DOC PREVIEW
Berkeley BIOLOGY 1B - Evolution lecture

This preview shows page 1 out of 4 pages.

Save
View full document
View full document
Premium Document
Do you want full access? Go Premium and unlock all 4 pages.
Access to all documents
Download any document
Ad free experience
Premium Document
Do you want full access? Go Premium and unlock all 4 pages.
Access to all documents
Download any document
Ad free experience

Unformatted text preview:

Almost all large vertebrates and many other species went extinct.Surviving groups radiated to become the dominant flora and fauna today.The probably impact crater has been located in Mexico.Bio 1B Lecture Outline (please print and bring along) Fall, 2008B.D. Mishler, Dept. of Integrative Biology 2-6810, [email protected] lecture #9 -- Fossils: Mesozoic and Cenozoic -- Nov. 24th, 2008Summary of lecture:• Finish talking about plant evolution starting in Devonian, leading to Angiosperms in Mesozoic• Mesozoic and Cenozoic:–“Reptiles” (Diapsids vs. Synapsids)–Dinosaur biology and diversity–Birds–Mammals–Primate and Human evolutionStarting in Devonian, diversification of land plants: increasing diploid (sporophyte) dominance; telome theory to explain increasing division of labor and complexity in the sporophyte; origin of seeds; origin of flower. Several factors illustrate the general principles mentioned last lecture:–Early diversification of major group, followed by later winnowing (decimation and diversification).–Increasing complexity -- flowers composed of several types of modified leaves, illustrating division of labor–Trend from haploid to diploid dominance (why?)–Coevolution with insects! Illustrates another example of the importance of coevolution as a general principle.• 251 Myr - Mesozoic Era (Triassic, Jurassic, Cretaceous)Dinosaurs, flying reptiles, marine reptiles, mammals (Fig. 34.35 (8th); Fig. 34.32 (7th)), birds (Fig. 34.30 (8th) ; Fig. 34.29 (7th)), and flowering plants appear; insects, dinosaurs, and marine invertebrates diversifyinsect diversification: coevolution with flowers -- mutual adaptive radiation. Illustrates another example of the importance of coevolution as a general principle.conditions in the Triassic During the Triassic, almost all the Earth's land mass was concentrated into a single supercontinent centered more or less on the equator, called Pangaea. The Triassic climate was generally hot and dry, no glaciers, some swampy areas.diapsids: - two openings on each side of skull - lizards, snakes, archosaurs and their descendants (crocodiles, pterosaurs, dinosaurs, and birds)synapsids: - single opening low on each side of skull - mammal-like reptiles and mammalsEvolution #9, pg. 1plesiosaurs: marine reptiles of the Mesozoic.icthyosaurs: marine reptiles of the Mesozoicpterosaurs: flying reptiles of the MesozoicTurtles, lizards, snakes, crocodilians"dinosaurs": distinguished from other diapsid reptiles by erect gait (straight legs attached underneaththeir bodies). Dinosaur diversity: many types of medium- to large-sized predators and herbivores; limited in other ways such as lack of digging and climbing forms.Mass extinction at end of Cretaceous (dinosaurs, pterosaurs, icthyosaurs and plesiosaurs extinct): Pangaea breaking up, climate changing, sea level changing, meteorite impact (Fig. 25.15 (8th); Fig. 26.9 (7th))Luis Alvarez (UC Berkeley!): discovered that the usually rare element iridium is abundant in a thin layer of rocks that mark the end of the Cretaceous, and proposed that a large meteorite or asteroid (at least 10 km wide!) struck earth at that time and caused the Cretaceous extinction Almost all large vertebrates and many other species went extinct.At the end of the Cretaceous 65 mya, called the K/T boundary, almost all large vertebrates (dinosaurs, pterosaurs, plesiosaurs), many tropical vertebrates, most plankton and many tropical invertebrates, especially reef-dwellers, became extinct, andmany land plants were severely affected.  Surviving groups radiated to become the dominant flora and fauna today.Surviving groups, including insects, mammals, birds, and flowering plants on land, and fishes, corals, and mollusks in the ocean went on to diversify tremendously soon after the end of the Cretaceous. It was a major event in the history of life that profoundly affected life on earth since. No one doubts that the world would be very different had this mass extinction not occurred.  The probably impact crater has been located in Mexico.Later, the impact crater in Yucatan was found near the port city of Progresso and is known as the Chicxulub structure. The crater is 200-300 km in diameter and lies beneath 1100 m. of limestone. It was known to the Mexican national petroleum Evolution #9, pg. 2company (now Pemex). After the Berkeley group suggested an impact at the K/T boundary, Pemex scientists recognized that their observations were consistent with the idea that they had found the impact crater. Roughly 200,000 km3 of material was ejected and vaporized as a result of the impact. archaeopteryx: classified as the first bird (150 Myr). Distinguishing characteristics were feathers (asymmetric), wings, and an ability to glide, “dinosaurs” with proto-feathers and feathers have recently been discovered.modern bird diversity• 65 Myr - Cenozoic Era(Tertiary (Paleocene, Eocene, Oligocene, Miocene, Pliocene),Quaternary (1.8 Myr) (Pleistocene, Holocene (Recent) (10,000 yrs))Diverse forms of mammals, birds, flowering plants, and insectsMajor radiation of mammals, birds and pollinating insects. By end of Eocene mammals of every size and lifestyle had appeared with many similar to modern forms and others very different.Radiation of angiosperms, including appearance of grasses.Humans (Homo sapiens) appear in the PleistoceneMass extinction at end of Pleistocene, primarily non-marine, many large mammals extinct• Transitional FossilsMany examples of transitional fossils are known, e.g.,Paleozoic: “fish” to amphibians (tetrapods) (Fig. 34.20 (8th); Fig. 34.19 (7th)), amphibians to “reptiles”Mesozoic: mammal-like reptiles to mammals, ‘dinosaurs’ to birds, wasps to antsCenozoic: land mammals to whales (Fig. 22.16 (8th); Fig. 22.18 (7th)).• Primate evolutionEvolution #9, pg. 3The two major groups of the primates are the prosimians and the anthropoids (Fig. 34.37 (8th); Fig. 34.38 (7th)).prosimians: (“premonkeys”) lemurs of Madagascar, lorises, pottos, and tarsiers that live in tropical Africa and southern Asia.anthropoids: monkeys, apes and humans (see new display in VLSB outside library)anthropoid evolution: binocular vision, larger brain, opposable thumb, complex social interactionshominoids: apes and hominidshominids: humans and their direct ancestorshominid genera: Ardipithicus, Australopithecus, and Homo.hominid evolution: bipedalism, enlargement of brain, and


View Full Document

Berkeley BIOLOGY 1B - Evolution lecture

Documents in this Course
Notes 1

Notes 1

4 pages

EVOLUTION

EVOLUTION

12 pages

Evolution

Evolution

12 pages

Load more
Download Evolution lecture
Our administrator received your request to download this document. We will send you the file to your email shortly.
Loading Unlocking...
Login

Join to view Evolution lecture and access 3M+ class-specific study document.

or
We will never post anything without your permission.
Don't have an account?
Sign Up

Join to view Evolution lecture 2 2 and access 3M+ class-specific study document.

or

By creating an account you agree to our Privacy Policy and Terms Of Use

Already a member?