CO2 As a Primary Driver of Phanerozoic Climate
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Lecture 20 - the History of Life on Earth
Lecture 20 - The History of Life on Earth Lecture 20 The History of Life on Earth Astronomy 141 – Autumn 2012 This lecture reviews the history of life on Earth. Rapid diversification of anaerobic prokaryotes during the Proterozoic Eon Emergence of Photosynthesis and the rise of O2 in the Earth’s atmosphere. Rise of Eukaryotes and the Cambrian Explosion in biodiversity at the start of the Phanerozoic Eon Colonization of land first by plants, then by animals Emergence of primates, then hominids, then humans. A brief digression on notation: “ya” = “years ago” Introduce a simple compact notation for writing the length of time before the present day. For example: “3.5 Billion years ago” “454 Million years ago” Gya = “giga-years ago”, hence 3.5 Gya = 3.5 Billion years ago Mya = “mega-years ago”, hence 454 Mya = 454 Million years ago [Note: some sources use Ga and Ma] Astronomy 141 - Winter 2012 1 Lecture 20 - The History of Life on Earth The four Eons of geological time. Hadean: 4.5 – 3.8 Gya: Formation, oceans & atmosphere Archaean: 3.8 – 2.5 Gya: Stromatolites & fossil bacteria Proterozoic: 2.5 Gya – 454 Mya: Eukarya and Oxygen Phanerozoic: since 454 Mya: Rise of plant and animal life The Archaean Eon began with the end of heavy bombardment ~3.8 Gya. Conditions stabilized. Oceans, but no O2 in the atmosphere. Stromatolites appear in the geological record ~3.5 Gya and thrived for >1 Billion years Rise of anaerobic microbes in the deep ocean & shores using Chemosynthesis. Time of rapid diversification of life driven by Natural Selection. -
Two Stages of Late Carboniferous to Triassic Magmatism in the Strandja
Geological Magazine Two stages of Late Carboniferous to Triassic www.cambridge.org/geo magmatism in the Strandja Zone of Bulgaria and Turkey ł ń 1,2 3 1 1 Original Article Anna Sa aci ska , Ianko Gerdjikov , Ashley Gumsley , Krzysztof Szopa , David Chew4, Aleksandra Gawęda1 and Izabela Kocjan2 Cite this article: Sałacińska A, Gerdjikov I, Gumsley A, Szopa K, Chew D, Gawęda A, and 1Institute of Earth Sciences, Faculty of Natural Sciences, University of Silesia in Katowice, Będzińska 60, 41-200 Kocjan I. Two stages of Late Carboniferous to 2 3 Triassic magmatism in the Strandja Zone of Sosnowiec, Poland; Institute of Geological Sciences, Polish Academy of Sciences, Warsaw, Poland; Faculty of ‘ ’ Bulgaria and Turkey. Geological Magazine Geology and Geography, Sofia University St. Kliment Ohridski , 15 Tzar Osvoboditel Blvd., 1504 Sofia, Bulgaria 4 https://doi.org/10.1017/S0016756821000650 and Department of Geology, School of Natural Sciences, Trinity College Dublin, Dublin, Ireland Received: 9 February 2021 Abstract Revised: 3 June 2021 Accepted: 8 June 2021 Although Variscan terranes have been documented from the Balkans to the Caucasus, the southeastern portion of the Variscan Belt is not well understood. The Strandja Zone along Keywords: the border between Bulgaria and Turkey encompasses one such terrane linking the Strandja Zone; Sakar unit; U–Pb zircon dating; Izvorovo Pluton Balkanides and the Pontides. However, the evolution of this terrane, and the Late Carboniferous to Triassic granitoids within it, is poorly resolved. Here we present laser ablation Author for correspondence: – inductively coupled plasma – mass spectrometry (LA-ICP-MS) U–Pb zircon ages, coupled ł ń Anna Sa aci ska, with petrography and geochemistry from the Izvorovo Pluton within the Sakar Unit Email: [email protected] (Strandja Zone). -
The Geologic Time Scale Is the Eon
Exploring Geologic Time Poster Illustrated Teacher's Guide #35-1145 Paper #35-1146 Laminated Background Geologic Time Scale Basics The history of the Earth covers a vast expanse of time, so scientists divide it into smaller sections that are associ- ated with particular events that have occurred in the past.The approximate time range of each time span is shown on the poster.The largest time span of the geologic time scale is the eon. It is an indefinitely long period of time that contains at least two eras. Geologic time is divided into two eons.The more ancient eon is called the Precambrian, and the more recent is the Phanerozoic. Each eon is subdivided into smaller spans called eras.The Precambrian eon is divided from most ancient into the Hadean era, Archean era, and Proterozoic era. See Figure 1. Precambrian Eon Proterozoic Era 2500 - 550 million years ago Archaean Era 3800 - 2500 million years ago Hadean Era 4600 - 3800 million years ago Figure 1. Eras of the Precambrian Eon Single-celled and simple multicelled organisms first developed during the Precambrian eon. There are many fos- sils from this time because the sea-dwelling creatures were trapped in sediments and preserved. The Phanerozoic eon is subdivided into three eras – the Paleozoic era, Mesozoic era, and Cenozoic era. An era is often divided into several smaller time spans called periods. For example, the Paleozoic era is divided into the Cambrian, Ordovician, Silurian, Devonian, Carboniferous,and Permian periods. Paleozoic Era Permian Period 300 - 250 million years ago Carboniferous Period 350 - 300 million years ago Devonian Period 400 - 350 million years ago Silurian Period 450 - 400 million years ago Ordovician Period 500 - 450 million years ago Cambrian Period 550 - 500 million years ago Figure 2. -
Devonian and Carboniferous Stratigraphical Correlation and Interpretation in the Central North Sea, Quadrants 25 – 44
CR/16/032; Final Last modified: 2016/05/29 11:43 Devonian and Carboniferous stratigraphical correlation and interpretation in the Orcadian area, Central North Sea, Quadrants 7 - 22 Energy and Marine Geoscience Programme Commissioned Report CR/16/032 CR/16/032; Final Last modified: 2016/05/29 11:43 CR/16/032; Final Last modified: 2016/05/29 11:43 BRITISH GEOLOGICAL SURVEY ENERGY AND MARINE GEOSCIENCE PROGRAMME COMMERCIAL REPORT CR/16/032 Devonian and Carboniferous stratigraphical correlation and interpretation in the Orcadian area, Central North Sea, Quadrants 7 - 22 K. Whitbread and T. Kearsey The National Grid and other Ordnance Survey data © Crown Copyright and database rights Contributor 2016. Ordnance Survey Licence No. 100021290 EUL. N. Smith Keywords Report; Stratigraphy, Carboniferous, Devonian, Central North Sea. Bibliographical reference WHITBREAD, K AND KEARSEY, T 2016. Devonian and Carboniferous stratigraphical correlation and interpretation in the Orcadian area, Central North Sea, Quadrants 7 - 22. British Geological Survey Commissioned Report, CR/16/032. 74pp. Copyright in materials derived from the British Geological Survey’s work is owned by the Natural Environment Research Council (NERC) and/or the authority that commissioned the work. You may not copy or adapt this publication without first obtaining permission. Contact the BGS Intellectual Property Rights Section, British Geological Survey, Keyworth, e-mail [email protected]. You may quote extracts of a reasonable length without prior permission, provided a full acknowledgement -
The Mesozoic Era Alvarez, W.(1997)
Alles Introductory Biology: Illustrated Lecture Presentations Instructor David L. Alles Western Washington University ----------------------- Part Three: The Integration of Biological Knowledge Vertebrate Evolution in the Late Paleozoic and Mesozoic Eras ----------------------- Vertebrate Evolution in the Late Paleozoic and Mesozoic • Amphibians to Reptiles Internal Fertilization, the Amniotic Egg, and a Water-Tight Skin • The Adaptive Radiation of Reptiles from Scales to Hair and Feathers • Therapsids to Mammals • Dinosaurs to Birds Ectothermy to Endothermy The Evolution of Reptiles The Phanerozoic Eon 444 365 251 Paleozoic Era 542 m.y.a. 488 416 360 299 Camb. Ordov. Sil. Devo. Carbon. Perm. Cambrian Pikaia Fish Fish First First Explosion w/o jaws w/ jaws Amphibians Reptiles 210 65 Mesozoic Era 251 200 180 150 145 Triassic Jurassic Cretaceous First First First T. rex Dinosaurs Mammals Birds Cenozoic Era Last Ice Age 65 56 34 23 5 1.8 0.01 Paleo. Eocene Oligo. Miocene Plio. Ple. Present Early Primate First New First First Modern Cantius World Monkeys Apes Hominins Humans A modern Amphibian—the toad A modern day Reptile—a skink, note the finely outlined scales. A Comparison of Amphibian and Reptile Reproduction The oldest known reptile is Hylonomus lyelli dating to ~ 320 m.y.a.. The earliest or stem reptiles radiated into therapsids leading to mammals, and archosaurs leading to all the other reptile groups including the thecodontians, ancestors of the dinosaurs. Dimetrodon, a Mammal-like Reptile of the Early Permian Dicynodonts were a group of therapsids of the late Permian. Web Reference http://www.museums.org.za/sam/resource/palaeo/cluver/index.html Therapsids experienced an adaptive radiation during the Permian, but suffered heavy extinctions during the end Permian mass extinction. -
A Fundamental Precambrian–Phanerozoic Shift in Earth's Glacial
Tectonophysics 375 (2003) 353–385 www.elsevier.com/locate/tecto A fundamental Precambrian–Phanerozoic shift in earth’s glacial style? D.A.D. Evans* Department of Geology and Geophysics, Yale University, P.O. Box 208109, 210 Whitney Avenue, New Haven, CT 06520-8109, USA Received 24 May 2002; received in revised form 25 March 2003; accepted 5 June 2003 Abstract It has recently been found that Neoproterozoic glaciogenic sediments were deposited mainly at low paleolatitudes, in marked qualitative contrast to their Pleistocene counterparts. Several competing models vie for explanation of this unusual paleoclimatic record, most notably the high-obliquity hypothesis and varying degrees of the snowball Earth scenario. The present study quantitatively compiles the global distributions of Miocene–Pleistocene glaciogenic deposits and paleomagnetically derived paleolatitudes for Late Devonian–Permian, Ordovician–Silurian, Neoproterozoic, and Paleoproterozoic glaciogenic rocks. Whereas high depositional latitudes dominate all Phanerozoic ice ages, exclusively low paleolatitudes characterize both of the major Precambrian glacial epochs. Transition between these modes occurred within a 100-My interval, precisely coeval with the Neoproterozoic–Cambrian ‘‘explosion’’ of metazoan diversity. Glaciation is much more common since 750 Ma than in the preceding sedimentary record, an observation that cannot be ascribed merely to preservation. These patterns suggest an overall cooling of Earth’s longterm climate, superimposed by developing regulatory feedbacks -
Carboniferous Rainforest Collapse
Carboniferous Rainforest Collapse GEOL 204 The Fossil Record Spring 2020 Section 0103 Fossil Sites of Carboniferous Rainforest April Conway, John Howley, Collapse: Hamilton, USA, Jarrow, UK, Linton, USA, Olivia Medina, and Drew Tidwell Newsham, USA, Nyrany, Czechoslovakia, Joggins, Canada (Joggins, Canada site shown in figure 2) What was the Carboniferous Rainforest Collapse? The Carboniferous Rainforest Collapse was a minor extinction that happened 305 Ma (Late Moscovian to early Pennsylvanian). It was originally a rainforest home Extinction Patterns on Land to many tetrapods and plants. The rainforest was also very good for the production Plants decreased in diversity which in turn caused a decrease of coal. (Figure 1). in the oxygen levels . This affected the large arthropods and other invertebrates which could not maintain their size with these decreased levels of oxygen. This caused them to be What caused the Carboniferous Rainforest Collapse? wiped out during the collapse, especially giant dragonflies. Animals were also drastically affected because of the lack of Originally in the Moscovian the climate was hot and wet which is perfect for the growth of an available resources for survival and were forced to adapt ecosystem in a rainforest. Eventually, the climate changed to cool and dry which caused the living quickly to their new limited surroundings. organisms and plants in the rainforest to struggle. As the plants continued to struggle, the oxygen levels decreased which made life for living organisms even more difficult. Another possible cause of the minor extinction was intense glaciation which led to lower sea levels. This is also related to the issues that arose from a colder climate. -
Late Devonian and Early Carboniferous Chondrichthyans from the Fairfield Group, Canning Basin, Western Australia
Palaeontologia Electronica palaeo-electronica.org Late Devonian and Early Carboniferous chondrichthyans from the Fairfield Group, Canning Basin, Western Australia Brett Roelofs, Milo Barham, Arthur J. Mory, and Kate Trinajstic ABSTRACT Teeth from 18 shark taxa are described from Upper Devonian to Lower Carbonif- erous strata of the Lennard Shelf, Canning Basin, Western Australia. Spot samples from shoal facies in the upper Famennian Gumhole Formation and shallow water car- bonate platform facies in the Tournaisian Laurel Formation yielded a chondrichthyan fauna including several known species, in particular Thrinacodus ferox, Cladodus thomasi, Protacrodus aequalis and Deihim mansureae. In addition, protacrodont teeth were recovered that resemble formally described, yet unnamed, teeth from Tournaisian deposits in North Gondwanan terranes. The close faunal relationships previously seen for Late Devonian chondrichthyan taxa in the Canning Basin and the margins of north- ern Gondwana are shown here to continue into the Carboniferous. However, a reduc- tion in species overlap for Tournaisian shallow water microvertebrate faunas between the Canning Basin and South China is evident, which supports previous studies docu- menting a separation of faunal and terrestrial plant communities between these regions by this time. The chondrichthyan fauna described herein is dominated by crushing type teeth similar to the shallow water chondrichthyan biofacies established for the Famennian and suggests some of these biofacies also extended into the Early Carboniferous. Brett Roelofs. Department of Applied Geology, Curtin University, GPO Box U1987 Perth, WA 6845, Australia. [email protected] Milo Barham. Department of Applied Geology, Curtin University, GPO Box U1987 Perth, WA 6845, Australia. [email protected] Arthur J. -
Ediacaran Algal Cysts from the Doushantuo Formation, South China
Geological Magazine Ediacaran algal cysts from the Doushantuo www.cambridge.org/geo Formation, South China Małgorzata Moczydłowska1 and Pengju Liu2 1 Original Article Uppsala University, Department of Earth Sciences, Palaeobiology, Villavägen 16, SE 752 36 Uppsala, Sweden and 2Institute of Geology, Chinese Academy of Geological Science, Beijing 100037, China Cite this article: Moczydłowska M and Liu P. Ediacaran algal cysts from the Doushantuo Abstract Formation, South China. Geological Magazine https://doi.org/10.1017/S0016756820001405 Early-middle Ediacaran organic-walled microfossils from the Doushantuo Formation studied in several sections in the Yangtze Gorges area, South China, show ornamented cyst-like vesicles Received: 24 February 2020 of very high diversity. These microfossils are diagenetically permineralized and observed in pet- Revised: 1 December 2020 rographic thin-sections of chert nodules. Exquisitely preserved specimens belonging to seven Accepted: 2 December 2020 species of Appendisphaera, Mengeosphaera, Tanarium, Urasphaera and Tianzhushania contain Keywords: either single or multiple spheroidal internal bodies inside the vesicles. These structures indicate organic-walled microfossils; zygotic cysts; reproductive stages, endocyst and dividing cells, respectively, and are preserved at early to late Chloroplastida; microalgae; animal embryos; ontogenetic stages in the same taxa. This new evidence supports the algal affiliations for the eukaryotic evolution studied taxa and refutes previous suggestions of Tianzhushania being animal embryo or holo- Author for correspondence: Małgorzata zoan. The first record of a late developmental stage of a completely preserved specimen of Moczydłowska, Email: [email protected] T. spinosa observed in thin-section demonstrates the interior of vesicles with clusters of iden- tical cells but without any cavity that is diagnostic for recognizing algal cysts vs animal diapause cysts. -
Coevolution of Global Brachiopod Palaeobiogeography and Tectonopalaeogeography During the Carboniferous Ning Li1,2*, Cheng-Wen Wang1, Pu Zong3 and Yong-Qin Mao4
Li et al. Journal of Palaeogeography (2021) 10:18 https://doi.org/10.1186/s42501-021-00095-z Journal of Palaeogeography ORIGINAL ARTICLE Open Access Coevolution of global brachiopod palaeobiogeography and tectonopalaeogeography during the Carboniferous Ning Li1,2*, Cheng-Wen Wang1, Pu Zong3 and Yong-Qin Mao4 Abstract The global brachiopod palaeobiogeography of the Mississippian is divided into three realms, six regions, and eight provinces, while that of the Pennsylvanian is divided into three realms, six regions, and nine provinces. On this basis, we examined coevolutionary relationships between brachiopod palaeobiogeography and tectonopalaeogeography using a comparative approach spanning the Carboniferous. The appearance of the Boreal Realm in the Mississippian was closely related to movements of the northern plates into middle–high latitudes. From the Mississippian to the Pennsylvanian, the palaeobiogeography of Australia transitioned from the Tethys Realm to the Gondwana Realm, which is related to the southward movement of eastern Gondwana from middle to high southern latitudes. The transition of the Yukon–Pechora area from the Tethys Realm to the Boreal Realm was associated with the northward movement of Laurussia, whose northern margin entered middle–high northern latitudes then. The formation of the six palaeobiogeographic regions of Mississippian and Pennsylvanian brachiopods was directly related to “continental barriers”, which resulted in the geographical isolation of each region. The barriers resulted from the configurations of Siberia, Gondwana, and Laurussia, which supported the Boreal, Tethys, and Gondwana realms, respectively. During the late Late Devonian–Early Mississippian, the Rheic seaway closed and North America (from Laurussia) joined with South America and Africa (from Gondwana), such that the function of “continental barriers” was strengthened and the differentiation of eastern and western regions of the Tethys Realm became more distinct. -
Evolution, Evolution, Phanerozoic Phanerozoic Life and M E Ti Ti
Evolution, Phanerozoic Life and Mass Ex tincti ons Hilde Schwartz [email protected] Body Fossils Trace Fossils FOSSILIZED Living bone Calcium hydroxyapatite Ca10(PO4)6(OH,Cl, F, CO3)2 FilbFossil bone Fluorapatite Ca10(PO4)6(F,CO3,OH,Cl)2 EVOLUTION Descent with modification. …via tinkering with the natural genetic and phenotypic variations found in nearly all biologic populations. Wollemi pine: zero genetic variability Evidence: comparative anatomy, molecular genetics, vestigal structures, observed natural selection, and so on. Evolutionary Mechanisms Mutation Gene flow Natural selection adaptive Genetic drift random Hawaiian honeycreepers Microevolution MliMacroevolution Phanerozoic Milestones Hominids (5-(5-66 Ma) Mammal ‘explosion’ Primates Birds, Flowering plants Mammals, dinosaurs, turtles, pterosaurs, etc… Modern corals Land plant ‘explosion’ Reptiles Amphibians, giant fish, vascular plants Life on land (Plants, insects) ‘Jaws’ Vertebrates (jawless ‘fishes’) Animal ‘explosion’ Drivers of evolution Biological innovations Plate tectonics Evolvinggg global chemistry Global temperature Evolution of degradation- resistant vascular plants Berner, R. A. (2003) The long‐term carbon cycle, fossil fuels and atmospheric composition. Nature 426:323–326. Cool horse Hot horse Patterns of Phanerozoic Evolution 1.9 – 100 million species of macroorganisms Bent o n, 1985 1. Diversity has increased through time Can we trust the fossil record? Biological characteristics HbittHabitat Taphonomic processes Time The “Pull of the Recent”? Peters, 2005 Based on data in Sepkoski, 1984 (A), Niklas et al., 1983 (B), and Benton, 1985 (C,D) Number of species preserved in Lagerstatten Patterns of Phanerozoic Evolution 2. The locus of diversity has changed through Benton and Harper, 1997 time 0% of macroscopic 8585--9595% of macroscopic species are terrestrial species are terrestrial Vermeij and Grosberg, 2010 Patterns of Phanerozoic Evolution 3Etiti3. -
Rates of Species-Level Origination and Extinction: Functions of Age, Diversity, and History
Acta Palaeontologica Polonica Vol. 36, No 1 pp. 3947 Warszawa, 1991 JENNIFER A. KITCHELL and ANTON1 HOFFMAN * RATES OF SPECIES-LEVEL ORIGINATION AND EXTINCTION: FUNCTIONS OF AGE, DIVERSITY, AND HISTORY KITCHELL, J. A. and HOFFMAN, A.: Rates of species-level origination and ex- tinction: Functions of age, diversity, and history. Acta Palaeont. Polonica, 39--61. 38, 1, 1991. Global-scale data on the Oligocene to Recent planktic foraminifers and coccoliths from the tropical Pacific and Atlantic Oceans are employed for quantitative testing of alternative models (Red Queen and Stationary Hypotheses) of the rela- tionship between speciation rates, extinction rates, taxonomic diversity, abiotic events, and history of the paleosystem. The results demonstrate that although the Law of Constant Extinction is supported by the data, the theoretical implica- tions are quite ambiguous because the two considered models appear as end- members of a continuum. K e y w o r d s: Evolution, extinction, Red Queen Hypothesis, Foraminiferida, Coccolithophorida. Jennifer A. Kitchell, Museum of Paleontology, University of Michigan, Ann Arbor, Michigan #lo@, USA; Anton1 Hoffman, Instytut Paleobtologti, Polska Akademia Nauk, Al. Zwirki i Wigury 93, 02-089 Warszawa, Poland. Received: April 1990. INTRODUCTION Numerous interacting determinants characterize evolving biological systems. A common partitioning of the character-environment interaction, essential to studies of natural selection (Sober 1984), separates abiotic from biotic factors of 'environment'. Causal prominence to the biotic factors of the selective regime is given by the Red Queen Hypothesis of Van Valen (1973). This hypothesis is based on a zero-sum assumption that what one species gains, other species must lose or counter with evolution- ary change.