Cambrian. Marella. Anomalocaris. Hallucigenea. Jellyfish?. Shrimp?. Sponge?. Parts of Anomalocaris were at first thought to be three separate animals. Anomalocaris. Wiwaxia corrugata. Wiwaxia corrugata. Marrella splendens. Hallucigenia. GLB in the Paleozoic Era.
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GLB in the Paleozoic Era • Central North America experienced repeated transgressions and regressions of shallow, tropical seas during Paleozoic • Midwest is below equator • Large areas of tropical coral reefs • Seas deposited layers of materials that became sedimentary rocks • Limestone, shales, sandstone, gypsum • Thornton Quarry, Sagawau Canyon limestone
Ordovician Period • 490 - 443 Million Years Ago • Shallow, shifting seas covered most of North America • Biodiversity increasing rapidly • Corals, bryozoans, crinoids, cephalopods, a great variety of new brachiopods, trilobites • First fish appear in fossil record • Squid-like cephalopods were the largest creatures in Ordovician seas. • Cone-shaped shells sometimes reached a length of 5 meters (about 16 ft.).
Ordovician Period • Sea floor covered by calcium carbonate mud produced by the breakdown of "stony" algae and animal remains. • Bryozoans and algae trapped the sediment to form small mounds. • Mounds protected animals, such as brachiopods, corals, crinoids, starfish, mollusks, and trilobites. • Receptaculitids are common in the rocks from this area.
Ordovician Period Algae with Skeletons • Receptaculitesappeared around 488 million years ago in the Lower Ordovician and disappeared 250 million years ago in the Lower Triassic. • Their modern-day cousins, the Dasycladaceae, are algae that also form calcareous skeletons.
Tentaculites oswegoensis • Waubonsee Creek in Oswego, IL • Rock called Brainerd Formation • Shale and thin dolomite • Upper Ordovician and Silurian • Tentaculites oswegoensis • Fossils found only known in Illinois • Animal ranged from Oswego, IL (Kendall County) to possibly Kankakee River State Park in Will County.
Graptolites • ‘Graptolite' means 'writing in rock‘ • Hemichordate – related to echinoderms & chordates • Most graptolites are thought to have been planktonic, floating or slowly sinking through the water. • The spiral shape of some was probably an adaptation to slow sinking. • Other graptolites may have been connected to gas-filled sacs, keeping them buoyant. • Lived in water with low oxygen levels • Fed on plankton
Silurian Period • 443 - 417 Million Years Ago — Silurian Period • Shallow, tropical sea covered Illinois (then south of the equator) • Reefs, corals, crinoids, and shelled invertebrates flourished • Delicate corals, bryozoans, and crinoids were in protected pockets and along the sides of the reefs. • Brachiopods, snails, clams, and trilobites were hidden in the tangle of the complex branches of these animals • These shelled animals were eaten by predatory, squid-like cephalopods. • Largest animals of the time were 2-meter-long (6.5 ft.) sea scorpions called eurypterids
Silurian Period • Ocean reefs occurred in a band 30 degrees to the north and south of the equator. • Most widespread distribution of reefs in the history of North America during Silurian • Reefs ranged from • less than a meter (3.3 ft.) to several kilometers in diameter and • less than 3 meters (about 10 ft.) to nearly 304 meters (about 1000 ft.) high.
Silurian Period • Rich fossil deposits in Illinois and lower Midwest from this period • Many fossils from ancient Silurian reefs • e.g. Trilobites, Ammonites, Eurypterids, Corals, Crinoids, Brachiopods, Jawless Fish, Primitive Sharks • Be sure to visit the online Silurian Reef exhibit from the Milwaukee Public Museum! • Plants and wingless insects arose • But GLB fossils of these are rare since entire region was under water
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