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Geology 1023

Geology 1023. Shields and Precambrian fossils. Continental building-blocks (see map at side of lab). Shield : central core of Precambrian rocks Virtually all shield rocks are igneous or highly deformed metamorphic rocks

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Geology 1023

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  1. Geology 1023 Shields and Precambrian fossils

  2. Continental building-blocks (see map at side of lab) • Shield: central core of Precambrian rocks • Virtually all shield rocks are igneous or highly deformed metamorphic rocks • Platform: a thin (a few hundred metres) skin of undeformed sedimentary Phanerozoic rocks • Divided into various sequences mentioned in class • Sauk, Tippecanoe, Kaskaskia, Absaroka, Zuni • Mobile (orogenic) belts: currently (or recently) active mountain chains, not yet fully worn down • Cordillera and Appalachians in North America.

  3. This week’s lab is in two parts • Rocks of the Shield • In the exercise you will look at maps and answer questions that pertain to the study of these ancient and mostly highly-deformed rocks • Precambrian life: • A first look at organisms that first arose in the Precambrian • Note that most of the specimens are of Phanerozoic fossils but they represent groups that first developed in the Precambrian

  4. Doing the lab. • Q. 1. Based on 3 maps (2543, 2586 & 900A). • (a) – (f) relate to reading information from map 2543 of Central Ontario • Mostly related to seeing the distribution of the rocks (shown on the map) and their ages (as shown on the legend) • (g) asks you to compare the geological map (2542) and the map showing the magnetic fields in the area (2586). • Magnetic fields are produced by the rocks and help us understand rock distribution even when the rocks are hidden from view.

  5. Doing the lab. • Canada’s wealth and status in the world today comes from our role as a resource-rich country. • A huge percentage of Canada’s wealth has come from mining. The Precambrian shield has provided a considerable amount of Canada’s mineral wealth. • Q. 1 (i). Asks you to look at map 900A, which shows the distribution of current (or recent) mining and oil and gas operations in Canada • At the side of the map is a legend for each Province • Determine the major minerals/elements mined in the the Precambrian shield areas of ON, QC, MB

  6. Precambrian life • Life arose in the Precambrian • Oldest known preserved life forms are colonial single-celled organisms of the Kingdom Monera which formed cabbage-shaped mounds called stromatolites • Oldest stromatolites are from 3.5 Ga (billion years ago) • Stromatolites are still found in parts of the world today.

  7. Modern stromatolites

  8. Ancient stromatolite

  9. Multi-cellular life • Multicellular organisms (like ourselves) first developed in the last part of the Precambrian • One famous group of multicellular organisms is known as the Ediacaran fauna, first found in Ediacara, Australia • Ediacaran fauna are now extinct • We do not have a collection of these bizarre-looking organisms which resemble primitive sea-pens, jelly-fish etc.

  10. Multi-cellular life • The two most primitive groups of multicellular organisms which are still living today are the Porifera, sponges, and the Cnidaria, which include jellyfish, sea anemones and corals. • Sponges and corals both have skeletal elements and thus are well-represented in the fossil record

  11. Sponges • Sponges are probably the most primitive multi-cellular organisms around today • Consist of a largely undifferentiated mass of gelatinous cells supported by a variably rigid structure (your modern bath-sponge is the skeleton of a modern sponge animal) • Sponges absorb water through their sides, extract food, and emit the water through their top – hence the chimney-type shape of most sponges.

  12. A modern funnel-shaped sponge

  13. Bath sponges, the skeletons of primitive animals

  14. A fossil sponge

  15. Cnidaria • Phylum that includes jellyfish, anemones, and corals • All are jelly-like organisms with “stinging” cells • Only corals produce a skeleton (a calcium carbonate structure attached to the bottom) • Most corals are colonial, but some Paleozoic (and probably Precambrian ones) were solitary. Many produced a conical cup-shaped skeleton (“cup corals”)

  16. Doing the lab. • Q. 2. Refresh your memory as to the Linnean classification scheme • Q. 3. Draw a representative portion of the stromatolite at the back of the lab. • Drawings do not have to be highly artistic, just show the relevant features • All drawings must have a scale, and label what you can (laminations in the case of the stromatolite)

  17. Doing the lab • Q. 4. Examine the examples of sponges at the back of the lab. • In the rock and fossils set (in drawer at the back of the lab) is a specimen of the calcareous sponge Girtyocoelia. Make a drawing of it with scale and labels. • At the back of the lab is a second handout “Diagrams showing simple body plans…”. Use it to determine features of interest.

  18. Various sponges showing inhalant pores and exhalant osculum.

  19. Doing the lab • Q. 5. Examine the specimens of corals at the back of the lab. There are both “solitary” and “colonial” forms. • Examine the set of fossils in the drawers at the back and identify the 4 that are corals. • Determine the genus and age range for two of the solitary forms. • Draw a solitary and a colonial form. Use the handout “Diagrams showing simple body plans…”to help you assign labels.

  20. Various coral diagrams showing, calice, tabula(e), septum(a), etc.

  21. Questions?

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