Formation of mountains – weathering, erosian..
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Transcript of Formation of mountains – weathering, erosian..
Formation of mountains –weathering, erosian.
Sedimentary rocks
Dating RocksRelative - Absolute
Nicolai Stenonis (1638-1686). "...at the time when any given stratum was being
formed, all the matter resting upon it was fluid, and, therefore, at the time when the lower stratum was being
formed, none of the upper strata existed.”
Steno’s Principle of Superposition
(Prodromus, 1669)
That is, in a sequence of strata, any stratum is younger than the sequence of strata on
which it rests, and is older than the strata that rest upon
it.”
Radioactive element Half-life
Radon-219 4 seconds
Iodine-131 8 days
Cobalt-60 5 years
Caesium-137 30 years
Carbon-14 5,730 years
Uranium 238 700 million years
Potassium-40 1.25 billion years
Radioactive Isotope Decays to Half-life (years)
Rubidium-87 Strontium-87 49,000,000,000
Rhenium-187 Osmium-187 41,600,000,000
Thorium-232 Lead-208 14,000,000,000
Uranium-238 Lead-206 4,500,000,000
Potassium-40 Argon-40 1,250,000,000
Uranium-235 Lead-207 704,000,000
Samarium-147 Neodymium-143 108,000,000
Iodine-129 Xenon-129 17,000,000
Aluminium-26 Magnesium-26 740,000
Carbon-14 Nitrogen-14 5,730
1 proton = neutron + electron.
An atom nucleus looses an electron:1 Neutron 1 proton.
( atom number +1, atom mass not changed)
An atom nucleus gains an electron:1 proton 1 neutron.
( atom number -1, atom mass not changed)
e = N-P; gains a N, loses a P
Radioactive Isotope Decays to Half-life (years)
Rubidium-87 Strontium-87 49,000,000,000
Rhenium-187 Osmium-187 41,600,000,000
Thorium-232 Lead-208 14,000,000,000
Uranium-238 Lead-206 4,500,000,000
Potassium-40 Argon-40 1,250,000,000
Uranium-235 Lead-207 704,000,000
Samarium-147 Neodymium-143 108,000,000
Iodine-129 Xenon-129 17,000,000
Aluminium-26 Magnesium-26 740,000
Carbon-14 Nitrogen-14 5,730
Accuracy of Radiometric Dating.
1. Several radioisotopes usually occur together in a rock and decay at different rates so the dates can be cross-checked. Nevertheless, invariably the dates agree.
Accuracy of Radiometric Dating.
2. The half-life of isotopes doesn’t change when scientists subject them to extreme temperatures and pressures or chemical environments.
Radiometric dating of meteorites:
the earth and solar system are 4.6 billion years old.
(Oldest earth rocks - Northern Canada:4.3 billion years old)
N gains 1 e (e = N-P)
Accuracy of Radiometric Dating.
1. Several radioisotopes usually occur together in a rock and decay at different rates so the dates can be cross-checked. Nevertheless, invariably the dates agree.
Accuracy of Radiometric Dating.
2. The half-life of isotopes doesn’t change when scientists subject them to extreme temperatures and pressures or chemical environments.
Accuracy of Radiometric Dating.
3. Radiometric dates coincide with dates obtained by other methods.c) Carbon dating agrees with the
historic record.d) Dates of the early paleozoic
coincide with dates calculated from annual and daily coral rings.
e) Radiometric dates agree with dates obtained from tree rings.
The Fossil Record
Fossils:= Remains of past organisms.
Actual (or petrified) body (parts) Excrements (coprolites) Gastroliths (stomach stones) Imprints (burrows, foot, feathers ) molecular residues
Coprolites.
Fossilization:1. Remains in water (river, lake, ocean)2. Sink to the bottom.3. Get covered by sediment
Fossils in sedimentary rock! Exceptions:a) tar pits (La Brea, Los Angeles)b) conifer amberc) sanddunes
TIME
Fossilization
Xing Xu stands among the remains of duck-billed dinosaurs in Zhucheng, China
Nature 6 September 2012 vol 489 p22
Fossilization:1. Remains in water (river, lake, ocean)2. Sink to the bottom.3. Get covered by sediment4. Petrified
Hard > soft body parts Aquatic > terrestrial
5. Discovery of fossils Exposure on the surface Timely removal
The fossil record must be incomplete
Fossil plant, Carboniferous
Turtle sex recorded in rock.
Jeholodens: early mammaliformes
(165 million years old)
Nature 1999, 398, p326.
Jeholodens jenkinsi
(165 million years ago)
Eomaia: common ancestor of the Eutheria or placentals.
(About 128 million years old)
Nature 2002, 416 p816.
Eomaia: common ancestor of the Eutheria or placentals.
(About 128 million years old)
Nature 2002, 416 p816.
Eomaia: common ancestor of the Eutheria or placentals.
(About 128 million years old)
Nature 2002, 416 p816.
Jeholornis: long-tailed, seed-eating bird of the early cretaceous of China.
(Nature 2002, 418 p405).
What does the fossil record tell?
1. The history of life on earth is old.
3.5 bya: first life
Stromatolites(2 .7 billion years ago)
What does the fossil record tell?1. History of Life: old2. Fossils are lacking in the oldest
layers. 3.5 bya: first life (bacteria) 1.5 bya: eukaryotes 0.7 bya: multicellular organisms 0.45 bya:fish 0.35 bya: amphibians 0.30 bya: reptiles 0.20 bya: mammals 0.15 bya: birds
TrilobitesOrdovician, Oklahoma
The fossilized remains of a pregnant mare and fetus (white circle) offer a glimpse into the reproduction of E. messelensis.
American Association for the Advancement of Science Science 2014;346:792-793
Published by AAAS
Archaeopteryx:A transitional fossil between reptiles & birds
Intermediate forms
Thick, bony wall around middle ear.
Large, powerful tail, shorter legs, fat pad in jaw for hearing, brakish water
Salt water habitat
Nasal opening shifted back, eyes on side of head
Tail flukes, very small hindlegs,
Echolocation for hunting
Complete loss of hind legs, nasal opening reaches position of blowhole
in living whales
Baleen for filtering food
Hippopotamus
(Pakicetus)
(Ambulocetus)
(Kutchicetus)
(Rodhocetus)
(Dorudon)
(Basilosaurus)
Reconstruction of the Tethys Sea in the Middle Miocene (45 Mya)
What does the fossil record tell?
1. History of Life: old.2. Fossils are lacking in the oldest
layers.3. Earliest life simpler ; more
recent organisms more comlex.4. Many extinct organisms.
Ordovician
What does the fossil record tell?
5. Ancient organisms were very different from living species, resembling modern species more and more as one moves up to more recently formed rocks.
What does the fossil record tell?
6. Fossils in adjacent layers above and below) were more similar to each other than to those found in layers more widely separated.
Crinoids
What does the fossil record tell?
7. Fossils in the most recently deposited rocks tend to resemble modern species living in THAT area.
Fossil marsupials were found in profusion only in recent sedimentary rocks of Australia, and that is where most modern (extant) marsupials live.
Thylacoleo carnifex (marsupial lion)
What does the fossil record tell?
8. There are no authentically anachronistic fossils!.
Island Biogeography
Biogeography:= Distribution of life on earth.
Islands:
Continental IslandsEngland (0.3 Mya), Japan, Sri Lanka, Madagascar (160 Mya)
Oceanic Islands: Hawaii, St. Helena, Juan
Fernandez, Galapagos
Hawaii
Galapagos
Juan Fernandez Archipelago
St Helena
Juan Fernandez Archipelago
Juan Fernandez Firecrown
Masafuera Ravadito
Marine Inguano
Hawaiian Islands
Hawaiian monk seal
St. Helena Wirebird (Charadrius sanctaehelenae)
St. Helena Wirebird (Charadrius sanctaehelenae)
Three facts about oceanic islands:
1. They are missing groups of species that live on continents and continental islands
2. The groups that ARE found on oceanic islands are replete with many similar species.
3. Often related, but not identical, to species living on nearby continents.
Compared to other areas of the world, life on oceanic islands is
UNBALANCED.
Native Missing
some Plants Land mammals
some Birds Reptiles
some Insects Amphibians
Freshwater fish
Good Colonizers
The End.