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SCIENCE AND THE BIBLE TALK ABOUT THE EARLY EARTH
Because the Precambrian part of geologic history covers so much material, the discussion is split into three parts with this being the second. Here is a summary of the three sections:
- The first section summarizes the standard model for formation of the Universe, Solar System and Earth, Moon, oceans, continents, and plate tectonics.
- This second section describes Precambrian rock exposures, as well as the atmosphere, climate, and Precambrian life. Many illustrative pictures are included. Design examples and creationist ideas are interspersed throughout.
- The third section provides two perspectives suggested by creationists: (1) a young universe and life and (2) old inorganic material, but young life.
PRECAMBRIAN ROCK EXPOSURES
Large areas of Precambrian cratons are exposed in what are called shields in Australia, the central part of Canada, western (Fig.1) and central Africa (Fig.2), the Baltic region (Fig.3), and major parts of China, Brazil (Fig.4) and Argentina, and India.
Many small outcrops of Precambrian rocks are exposed as basement rocks in other parts of the world such as Korea (Fig.5), Peru (Fig.6), Mt. Sinai (Fig.7), and southern Israel at Timnah (Snelling, 2010). Outcrops in the United States are found in places like northern Michigan, the bottom of the Grand Canyon, the Colorado Rocky Mountains (Fig.9), New Mexico (Fig.10), and the Transverse Ranges of southern California (Fig.11). Some of the first cratons to form at about 3.3 Ga were the Kaapvaal and Zimbabwe (Fig.12) cratons in southern Africa and the Pilbara and Yilgarn cratons in Australia. Some of the other three dozen cratons include: the Slave and Superior cratons in Canada, three in Greenland, and cratons in Scandinavia and the Antarctic.
After the cratons formed, they eroded to produce sedimentary deposits between them and some collided due to early plate tectonic motion. The collisions produced volcanic activity, granitic intrusions, and metamorphism of the sediments that often resulted in green rocks. These granite-greenstone mobile fold belts are common between various cratons exposed on the continents. Some volcanic rocks intruded under water forming pillow structures, e.g., in Russia (Fig. 13), South Africa (Fig. 14), and Michigan (Fig. 15). Other volcanic rock resulted from mantle melting at especially high temperatures yielding the uniquely high-magnesium komatiite, named after the Komati River (Fig.16) in South Africa; one good example of komatiite comes from western Russia (Fig.17)
Granitic magma was intruded underground to form chambers as in Namibia (Fig. 18), to break up the host rock as in eastern South Africa (Fig. 19), and to mix with host rock as near Cape Town (Fig. 20). Igneous, magmatic activity associated with craton movement produced large dikes of low silica rocks such as the Great Dyke in Zimbabwe and layered igneous intrusions such as the Skaergaard in Greenland and the Bushveld Complex in South Africa that are important sources of platinum group elements. Metamorphosed sediments include sandstone, limestone, and shale, with turbidites in South Africa (Fig. 21) as one example. Other examples of fold belts include: the several 0.9-0.5 Ga Pan-African fold belts in Zambia (Fig. 22) between the Congo and Zimbabwe cratons that are a major source of copper, the 3.5-3.2 Ga Barberton granite-greenstone complex in South Africa between the Zimbabwe and Kaapvaal cratons that displays greenstone rock (Fig. 23), and the 3.8 Ga Isua Greenstone Belt in Greenland that is one of the oldest.
Numerous impact structures are found in the Precambrian such as the large Vredefort Dome (Fig. 24) in South Africa formed at 2 Ga and the Sudbury structure in Ontario, Canada formed by a 10-15 km bolide at 1.8 Ga.
In many places an unconformity exists between the Precambrian rocks and the fossil-bearing Cambrian sediments above them, e.g., in Colorado Springs (Fig. 25). However, in a few places the unconformity in the sedimentary record may be lacking, e.g., in Morocco (Schmitt, 1978) and Newfoundland (Hutchinson, 1962; Narbonne et al., 1987; Brasier et al., 1994).
A second great oxidation event occurred in the late Precambrian, when oxygen built up from 1% to 20%. This may have been due to phosphorous-driven algal blooms or feedback between microbes and clay minerals. The current concentration of 20% oxygen in the atmosphere is ideal: less would not be sufficient for complex, active animals and more would make it difficult to keep fires under control.
Evidence for cooling events are found in the Precambrian at 2.9, 2.4-2.2, and 1.4 Ga, but evidence for glaciation is especially prominent near the end during what is called Snowball Earth. This evidence comes from rocks scratched by glacial movement, moraines of jumbled rocks carried by glaciers, and rocks called tillites that are dropped from glaciers. A seminal paper (Hoffman et al., 1998) called “A Neoproterozoic Snowball Earth” described tillites from the Skeleton Coast of Namibia suggesting that glaciers occurred at sea level near the equator which would indicate that the entire Earth had frozen over. Others have advocated a less extreme version with the Earth not totally frozen over, resulting in a slush ball instead of a snow ball.
The end-Precambrian cooling events are considered to be part of a cooling/heating cycle resulting from varying carbon dioxide in the atmosphere. The glacial climate resulted from massive blooms of photosynthetic algae that took CO2 out of the air and removed the greenhouse effect. A buildup of white snow and ice reflected the Sun’s heat back into space giving positive feedback to the cooling. The rapid growth of algae concentrated isotopically light carbon leaving isotopically heavy carbon to be incorporated into contemporaneous limestone deposits at 0.79-0.74 Ga. Later when microbial activity slowed down, CO2 began to build up in the atmosphere resulting in a greenhouse effect and causing the carbon isotopes in limestone to become much lighter. These limestones deposited at the end of the glacial cycle and above the glacial deposits are called “cap carbonates.” This snowball/hothouse cycle probably occurred three times around the 0.73 Ga Sturtian glaciation, the 0.65 Ga Marinoan glaciation, and the 0.58 Ga Gaskiers glaciation.
PRECAMBRIAN LIFE (images and descriptions)
In the standard science model (Schopf, 1983; Mesler and Cleaves, 2015), living organisms developed in the Archean with the first evidence for bacteria found at about 3.5 Ga. It is true that complex biomolecules are ubiquitous and are found in hot undersea vents, acidic streams, boiling pools, frozen Antarctic rocks, and stratospheric dust particles. In fact, half of Earth’s biomass lies miles below its surface. The building blocks of sugars, amino acids, and lipids can easily be formed by ultraviolet radiation, or violent ionizing radiation from lightning, or gentler oxidation-reduction reactions. These building blocks can even be assembled into macromolecules. Thomas Gold and others have suggested that methane and petroleum biomolecules may be abiogenic and come from deep in the earth, instead of being produced by living organisms.
However, making only right-handed or left-handed molecules is a “daunting challenge” and developing self-replicating molecules is the “greatest enigma.” (Hazen, 2012) It has been variously suggested that organic molecules formed on mineral surfaces, or in a lipid world, or in an RNA world. Although many scenarios have been suggested for developing life from non-life, none are very convincing.
The most prominent evidence for life in the Precambrian are stromatolites apparently formed from microbial mats. These concentric geologic structures are interpreted to result from single-celled organisms growing in sheets that catch sedimentary particles upon which the next mat of bacteria grows. Modern day examples of these are found in Shark Bay, Australia. Examples from the Precambrian are found in the bottom of the Grand Canyon (Wise, 2005), in the Upper Peninsula of Michigan (Fig. 28), in southern Africa, and many other places.
Evidence for multicellular life is not found until the end of the Precambrian in the 0.64-0.54 Ga Ediacaran (formerly Vendian) period. Soft-bodied fossils displaying symmetrical impressions were recognized from 0.58 Ga rocks in Ediacara of southern Australia. Most remarkable are the 0.63 Ga Doushantuo formation fossils of southern China that display clumps of cells interpreted to be animal eggs and embryos.
After the Precambrian, living organisms radiated rapidly in what is called the Cambrian explosion of trilobites, clams, brachiopods, bryozoans, sponges, horn corals, and many other new life forms. One can see the exact layer where this abrupt change from Precambrian to Cambrian occurs in Morocco. The Burgess Shale, made famous by Stephen Jay Gould’s book Wonderful Life (1990), is another prime example of this explosion of life forms.
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- Jean-François Moyen, Gary Stevens, and Alex Kisters (2007). “FT2 Post-conference field trip to the Mesoarchaean Barberton Granite-Greenstone terrain.” 6th International Hutton Symposium on the origin of granites and related rocks, 7-12 July 2007, 168p.
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