnetic signal preserved in the iron atoms in the magnetite and to measure the strength and orientation of the ancient magnetic field.

[Note: Not just any rocks can be used in analyses in dating ancient geological events, because millennia of deformation and reworking of the Earth’s crust could re-set geological timepieces, so great care is taken in selecting the best candidates for dating.]

Source: Tarduno, John, et al., March 5, 2010 Science.

Grossman, Lisa, Shields were up on early Earth. Science News March 27, 2010, p. 12.