TIMPUL GEOLOGIC Istoria geologica a Pamantului PLAN- GHID pe baza caruia se va realiza proiectul • http://doru.juravle.com/cursuri/resurse/cursuri_2010-2011/ggp/01.%20GEOL OGIE%20GENERALA%20-%20PREZENTARE%2001%20-%20Notiuni%20introductive.pdf • http://palaeos.com/ • http://sci.waikato.ac.nz/evolution/EvolutionOfLife.shtml • http://www.pbs.org/wgbh/nova/link/hist_nf.html TEMA 16 TIMPUL GEOLOGIC
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TIMPUL GEOLOGIC Istoria geologica a Pamantului PLAN- GHID pe baza caruia se va realiza proiectul
TEMA 16 TIMPUL GEOLOGIC. TIMPUL GEOLOGIC Istoria geologica a Pamantului PLAN- GHID pe baza caruia se va realiza proiectul. http://doru.juravle.com/cursuri/resurse/cursuri_2010-2011/ggp/01.%20GEOLOGIE%20GENERALA%20-%20PREZENTARE%2001%20-%20Notiuni%20introductive.pdf http://palaeos.com/ - PowerPoint PPT Presentation
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• 1. GEOCRONOLOGIE• Geocronologia este o ramura a stratigrafie care se
ocupa cu datarea (stabilirea vârstei) depozitelor geologice si ierarhizarea cronologica a acestora, rezultând unitai geocronologice (de timp), concretizate în unitai cronostratigrafice.
• Datarea se poate face– relativ, aplicându-se corelarile pornind de la principiul
superpoziei geometrice a stratelor si evoluiei organismelor biologice
– în mod absolut, folosindu-se metode radiometrice.
II EONUL FANEROZOIChttp://palaeos.com/timescale/phanerozoic.htm#Paleozoic
Erele: Paleozoic, Mezozoic, Neozoic
• ERA PALEOZOIC -CARACTERIZARE• Geografia Paleozoicului (imagini, harti)• Viata in Paleozoic (desene)
– Of the three main eras that make up the Phanerozoic, the Paleozoic is the longest and most diverse, spanning the period from very early multicellular life that only inhabited the oceans to quite advanced tetrapods* and reptiles and extensive forests on land.
– Early Paleozoic: Age of Invertebrates Coelomate radiation (Cambrian explosion) - origin of major groups of organisms; nervous system, behavior patterns and simple consciousness (the nascent Noosphere); continents drift apart.
– Middle Paleozoic: Age of Fish Tropical conditions. Extinction of many "experimental" animal groups; diversification of surviving invertebrate groups, rise of vertebrates (fish). Life moves on land (rhyniophytes, lycophytes, uniramous arthropods, proto-amphibians).
– Late Paleozoic: Age of Tetrapods* and Reptiles Ice age. Coal forests of giant lycopsids, calamites, pteridophytes and ferns cover the tropical landmasses. Southern landmass of Gondwanaland buried under glaciers; continents drift together. Reptiles conquer the land
• ERA MEZOZOIC –CARACTERIZARE DESCRIERE imagini, harti
• Geografia Mezozoicului• Viata in Mezozoic(desene)
– The Mesozoic has been called the "age of reptiles", but "age of dinosaurs" would be more appropriate. There is still controversy over whether dinosaurs really were stupid sluggish ectotherms ("reptiles") or active high-metabolism (endotherm) creatures more like birds. Even if we define them as "reptiles" the age of reptiles as such begins in the Permian period of the Paleozoic era anyway.
– Tropical (Greenhouse) Conditions. Pangaea continues during the early Triassic; then landmasses begin to drift apart. Shallow oceans cover much of the continents, breaking the land into large islands. Mammals remain small, possibly nocturnal. Most modern groups of organisms appear. Vertebrate animals (mammals, birds, theropod dinosaurs) develop larger brains then their earlier reptilian ancestors.