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BYA

CELL-CELL COMMUNICATION. EVOLUTION OF SEX (Meiosis). ORIGIN OF THE NUCLEUS AND ORGANELLES. ORIGIN OF LIFE. Ancestral humans. 0.002. Diversification of mammals. Invasion of the land. 0.6. Diversification of animals. 1.0. Origin of the major eukaryotic groups. 1.9.

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BYA

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  1. CELL-CELL COMMUNICATION EVOLUTION OF SEX (Meiosis) ORIGIN OF THE NUCLEUS AND ORGANELLES ORIGIN OF LIFE Ancestral humans 0.002 Diversification of mammals Invasion of the land 0.6 Diversification of animals 1.0 Origin of the major eukaryotic groups 1.9 Eukaryotic cells abundant 2.8 Atmospheric oxygen plentiful 3.6 Simple cells abundant 3.8 Stabilization of the earth 4.6 Origin of the earth BYA

  2. EVOLUTION OF COMPLEX LIFE FORMS

  3. THE PROTEROZOIC ERA: 2.5 BYA TO 543 MYA • Most of this era was characterized by prokaryotes and eukaryotic algae. • First evidence of multicellularanimal life appeared less than 1 BYA. • Oldest fossils of multi-cellular animals are 640 million years old. • The best-known Precambrian animals are the EDIACARAN FAUNA. • Soft-bodied, lacking skeletons. • Crept or stood upon the sea floor. • Most don’t fit into modern Phyla.

  4. Ediacaran Fossils: • Large diversity of forms with unknown affinities to more recent fossil groups. • Do these fossils represent a “failed” metazoan lineage? Dickinsoniana

  5. EDIACARAN ASSEMBLAGE (600 – 543 MYA)

  6. Discovery of Possible Earliest Animal Life Pushes Back Fossil Record - 650 million years ago Stromatolite column of bacterial mats in Australia; sponge fossils are between stromatolites Evidence from biomarkers and molecular clocks points to the existence of sponges tens of millions of years before their earliest fossil remains. Fossils from South Australia may narrow that gap. Possible animal-body fossils in pre-Marinoan limestones from South Australia Maloof1et al. 2010 Nature Geoscience3, 653 - 659

  7. EARLY METAZOAN EMBRYOS From the Doushantuo Formation, Southern China 570 MYA FROM: Xiao et al. 1998 Nature

  8. PALEOZOIC ERA: CAMBRIAN PERIOD (543 to 500 MYA) • The “Cambrian Explosion” started about 530 MYA. • Almost all of the modern phyla and classes of skeletonized marine animals suddenly appear in the fossil record. • This explosion may have occurred in 30 MY or maybe as little as 5-10 MY (according to the fossil record). • The most amazing record of this period appears in the BURGESS SHALE, which is near Banff, BC, Canada. • Almost all of the fundamentally different animal body plans were present by the end of the Cambrian. • Cambrian ended with a mass extinction.

  9. Usually Fossils Look Like This In the Burgess Shale Formation They Look Like This! Lenoides serratus

  10. CAMBRIAN ASSEMBLEGE

  11. Hallucigenia

  12. Anomalocaris

  13. Marrella

  14. Cambrian Crustacean Cambrian Onychophoran?

  15. Pikaia Notochord Segmented Muscle

  16. Primitive Chordate??? Haikouella lanceolata

  17. Conodonts: Ancestral Chordates

  18. DIVERSIFICATION DURING THE PRECAMBRIAN PERIOD RESULTED IN THE ORIGIN OF VIRTUALY ALL THE EXTANT MAJOR ANIMAL PHYLA!! • (AS WELL AS QUITE A FEW WE KNOW ALMOST NOTHING ABOUT)

  19. Diversification of Regulatory Genes Underlying Animal Body Plans

  20. Evolution of the Hox Gene Cluster • Expansion of a gene family • Acquisition of novel gene function • Increasing complexity Is morphological complexity correlated with genetic/genomic complexity?

  21. The Enigmatic Placozoans

  22. WHAT PRECIPITATED THE CAMBRIAN EXPLOSION? • Diversification may have been promoted by increasing oxygen levels in the atmosphere. • Vacant ecological niches may have fostered diversification. • Key innovations related to multicellularity and the organization of developmental processes may have evolved (e.g., collagen, hierarchies of gene action). • Nobody knows for sure. • Or maybe there was no such thing…

  23. Molecular Evidence for Deep Precambrian Divergences Among Metazoan Phyla FROM: Wray et al. 1996 Science

  24. An Early Cretaceous Tribosphenic Mammal and Metatherian Evolution Zhe-Xi Luo, Qiang Ji, John R. Wible, Chong-Xi Yuan 125 MYA

  25. Large Mesozoic mammals fed on young dinosaurs: 139-128 MYA Cifelli & Davis SCIENCE 2003 Nature433, 149 - 152 (13 January 2005) YAOMING HU, JIN MENG, YUANQING WANG & CHUANKUI LI

  26. CENOZOIC ERA: Paleocene epoch (65-55.6 Mya) Mammalian radiation after the extinction of the dinosaurs.

  27. Ancestral humans 2 Diversification of mammals 65 100 Origin of flowering plants/ diversification of insects 150 Origin of early Mammals 200 Origin of Birds 300 Origin of amniotic egg 400 Origin of land plants 550 Origin of the major groups of animals MYA

  28. BIG PATTERNS IN THE HISTORY OF LIFE • If life originated on earth, the main plan may have been set down in a “relatively” short period of time. • In terms of the appearance of major evolutionary novelties, long periods of stasis appear in the fossil record. • Explosive periods of diversification appear to follow the “invention’ of new genetic mechanisms or ecological changes precipitated by life itself. • Periods of stasis in the complexity of life appear to be getting shorter – suggesting evolution has “autocatalytic” properties.

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