Snowball Earth and the Evolution of Animals. Alex L. Sessions Division of Geological and Planetary Sciences Caltech Alumni Seminars, May 2006 A Brief History of Life on Earth Cenozoic millions of years Eon Era 0 100 Period Tertiary Mesozoic Cretaceous Jurassic 300 Phanerozoic 200 Triassic Permian 400 Paleozoic Carboniferous Devonian Silurian Ordovician 500 Cambrian Caltech Alumni Seminars, May 2006 A Brief History of Life on Earth Cenozoic millions of years Eon Era 0 100 Period Tertiary Mesozoic Cretaceous Jurassic 300 Phanerozoic 200 Triassic Permian 400 Paleozoic Carboniferous Devonian Silurian Ordovician 500 Cambrian Caltech Alumni Seminars, May 2006 A Brief History of Life on Earth 100 Period Tertiary 0.5 Mesozoic Paleozoic Jurassic Triassic Permian 2.0 Carboniferous 2.5 Devonian 3.0 Silurian Ordovician Proterozoic 1.0 3.5 Meso Paleo Archaean Mesozoic Phanerozoic Era Neo 1.5 Paleozoic 400 Eon Cretaceous 200 300 billions of years 0 Phaner. Cenozoic millions of years Eon Era 0 500 4.0 4.5 Hadean Cambrian Caltech Alumni Seminars, May 2006 A Brief History of Life on Earth 100 Period Tertiary 0.5 Mesozoic Paleozoic Jurassic Triassic Permian 2.0 Carboniferous 2.5 Devonian 3.0 Silurian Ordovician Proterozoic 1.0 3.5 Meso Paleo Archaean Mesozoic Phanerozoic Era Neo 1.5 Paleozoic 400 Eon Cretaceous 200 300 billions of years 0 Phaner. Cenozoic millions of years Eon Era 0 500 4.0 4.5 Hadean Cambrian Caltech Alumni Seminars, May 2006 A Brief History of Life on Earth 100 Period Tertiary 0.5 Mesozoic Paleozoic Jurassic Triassic Permian 2.0 Carboniferous 2.5 Devonian 3.0 Silurian Ordovician Proterozoic 1.0 3.5 Meso Paleo Archaean Mesozoic Phanerozoic Era Neo 1.5 Paleozoic 400 Eon Cretaceous 200 300 billions of years 0 Phaner. Cenozoic millions of years Eon Era 0 500 4.0 4.5 Hadean Cambrian Caltech Alumni Seminars, May 2006 an op yr s 41 ccu ssp ma s pla o rm e Th hrax Methano spirillum mari n e SBAR pSL p pGr 5 12 GrtA tC26 4 Py ro Sul Th dicti folob us er um m op ro te us 0.10 changes/site Co p Tri t mo Gi na s a ita m Entomoeba ia pler Neo ar di a ph or im ir Va modified from Pace (1997) ho Evolutionary relationships between the three domains of life, based on 16SrRNA sequences. Anatomical diversity belies a great deal of biochemical diversity. xa He Dichyostelium ric a um om ar os ys an Ph ryp T lena Eug Eucarya Po r Para phy mec ra ium Babosla rin u Homo s Zea onas hom p y ria Cr ya sta l h Ac Co ha Arc us lob g eo Halot m ilu of m er 50 Th pSL 2 2 pSL Root 8 pJP 7 pJP 27 Th Th erm er us m o pO tog Aq PS a u 56 EM ifex 17 us oco us m teriu erm th th no m Me ha et M riu te dr io De n ch sulf lo ov Syne ropla ibrio choc st oc Gloeobcus Chlamydia acter Chlorobium ma e Lepton tridium Clos illus Bac rium ter e ac 9 ct ba hrob PS1 o i l t e r O H A p ium ob c ir m mo er Th han on Archaea Thermococcus ch c ba ro Ag ito ac anob Meth m Met Bacteria lus ocyc Rhod Planctomyces Flexibacter Flavo bacte rium Phylogenetic Tree of Life Caltech Alumni Seminars, May 2006 Early Animal Divergence 535 579 549 604 634 664 494 546 Dendraster Encope Eucidaris Asterina Antedon Ptychodera Saccoglossus Mytilus edulis Mytilus californianus Modiolus Nucula Haliotis Crepidula Chaetopterus Nereis Amphiporus Lineus Cerebratulus Lestes Enaliagma Drosophilia Anopheles Priapulus Obelia Metridium Scypha Leucosolenia Microclona Ephydalia Trochospongilla Saccharomyces Arabidopsis modified from Peterson & Butterfield (2005) Caltech Alumni Seminars, May 2006 Neoproterozoic Changes 1st Taxa ∆34S (‰) δ13C (‰) BIF Ice Archaean Anoxic 2500 2000 Meso Proterozoic 1500 1000 Age (millions of years) Paleo Anoxic/ Sulfidic 3000 Neo Oxic 543 -8 0 +12 -60 modified from Anbar & Knoll (2002) 0 Caltech Alumni Seminars, May 2006 Snowball Earth? Neoproterozoic glacial deposits are found at virtually all latitudes. Was this a global glaciation? modified from Evans (2000) Caltech Alumni Seminars, May 2006 Snowball Earth? courtesy of www.snowballearth.org Caltech Alumni Seminars, May 2006 Fossils Morphologic fossils OH OH OH OH OH Chemical fossils Caltech Alumni Seminars, May 2006 Biomarker Analyses 2. Solvent extraction. 1. Crush rocks. 3. GC/MS analysis. Caltech Alumni Seminars, May 2006 GC/MS Data Chromatogram tells us relative abundances of compounds. Mass spectrum tells us identity of peaks. Caltech Alumni Seminars, May 2006 Vazante Formation, Brazil Lapa sub Landim sub Member Mbr 38 10 Morro do Calcario sub Mbr Mocombo sub Member Vazante Fm Lapa Fm 46 Phanerozoic Neoproterozoic (São Francisco Supergroup) 18 Mesoproterozoic (Espinhaço Supergroup) Paleoproterozoic-Archean (Basement) Sample Site Brazil Caltech Alumni Seminars, May 2006 Vazante Formation, Brazil TOC (%) Lapa sub Landim sub Member Mbr Morro do Calcario sub Mbr Mocombo sub Member Vazante Fm Lapa Fm 0 4 759 783 805 810 812 2x 816 2x 817 858 Retention Time Caltech Alumni Seminars, May 2006 Rogue’s Gallery of Biomarkers R Hopanes - aerobic Bacteria 2-Methylhopanes - Cyanobacteria R Steranes - Eukaryotes Gammacerane - Protists Arylisoprenoids - Green sulfur bacteria Caltech Alumni Seminars, May 2006 Shimen Section, South China Doushantuo Fm 105oE hu i Datangpo Fm Gucheng Fm An Shimen section Weng'an Hunan Guizhou Gu an gx i 20oN ck i 25oN 120oE be n Ya oc l b 115oE Hu o Nantuo Fm e z gt 30 N k 110oE ia s y o bl ha t a C 500 km Cathaysia block Yangtze block: platform facies Yangtze block: shelf slope facies Yangtze block: basinal facies Xieshuihe Fm Caltech Alumni Seminars, May 2006 Shimen Biomarkers nC19 Doushantuo Fm nC26 Nantuo Fm Datangpo Fm Gucheng Fm Xieshuihe Fm Caltech Alumni Seminars, May 2006 Conclusions • Biomarkers show no evidence of biotic crisis associated with glaciations. • Repeated ecological shifts are associated with glaciations. Phytoplankton more predominant. • Nutrient delivery a possible mechanism to connect these phenomena. Nutrients → phytoplankton → oxygen → animals Caltech Alumni Seminars, May 2006 Acknowledgements Collaborators: Chao Li, Alison Olcott, Frank Corsetti (USC), Ping’an Peng (GIG) Funding: NSF Earth Sciences Directorate More information: www.gps.caltech.edu/~als Caltech Alumni Seminars, May 2006
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