Saturday, June 21, 2014

PENT Archean to Mesozoic

A Planet of "Bacteria": most common form of life





Some stars (not Hollywood stars)
Mary Anning
The Iceman
The Bogman
Coelacanth
Cadborosaurus
Chewing teeth, hearing, warm bodies, “cute babies”
Cambrian explosion
Boyd Bushman
Obama/Attenborough meeting
Scotese continent animations

•Earth is unique in the Solar System:
    it supported life
.   Numerous earth-like planets in universe
.  Our solar system is not a 1st generation (~ 2rd)
. Earth went through many stages: One life form gave rise to another by necessity (reasons like change in climate or a disaster that killed many life forms)

Rise in Intelligence with time
One example is humans: size of brain increased as early humans worked hard to find food, planned a hunt, avoid predators or made tools
•There have been other forms of intelligent life before the humans appeared
Examples are cephalopods (like squid today). By imitating them we build submarines. Another example is Velociraptor 

Origin of Life
•Life almost as old as the earth
•Life on Earth is marine in origin(we see that in newborn babies, can swim & like water, also like climbing trees like our immediate ancestors)
•Earliest about 3.8 b.y. old in the sea
•Life didn’t move onto land until ~ 400 m.y. ago
•Needed enough oxygen as well as the protective ozone layer
•Plants moved first
•Animals did not have hard parts (skeletons)- not enough O2 in the water

How do we know about previous life?
•Simple: remains of previous life incorporated into sediments after death
•The sediments formed rocks which contain remains of life as fossils
•Rocks with fossils exposed to the surface today
•Discovered by prospectors/geologists/other interested people

Invertebrates & Vertebrates
•First animals (without skeletons) rarely become fossils, mostly stationary on ocean floor
•Some decided to explore & acquired skeletons
•First vertebrate was the fish
•During Carboniferous, vast forests & swamps with insects of tremendous size
•Fish stayed at water’s edge to hunt insects
•Became part-time land animals = amphibians

Land looked attractive
•Lots of food
•More oxygen to breath
•Protection from ozone available
•Less competition & no predators
•Became permanent residents = reptiles
•Some returned to the sea, because they sniffed food like ammonite meat & couldn’t pass up such a treat

A Landmark event
•Reptiles were the 1st 100 % land animal to appear on the Earth
•Its reproduction (the amniotic egg) method was a major achievement in the planet’s history
•Many of our features were created by the dinosaurs (such as chewing, cuteness of babies, warm blood, etc)
•Some colonized the skies by imitating the insects
•Climate got cold, too hard for cold-blooded animals
•The dust from the asteroid collision & the volcanoes that were created as a result finished most of the animals
•When the dust settled, there were only birds & mammals around
•This time the animals were warm-blooded and & could cope with a colder climate

Tree of Life
•Invertebrates -->  Fish--> Amphibians -->reptiles --> mammals & birds

Animals to Humans
•Dried-up forests of Africa brought the chimps (99 % identical to humans) to the ground looking for food
•Difficult to survive without fast-moving legs
•Required strategy of immense proportion – i.e. bigger brain
•Made tools & fire: a dramatic progress
•Made sounds, communicate, paint, travel, make a spear, make a boat
•Begin to wonder about the earth, religion, bury the dead
•Real progress in intelligence
•Now, we are able to destroy the whole humanity with nuclear weapons – practically insane

Genesis (Bible) versus Science
Both tells us a similar story if you could read the initial text of the Bible– in ancient Greek
(Ancient Hebrew text lost)
Some words have different meaning today, or words have many different meanings depending on the subject in question
The following from a publication of mine

•“day” or   verse      Events in   Events in       Radiometric
•  stage        in           Genesis    Science               dates
•               Bible                                                      (in 
•                                                                      billion/million
•                                                                          years ago)
•-------     -------       -----------     -----------        ---------------        
•                 1            Summary 
•                 2           Unformed
•                               matter
•                     (water=protons)
• First         3           Light         Big Bang        13.7  b.y.
•                                            First photons, protons
•               4,5     light divided 
                      from darkness  Atoms form    ½ m.y. after Big
•                                                                                      Bang
•                                             Last scattering
• Second  6–8  firmament 
                separating waters  Formation of stars/earth 4.6 b.y.
•                                              Creation of the earth

•Third      9,10  seas, land  form  Ocean, land      4.0   b..y.
•             11–13 green plants,
                   trees, seeds First plants on ocean floor  3.8 b.y.
• 
•  Fourth 14–19  sun, moon, 
                          stars           The sun is visible
•                                             First photosynthesis     3.0  b.y.
• 
•  Fifth    20–23 living things
                          in water,       First fish,insects      ~ 400 m.y.
•                        Flying creatures, etc
• 
•  Sixth    24, 25  all kinds of 
                       living creatures First land animals  ~ 300 m.y.
•                           reptiles
•               26–31  Humans        First humans             ~ 5 m.y.

It seems that someone from space is maintaining order 

By destroying some nuclear weapons 
. Their messages in crop circles and lights / sounds in the sky are amazing when studied
. Demonstrations of energy production without noise & poisonous exhaust would be beneficial if adopted my humans
•Remains of a factory waste processing tungsten & molybdenum, maybe 100,000 years old, found in Russia– this shows our planet is rare (has metals)
•Made their presence known since man created the atom bomb & nuclear weapons

EVENTS during Earth’s history
•It was all molten mantle to start with
•Crust formed from slow cooling of the magma
•Sea and atmosphere
•Later, creation of the continents
•Movement of the continents
•Mountains, reefs, deserts, coal & oil deposits
•Glaciations

UNIVERSE
•13.7 b.y. old & undergoes accelerated expansion
•Dark matter is 30 %: holds things together
•Dark Energy is 65 %: causes expansion of Universe to accelerate
•All visible matter (5 %) doesn’t have enough gravity to stop the expansion
Cosmic microwave background radiation: echo of the Big Bang (annoying hiss out of a communications antenna)

The Solar System
•One star: our Sun (= >99 % of mass)
•Planets & their moons (used to be meteors)
•Minor planets (Pluto & friends)
•Meteors from the Asteroid Belt, all combined together would form a small planet- but didn’t
•Comets from the outer reaches of solar system (Oort Cloud)

Distances in space
•Pioneer 10 spacecraft blasted off Mar. 1972
•Reached Jupiter   at 15km/s          Dec  1973
•Is now 13 billion km away
•Practically the edge of our Solar System
•Is aiming for star Aldebaran
•It will be there in 2 million years
•Only item that will outlast Earth- last forever
•Earth will be a Red Giant in 5 b.y.

Our Sun
•The Star : a nuclear factory
•2 Hydrogen atoms fuse to form one Helium, then,lithium, …………. last one to form is Iron
•The atoms bigger than iron created by supernovas
•Heaviest atom on Earth: Uranium
•Therefore, we are a “two-times re-processed material” very interesting to alien visitors

Planets & their moons
•Two groups of planets:
The Terrestrial &      the Jovian (Jupiter-like)
solid rock on surface                   gases
condensed at high Temp         low temp
very dense                                 low density
Fe – Ni alloys &                      ices of water,
silicates                                    ammonia, methane
Small                                                Large
                                                 radiate more heat than
                                                     they receive
      Few moons                          Many moons

Mercury
•Weak magnetic field
•Large solid core with thin mantle
•Many meteorite craters
•Some flood basalts
•Some cracks due to cooling of rocks in the interior
•Revolves around the sun very fast

Venus
•Brightest object in the sky
•“Earth’s twin”, similar size, but retrograde rotation
•Dense clouds of CO2 with sulfuric acid
•The ultimate greenhouse effect
•Air pressure on surface = 90 X Earth’s
•Very strong wind
•Recent volcanism

Mars
•The “Red Planet”
•Thin air with CO2, N2, no ozone. Most air escaped into space. Before, the greenhouse effect allowed water on the surface
•Strong wind up to 450 km/h
•Used to have stream channels
•Iron regolith with 13 % Fe –iron oxides & clay
•No organics in the soil
•Volcanic rocks ~ 50 % of surface
•Olympus Mons volcano ~  22 km high (tallest in Solar System)
•Polar ice caps with CO2 ice
•Landslides, craters & rift valleys
•No surface tectonism now

Ice Caps prominent (picture)        Mars “blueberries” (picture)
Hematite nodule: formed in water (picture)
Has to be sedimentary rocks (picture)    desert-like (picture)
Barchan dunes(picture)   wind storm (picture)

Jovian planets
•Small metal-silicate core
•Mantle with liquid metal, ice of water, methane & ammonia
•No firm surface
•Thick clouds rich in Hydrogen, water snowflakes & ammonia snowflakes
•Colors due to sulfur, phosphorus

Moons of Jupiter - of interest to us because of possible life
•Callisto: weak crust of ice + rock
                   mantle of water or water ice
                   no relief
. Ganymede: Craters & mountain ridges
. Europa: crust of ice, watery mantle
              “cracked eggshell” --> plate tectonics
            The largest ocean in the Solar system
            ~ 100 km deep
Io
•Sulfur-rich crust with molten sulfur mantle
•Active volcanoes
•No craters
•Brilliant yellow, red & brown
•Heat from tides of Jupiter

Enceladus: water under its ice?      Titan: atmosphere & surface lakes

Our Moon
•Receding 5 cm per year!!
•New Moon Blast Theory, 4 b.y. ago
•A Mars-size body hit earth at 50 km/sec. It set the stage for ocean tides & reproduction
•Evidence moon was closer: a Devonian coral had 3 ridges /year, so lunar month was 1 ½ day shorter
•Enough debris ejected from Earth’s outer layers (low in Fe) to form the moon
•Its movement is moderated (synchronized) so that its rotation period is the same as orbital period (27.3 days)
•No atmosphere (gravity force is too low to keep the air)
•Surface: “Highlands”      &    “Seas”
                    older rocks         younger rocks
                    4 – 4.6 b.y           3 – 3.9 b.y.
                    anorthosite         basalt
.  Soil: fragmentation of surface rock by meteors
            20 m deep
.  No hydrous minerals (clays, micas, amphibole)
•No water
•Chemistry: high in titanium
                        low in Fe, K, volatiles
.  Very thick lithosphere, cannot have plates
.  No magnetic field
.  Moonquakes : weak up to Richter 2
.  Density = 3.34 (Earth’s is 5.52)

Meteorites (3 types)
“Stony”: silicates of Fe, Mg    like our “mantle”
                    olivines, pyroxenes
“Irons” : Fe & Ni alloys               like our “core”
Carbonaceous chondrites: carbonates, water,
                  sulfates, volatiles – both high & low
                  temp. minerals: could not have
                  formed together, primitive solar
                  system material (not melted)

Falling stars, shooting stars, fireballs, thunderstones
•Travel very fast: 11 -70 km/sec
•Burn up by friction with air molecules, so they have a black crust, may fragment before hitting earth’s surface
•Expelled from the Asteroid Belt by collisions
•Fast collisions make craters, largest at Sudbury, 260 km across, 1.8 b.y. old
•Manitoba’s largest at Gypsumville, 40 km wide
•Largest recovered the Hoba Iron, S.Africa weighs 66 tons
•Down to micrometeorites
•The one responsible for the dinosaur demise was 10 km big & caused an “atmospheric blow-out” disaster
•People watch out for Near Earth Asteroids (NEAs) whose orbits may coincide with ours
•Aug.’72 “near miss” filmed over Wyoming

“Falls” v. “Finds”
•To see & recover a meteor is rare
•More frequently, one can find them in deserts or in Antarctica (frozen desert) or with a metal detector
•About 75 “finds” in Canada
•Finds named after nearest locality & owned by the finder (who can lease them to a museum)

•See Urals’ meteorite, Febr.15, 2012 (youtube videos)
•The largest since Tunguska in 1908
•Blinding glare from the East (direction of Sun, 9 am)
•A fireball, 3 min later a shock wave (air compressed in front of object)
•100,000 windows smashed, 1,500 people injured
•Explosion 23 km up, moving at 18 km/sec
•Force radiated by fireball ~ 90 kilotons (Hiroshima atom bomb was only 15 kilotons), but total energy delivered during entire entry was ~ 440 kilotons
•Meteorite was an ordinary chondrite with density of 3.6, therefore, should have been 18 m in diameter & 11,000 tons in mass
•Because it came from the east (China) many thought of a nuclear attack
Orbit
•Many cameras recorded the event, so scientists could work out direction and speed and it could be traced to its origin
•Another asteroid was coming 16 hours later, 2012 DA, in close proximity, but was much bigger.
•Two such extremely rare events occurred so close together, but were not related
•Meteor came from the Apollo group of asteroids – the largest class of asteroids whose orbits cross Earth’s
•Only Paul Chodas of NASA can calculate the orbits of meteors, comets, etc

Some meteorites / craters 
Tagish meteorite, Yukon, 2001: the most rare ever
-Willamette, USA’s biggest brought to the States by a glacier (from Canada)!
-Meteor crater, Arizona: best example of a crater
-Manicouagan: the “eye of Quebec”, 4th largest
-New Quebec crater, perfectly circular lake
-Peekskill meteorite broke a girl’s car in NY
The Sikhote Alin, Russia 1947: largest meteorite fall in history
Two volunteer astronomers spotting meteors/comets
Earth Impacts at a glance – red dots on the map
The meteor that killed the dinosaurs - poster

Comets (person with long hair)
•The comet of 79 AD was blamed for eruption of Vesuvius & destruction of Pompeii
Halley’s comet of 1066 was hanging in the sky for 2 months & “ favored” the victorious French at the battle of Hastings
•In 1665, one was responsible for the Black Plague
Influenza or flu was attributed to a passing comet
•Hale-Bopp in 1997: 39 members of the Heaven’s Gate cult in Calif. committed suicide to “take a ride” on the comet. Did they?
“frozen mudballs”, “dirty snowballs”
•Hale-Bopp was unusually bright & the farthest comet ever discovered by amateurs
•Originated from Oort Cloud, place of 1 trillion comets waiting to be disturbed
•Main body 15-20 km, usually peanut-shaped with long tail (coma) ~300 million km long
•Speed of 60 km/sec
Coma
•2 comas point away from the sun, top is dust & bottom is ionized gases
•Solar Wind vaporizes the ice & jets of water vapor & gases shoot out from the colder depths or cracks
•Comet’s fate is to crust over & suffocate becoming like a meteor
•Rich in hydrocarbons, aminoacids & organic molecules ---brought life to Earth?
Nucleus of a comet - picture

1994 crash on Jupiter (picture)

•Comet broke apart into 22 fragments as it passed Jupiter on its way to the sun
•Their orbits were predicted to crash on Jupiter a year later & all telescopes were looking when they created huge explosions bigger than the Earth
•If Jupiter is hit, it is possible Earth may get hit in the future

What does it represent?
•Primitive building blocks of the solar system
•“time capsules” of 4.5 b.y. ago
•Balls of ice & dust that did not get incorporated into planets
•Many probes sent to sample the coma & take pictures of the nucleus

Tunguska, 30 June, 1908

•Largest explosion of the century & also the mystery of the century
•Fireball from the SE, leaving a trail of light 800 km long, descending & shattered with cataclysmic explosions
•Tremendous noise, heard 1000 km away
•Explosion 7.6 km up, like 2000 atomic bombs
•Mass of 100,000 tons
•Magnetic storms & tremors recorded in Moscow
•“sky split apart” & great fire appeared
•People blown over 6 m
•Unusually colorful sunsets & sunrises continued for weeks worldwide. Bright enough at night to read a newspaper
•First scientists arrived in 1927
On the ground
•2000 km2 forest burned with radial tree-fall pattern (like a crop circle)
•Biological mutations & genetic abnormalities in trees / insects
•Some cosmic globules recovered made of Ca, Fe-Ni, silicates, Co-W, Pb
•It was like a nuclear blast
•The “thing” went back into space, 10 km large

Mystery problems
•Many favor a comet causing it
•No mushroom cloud, therefore not a nuclear explosion (as we know it)
•A meteor / comet cannot cause a geomagnetic storm
•In 1959 Russians reported radiation on the site, this suggests extra-terrestrial origin
•Explosion of a nuclear engine entering our atmosphere (it came at too shallow angle)

Long term results
•People started thinking about space
•Russians started the space exploration program (if someone came from space, we should go out and find out)

The USA followed soon enough. Space race had started

Fireball 2008, Alb /Sask border            The Buzzard Coullee meteor fall (pictures)

TELLING   TIME
Earth takes 365 days to orbit around the sun, but it slows down 
               It loses ½ sec in 100 years
                       or 5 days in 100 m.y.
               in 7 b.y. it will grind to a halt
However, the Sun will explode in 5 b.y.

BIOLOGICAL CLOCK
Our bodies are regulated by slight pull from the moon
The 28-lunar month -24.9 hours for a lunar day- affects mostly females ( hormonal cycle, period)
Also the blind  & those in polar winters (dark) follow the 24.9 hour clock acc. to the moon rise and fall
Tides also follow moon rise & fall

ABSOLUTE DATING
Many “clocks” were tried in the past to find the age of the earth
. 1600’s   Bishop Ussher   bible/counting generations    4004 BC Oct 26 9am
.Mayas                                                                                     3114 BC – 2012 AD
. 1800’s George Buffon       cooling of iron spheres                     75,000 years
. Late 1800’s Lord Kelvin     cooling of molten rock                 20 – 40 m.y
. 1899              John Joly      salinity of the oceans                         100 m.y.
. Early 1900’s  Madame Currie    radioactive decay                       4.6  b.y.
.   today                             more than 40 radiometric methods     no change

The NAMES we use
“month” from  “moon”                              (French name)
Monday                         moon                      Lundi
Tuesday       (Tiw’s)      Mars                       Mardi
Wednesday (Woden)  Mercury                 Mercredi
Thursday     (Thor)       Jupiter                    Jeudi
Friday          (Freya’s)   Venus                      Vendredi
Saturday                       Saturn                     Samedi
Sunday                          Sun                          Dimanche

William Smith, “strata man”
“Discovered earth’s strata on company time”
Canal surveyor, a misunderstood genius
Compiled a complete geological map of England & Wales based on fossils, published in 1815

Bedding in sedimentary rocks (picture)        Geological fault (picture)

9 Laws (principles) of Stratigraphy
1. the principle of Superposition
2.  ‘          ‘           ‘   Original Horizontality
3.  ‘          ‘          ‘  Original Continuity
4. Cross-cutting Relation
5. Inclusion: a rock fragment is older than the rock that surrounds it
6. Metamorphism

3 principles on fossils
7. Faunal Assemblage : unique to an interval of time
8. Faunal Succession: Life changes with time
9. Correlation: Same assemblage of life means same age

Explanations of Laws
1. younger layers on top & progressively older downwards
2/3. since sediments laid down in the shallow ocean, the layers are originally horizontal and continuous
4. If layers are disrupted / offset by a fault, the fault came afterwards
5. Inclusion could be a fossil. The animal is older than the rock it is found in
6. Metamorphism is later, it affected a previously un-metamorphosed rock
7. The group of fossils in a layer is unique (like the composition of our class)
8. Vertically layers have different groups of fossils
9. Comparing fossil assemblages from one area to another, if you find same fossils, it must be the same age

Unconformity
An interruption in the geologic record (like pages missing from a book)
Rocks missing because the area was dry land & erosion of exposed rocks took place and nothing was deposited

Hutton’s unconformity in Scotland (picture)

Radiometric Dating

Radioactive decay
Can be compared to an hourglass
Radioactive elements give off:
 -alpha particles: 2 neutrons + 2 protons  can be stopped by a piece of paper
 - beta particles: electrons     can’t go through skin
 - gamma radiation: extremely powerful (more powerful than X rays)
When an igneous rock crystallizes from the liquid state, a large variety of chemical elements are “frozen” into the host minerals of the rock
Some of these elements are unstable & their atoms spontaneously change into other atoms (daughter atoms or isotopes) through the process of radioactive decay
Rate of decay
Is constant
Measure amount of daughter element and parent element to find age of rock
For uranium, the daughter product is lead
About 20 radioactive elements exist, most decay extremely slowly
Only 4 radioactive isotopes useful for dating
Potassium -40, rubidium – 87, uranium – 235 & uranium - 238
There is a mineral called “Zircon”
Minerals with uranium are very rare
However, minerals with uranium in trace quantities are common
Because of its excellent stability, zircon is found in certain rocks that formed throughout Earth’s history
Excellent for the uranium / lead method in geochronology 

Carbon 14 method of age dating half life = 5,730 years 
For specimens younger than 70,000 years
Can date formerly living material
The C 14 clock starts ticking when an organism dies & is no longer taking C from the environment
C 14 is produced in the air by bombardment of cosmic rays which turn a certain proportion of N 14 into radioactive C 14
All organisms take in C 14 with the carbon they use for energy, at a ratio of about 1 in a trillion
Once it dies, the C 14 begins to decay

Tree ring dating
Back to 14,000 years

How old ? Nat. Geog. Sept 2001
Hubble Constant: galaxies move away from each other at speeds that increase proportionally with distance
Quasars & galaxies speed off, & their light that they emit lowers in frequency & shifts towards the red end of the spectrum
Fortunately, nature has created the perfect clock for geologists: Zircons are God’s gift to geochemistry

Examples of dates
Grand Canyon: bottom layer 2 b.y.
                                    top layer   250 m.y.
. Carving of the canyon started about 5 – 6 m.y. ago
.The Pyramid in Egypt: 4,440 years old ? From the alignment of pyramids with 2 polar stars visible at the time
. Saber Tooth Cat skull: 12,000 years old by C14
. The Shroud of Turin: 610 -740 years old by C14

Geological Time Scale

THE PRECAMBRIAN
Cambria: ancient name for Wales, U.K.
Where they found oldest fossils a long time ago
They thought there was no life before then
However, since then evidence of microscopic life forms plus soft-bodied creatures emerged
One can say that Precambrian is the Age of Bacteria 
The PRECAMBRIAN –lasted 21 hours of a day

Archean  4.0 – 2.5 b.y.                         Proterozoic 2.5b.y.—542 m.y.

Superior Province                                Churchill Province

Precambrian scenery (picture)

4.0 b.y. ago: collision
Mars-size asteroid (500 km big)
Experiments done (video)
Problem was HEAT generated by the impact
Evaporated all oceans
Still life survived or started right after
Conditions then
Hot temperatures, molten mantle on surface, lots of volcanoes
No oxygen in the air
Atmosphere: methane, ammonia, hydrogen
Oldest part of every continent called a SHIELD, because it has that shape in section
No magnetic field (need solid iron moving in the core)
The Canadian Shield has the largest exposure in the world – some parts are covered by later formations
Shields are made up of many parts amalgamated together by collisions
The margins of the shield are covered by later sedimentary rocks when they were submerged by the sea. These are called Platform areas. In Manitoba they cover the NE & SW corners

SHIELDS
Made up of two parts: Granite / gneiss & greenstone belts
Granite/ gneiss formed under the mountains
Volcanic & sedimentary rocks make up the greenstone belts. Their color is due to the abundant mineral chlorite. They may contain mineral deposits that formed along rifts
North America was part of Laurentia that also included Greenland & Northern Europe
Mountain Belts
Events in the Archean
Early: volcanoes, island arcs, mid-ocean rifts
Late: mountains from collision of volcanic belts, granite, gneiss, metals
10 hours in a day
All rocks completely deformed, rare fossils
Surface: hot, molten, lots of volcanoes
No magnetic field
UV radiation, moon was closer, strong tides
No crust to start with - evidence from meteorites
It took 0.5 b.y. to form some crust
High heat flow as the crust is thin. As it gets thicker, heat is trapped inside the earth. Released by plate tectonic processes
First Ice Age in lake Huron (2.5 b.y.)
How Ice Age can start: too much sulfur dioxide in the air (it blocks the sunlight)
Events of the Proterozoic 
In Manitoba: Trans Hudson Mountains (THO)
The tallest in Earth’s History (15 – 20 km high)
We know because the metamorphic minerals on the surface today (such as garnet) formed under the earth at depths of 15-20 km
Lynn Lake, Flin Flon, Snow Lake: metals  from black smokers in mid-ocean rifts – copper, zinc, nickel with some gold / silver
Supercontinent Rodinia formed 1.3 b.y. & broke apart 750 m.y.
Snowball Earth: 800 – 650 m.y. 
Too much sulfur dioxide in the air probably created it
With time carbon dioxide was produced under the ice and eventually broke through the ice and raised the temperature of the air
That is how the Ice Age ended
IRON
Was dissolved in the sea making the water red
When oxygen became available from bacteria, iron turned into oxide (magnetite) and was deposited on the ocean floor, like a sediment
This was the Banded Iron Formation (BIF)
Deposited between 2.5 b.y to 1.75 b.y. ago
Never formed again since
Today, it is the source of iron
Since that time iron is produced by weathering on land and gets oxidized into hematite (rust). The result is rocks stained red
So we have the “Red Beds” forming ever since instead of BIF
Rodinia, 1.1 b.y. ago (picture)
Snowball Earth
LIMESTONE
CO2 also caused limestone to form for the first time (it forms in warm, shallow seas)
Limestone trapped CO2 from the air and prevented Earth from spiraling into a never-ending greenhouse inferno like Venus’s
Explosion of Life soon after Snowball Earth
Unique rocks
Because Earth was bare of soil & trees (only trees keep the soil in place) the sediments were made of pure quartz (good for making glass)
Greywacke, made up mostly of clay & sand, formed in submarine slides (due to its clay content). It never formed since

Precambrian Metal deposits
Iron – most of the world’s
Nickel – most of the world’s
Uranium – most of the world’s
Copper – zinc
Gold, silver – a big part of the world’s
Titanium (Cross Lake)
Platinum – all of the world’s
Pegmatites with lithium, cesium, beryllium, tantalum
Gold: exceptional properties
One of the noble metals (resists chemical action, does not tarnish in air/water)
Only soluble in aqua regia
Can be alloyed with silver (electrum) & mercury (amalgam)
100 % pure known as 24 carats, but is soft
Malleability: 31 gr (1 oz) can be drawn into a wire more than 100 km long
Will make a perfect frying pan (no metal smell in food)
Excellent conductor of heat / electricity
Reflects IR light efficiently – used in office windows (only need a very small amount)
Extremely small amounts in perfume bottles, but it looks like a lot
If you see a small speck underground, you think it is as bright as the sun!
Copper (name from Cyprus, “Kypros”, in Greek)
Conductor of heat & electricity
Used in alloys such as brass / bronze
Also needed in the living in trace amounts
Nickel
Alloy with iron, stainless steel (no rust)
In loonie coins (that is why they created the coin, to use up Canada’s nickel production when price was very low)
Last time nickel was used in coins was by the ancient Greek kings in Afghanistan 200 years BC. They took the art of making nickel coins from the Chinese in exchange for method of making fortifications of cities (Wall of China)
Zinc
Used mostly in galvanizing iron (for example, nails have a whitish zinc coat so that they will not rust)
Beryllium
Light in weight
For aerospace industry
satellites
Lithium
The lightest metal
Mostly used in batteries (electric cars will use these when they will be in production)
A lithium mine in Manitoba, one of few in the world
Tantalum
Chemically inert
For capacitors in computers / mobile phones
For bone repairs

PRECAMBRIAN LIFE
Ingredients of life may have come by comets & some meteorites that contain aminoacids
Bacteria was the first & is the most abundant organism on Earth
3.8 b.y. Sulfur bacteria: oldest fossil. It forms in sulfur springs & black smokers. Breaks down S compounds from volcanoes to get the energy - chemosynthesis

Chemosynthesis
Fist form of life on earth
Found along ocean’s rifts where black smokers accompany the extrusion of basaltic lava
Clouds of superheated steam at ~ 400 degrees C charged with metals & hydrogen sulfide
Source of energy is the oxidation of sulfur compounds
Basis of food chain is bacteria
Bacteria metabolize sulfur gas
Giant invertebrates like blind crabs, 30 cm long worms, 60 cm clams & 2 m long blood-red tubeworms (have no mouth or stomach, bacteria live in their interior sac, they shoot minute stinging tentacles into the current to capture food)
Abundant food gives rise to Giantism
All live short lives & reach maturity 500 X faster than in shallow water 
Tube worms
Are like giant lipsticks
Tube is made of chitin
Symbiotic with bacteria
Bacteria metabolize H2S to produce carbohydrates--> energy 
H2S gas is toxic to life on land

Fossil black smokers
Today, represented by accumulation of metal sulfides of copper, nickel, zinc with gold, silver & also graphite (from organic remains of plants/animals)
Examples in Manitoba are in Thompson, Flin Flon, Snow Lake, Lynn Lake & Leaf Rapids

First photosynthesis CO2 + H2O-->  sugars + O2
Blue-green algae (cyanobacteria) fossils 3.0 b.y. old
Built stromatolites, cabbage-like mounds on the sea floor (still do that today)
Some of the first oxygen produced used to precipitate the iron in the sea to form BIF
After that, oxygen released into the air & killed other types of bacteria (“Gas Attack” ~ 3 b.y.)

Stromatolites: Earth’s First Fossils
Video: “Life from the Sea”

1.5 b.y. ago
Dramatic increase in size of micro-organisms
Bacteria combined with a nucleus bacteria to form a co-op  first single-cell animal
These animals incorporated cyanobacteria to form the first single-cell plants
Earliest cells were prokaryotes (no nucleus), reproduction by division
Later, eukaryotes (nucleus to protect organs from oxygen)
The invention of sexual reproduction, a definite speed up of evolution. Increases VARIATION among individuals

Multicellar animals from 750 m.y.
Each cell has specific function (tissue, organs)
The first animals were soft-bodied, left impressions as carbon films in rock by the process of distillation (carbonation)
Ediacaran Fauna: from 600 – 542 m.y.
Early forms had to make their own food (use sulfur compounds, sunlight & break down sugars)

Burgess Shale
Later invention was to eat another organism – only need to break it down with the help of oxygen
This is the first PREDATOR
In the Burgess Shale Fauna the predator was difficult to identify. It was called Anomalocaris
This Fauna was part of the “Cambrian Explosion”, all phyla evolved at once, then, nothing else since

Burgess Shale Fauna: World Heritage site
520 m.y. old, extends for 20 km along a side of a mountain, near Field, BC
Found by Walcott, 1909, 2,300 m altitude
The world’s most significant fossil find
Unusually diverse fauna of soft body animals
Ancestors of invertebrates, even an ancestor of all vertebrates – Pikaia
All known phyla of invertebrates are represented plus some others who did not survive
Pikaia: ancestor of all vertebrates
Hallucigenia (wrong way up)       Right way up

Excellent preservation in fine mud. Deep water environment below a shallow water algal reef
Mudflows carried animals over the reef, killing them & burying them in mud
Details like muscles, gut, fins, spines
200,000 fossils recovered
It is an extraordinary buried treasure, the animals have NO BONES

Philosophers have debated
Many questions are raised here: how are body plans constructed & how new phyla emerge?
Two kinds of opinions
Stephen Jay Gould: proposed the Marxist view that Human is an accident (in evolution). His book, “Wonderful Life”, 1989 was a best seller
Simon Morris: proposed the Christian view, that Intelligence will always come in the end
Anomalocaris: First PREDATOR 
Walcott quarry

History of Life & Fossilization
Life started about 4 b.y. ago & until 400 m.y. ago was entirely in the OCEAN
No life was possible on land due to bombardment of UV radiation from the sun
As soon as the level of oxygen in the air was ~ 10 %, the ozone layer started forming, which blocked the uv
Onto the land
First to conquer the land was the plants
Then the insects, which could decompose the plants
Finally, the fish who could avail of the abundant insect food on land

Animals
Invertebrates
Have external skeletons
First abundant animal life on Earth
Their fossils are so numerous & essential to make up the Earth’s History

Vertebrates
Internal skeletons
An invention to TRAVEL & look for food elsewhere
Fish was the first vertebrate animal

The Invertebrates
9 phyla or groups – all possible structures that nature could produce
Protozoa : have single cell- foraminifera have built the pyramids & responsible for oil/gas deposits
Porifera (sponges) : are primitive
Coelenterata: the corals
Bryozoa : moss-like animals
Brachiopods : ancient clams, stationary on the ocean floor
Molluscs: 3 subgroups- gastropods (snails), pelecypods (modern clams) & cephalopods (squids, octopus)
Echinoids : 5-fold symmetry
Arthropods: trilobites, today mostly insects
Graptolites: extinct plankton

Size of Life forms
From microscopic
Examples:
Diatoms (plants produce ¼ of our oxygen)
Foraminifera
Radiolaria
Bacteria: every time we wash our hands, we get rid of 25 million bacteria

To monsters 
Examples:
Giant squid, 8 m long
Dinosaurs 30 m long
Marine reptiles 13 m long

Fossilization
Living things have soft parts (decomposed by bacteria) & hard parts that can be preserved (usually made of calcite that reacts with the acid)
For preservation it is necessary to be buried in sediment
In unusual circumstances even soft parts can be preserved – like the Burgess Shale of deep water environment
Unaltered preservation
1. In ice    -Iceman in the Alps- 5,300 years ago
                                                    (in the Bronze Age)
                    - Iceman in BC – 500 years old
                   - Frozen mammoths in Siberia, also in
                           Canada, but ice has melted, only
                            tusks can be found

2. mummies     - in Egypt (dry climate)
                               - in Peru mountaintops,
                                        sacrificed maidens
3. in amber         trapped insect by the sticky-ness, attracted by smell. Resin polymerized when fossilized

4. tar pits          Los Angeles La Brea. Cenozoic with animals as old as 30,000 years

5. bogs, swamps       Denmark: body with rope around head from about 100 BC. In his intestines were seeds with disease that made him behave with mental problem - doped

La Brea tar pits, Los Angeles (video)

Altered
1. opal
2. petrified wood – silicified & permineralized.
                                       molecule by molecule
                                       Souris, Manitoba
3. pyrite in shells
Methods of alteration
Permineralized: cavities filled-in in teeth & bones. Much heavier than original
Distillation / carbonation : plants & insects, only carbon left, black in color
Impression: casts (internal) & molds (external)
   only shape preserved, skeleton dissolved
. Trace fossils: evidence that organism was there- footprints, burrows, borings, coprolites, gastroliths

The Iceman
Found in 1991 in the Alps
World’s most ancient intact human
46 years old, 1.6 m tall, 50 kg weight
Tatoos on lower spine, ankles, knees, normally covered by clothing, not for show off 
Hair cut
Body brown & dried out, mummified naturally
Trapped in ice at 98% humidity & - 6 ‘C (like our freezer)
Leather shoes were straw –insulated
Cap of brown bear fur
Wooden backpack with copper ax, stone dagger, bow from yew tree (the best in Europe), leather quiver with 14 arrows- flint points & feather- & an arrow repair kit
Food: berries & mushroom with infection-fighting properties
After thorough investigation
Killed by a flint arrowhead in an area with blood vessels, shot from behind
Deep wound in right hand, so he had hand-to-hand armed combat
Arthritic & infested with whipworm. Seriously ill 3 times in last several months
Cu, As in his hair: involved in copper smelting
Surprised investigators that he recently ate cereals & ibex meat (a real feast!)
Amber : name means electron
“gold of the north” : Baltic
Fossilized resin (burn: incense)
As old as Carboniferous up to Pleistocene
Most common in Cretaceous, Tertiary & Quaternary
Occurrences
With lignite beds
Coal beds
Sandstones
Clay shales
In Manitoba: Cedar Lake, excavated by Sask. River along its course
Uses
For varnish & lacquers
Burned as incense to dispel evil spirits & fumigate against mosquito (beware: the burning should be done indirectly)
Sailors to drive away sea serpents
Applied to violins
Removes lint from clothing
Jewelry & rosary beads

Beware
Hairsprays & perfumes will make a whitish coat that may be permanent
Kitchen substances or sources of heat will damage it

Opal
Hydrated silica. Water content varies, so is the color
Iridescent: rainbow effect from reflection / refraction of light as it passes through
Forms in volcanic areas
Hot groundwater seeps through replacing wood by hydrated silica as spheres
It is the alignment of these spheres in a bath of silica solution that creates the iridescence

Deposits
Coober Pedy, Southern Australia
E. Slovakia is the original site since the Roman times
Honduras
Mexico

Lab on Fossils

Lab on Fossils: some conclusions
“Scuba diving”: is to admire bright colors of the living invertebrates
People who live by the sea paint their houses with these colors
The invertebrates produce these COLORS:
    - certain clams, oysters produce purple (symbol of royalty) & red – also known as porphyry- (symbol of the Byzantine Emperors) also, the hierarchy in the Andes

    - squid produces black ink (to confuse predators)
----plane of symmetry of animals & humans
----You can eat inside of invertebrates raw (but beware of pollution today)
----Clam shells found to clean water from pollution (student project in Nova Scotia) 

Suture in ammonites: how soft parts are attached to the skeleton. The shorter the suture line, the easier to get eaten. So, the ammonites were intelligent, because they made their suture much longer, so they could survive from predators
The ammonite skeleton also has inter-connected chambers where air is passed along. The more air, the higher it climbs in the water. The less air, the deeper it can go.
This mechanism was “borrowed” by humans to make submarines

Sea shells: symbol of Australia (picture of the Sydney Opera House)

Ages
Precambrian              Age of bacteria
Paleozoic = old life    Age of invertebrates
Mesozoic = middle life  Age of Reptiles
Cenozoic = recent life    Age of Mammals

The PALEOZOIC : summary of main events 542 – 250 m.y.
Lots of shallow water (snowball had melted)
Appalachians in North America formed
Continents drift & combine to form Pangea
Unique environment in the Carboniferous: immense tropical forests that turned into coal
Widespread deserts in the Permian
Skeletons formed (there was enough oxygen)
“Explosion” of invertebrates (Cambrian explosion)
First fish, first amphibian, first reptile
Land plants, insects
Largest Mass Extinction on record (“Permian Death” or “The Great Dying” ) at ~ 250 m.y.

Environment
Shallow water: good place for life, soft bodied animals picked up O2 & CO2, Ca 2+ from erosion to form skeletons
Protection against predators
Their skeletons formed limestone
Previously plants manufactured their food from a gas (CO2) in the air
Now animals use O2 from plants to break up their food – very convenient
Sedimentary rocks form in shallow water from sediment transported by water/wind
Sand is no longer pure quartz
Shale in deeper water is rich in carbon and O2-poor. No scavengers in deep water

Reefs
Previously reefs were constructed from bacteria. Now invertebrates added, living in symbiosis with the algae
Reefs are barriers against waves of the ocean
The back-reefs are tremendously rich in invertebrates
If the sea level falls, the lagoon dries up depositing the salts dissolved in the water 

Evaporite deposits
In order of deposition:
1. halite
2. gypsum & anhydrite
3. magnesium salts
4. The last to form is potash

Continents
N. America had combined with Europe & Greenland to form Laurentia
Now, Laurentia + Asia = Laurasia
S. America + Africa + Australia = Gondwana
Finally,
Laurasia + Gondwana = Pangea
One detail: Florida was added to N. America, it was part of Africa

Videos on “supercontinents” on youtube
The earth’s continents for past 4.4 billion years
    (video probably by a teacher, uses today’s outline of continents, 2 minutes)


 .  Earth 100 million years from now (has exact shape of old continents, 3 minutes)

Mountains
The Appalachians were prominent like the Rockies. It is the result of collision of continents. Afterwards, erosion has lowered their peaks
3 stages:
Subduction of Iapetus under Laurentia
Caledonian Mts from subduction of Iapetus under N. Europe
Result was volcanic rocks & Red sandstone
Acadian: Baltica collided with Laurentia, uplift & deposition of red clastic rocks on land from erosion (red from iron oxides)

Carboniferous
A unique environment: widespread forests in N. America & Europe – in tropical climate
Forests & swamps periodically flooded
Sea level rises & falls due to glaciation in Gondwana
Cycles of non-marine deposits: sandstone + coal & marine shale and limestone

PALAEOZOIC   LIFE
First skeletons: protection from predators, protection from UV & attachment of muscles
In Cambrian: 50 % of fossils are trilobites – they lasted 340 m.y.; they have very advanced eyes – with 360 degree view of the sea for protection
From Ordovician get corals, graptolites, etc

360 degrees view (one of two eyes) - picture of trilobite eyes

First Fish
530 m.y.: Jawless Agnathids later get extinct
450 m.y.: Jawed with gills turning into jaws
                     Placoderms later get extinct
.Cartilaginous : primitive – sharks & rays
. Later, bony fishes appear of two types:
                         a. ray fins (most fishes) &
                         b. lobe fins with bones. These turned into amphibians 

Jawless fish          Placoderm (scary!) 

Archeopteris, first tree
Early fish developed lungs, vital to jump onto land. Lungfish breaths air, it lives in freshwater
A 360 m.y. old tetrapod from Greenland had 8 fingers. Limbs were not for walking, but pushing logs in freshwater lakes/swamps
Earliest footsteps, 348 m.y. old, in W. Ireland

Devonian  
The “Age of Fishes”
First time they are abundant

First Land Plants
Vascular 
First populated along the shores. Soil now can stay on land – kept by roots. This slowed down erosion, nutrients stayed on land. Enough oxygen (O2) in the air (from plants) to form the ozone (O3) layer
With plants on land, bacteria would stay on land to decompose them, so the insects invaded the land to feast on them. Dragonflies were 60 cm long (giants) & cockroaches 10 cm, etc

Animals
Fish turns into amphibian to avail of abundant insects – therefore, first amphibians were  meat-eaters
Later, amphibians turn into reptiles – the first 100 % land animals
Primitive reptiles were Dimetrodon (“sail-back”) & Theraspids, forerunners of mammals

Our babies
One can see various stages during their development
Embryo has eyes on the side (fish, amphibian, primitive reptiles), then they move to the front (advanced reptiles, mammals)
When baby is born is able to float (swim) in water
Mother’s womb is a bit of the ocean. Last stage before was the chicken egg. Mother has the egg –so to speak – inside the body. Why? For protection

Dimetrodon

New invention in plants
Gymnosperms
Female seeds stay on plant while male seeds are spread by wind (hit-and –miss)
Conifers survive in winter (that is why they were invented)

Manitoba in the Palaeozoic
Limestone with reefs & caves
Evaporites: gypsum, anhydrite, halite underground comes out as salt springs
Williston Basin: oil / gas deposits

Landmark events
Searching for the first animal: 570 m.y. South China, embryos in the earliest stage of division
First steps on land: near Kingston, Ont. 478 m.y. Arthropod trackways in sandstone, ripple marks in a dune, 8 pairs of legs moved in unison (like oars, rather than one after the other), must be on land
First land walker : Scotland, 345 m.y. tetrapod, amphibian, croc-like

First steps on land: Tetrapods

Walking feet
First proper walking foot, thought to be in a fish: one limb has complete foot attached with 5 digits, 1 m long
Has a twist on its bones that allows it to bring its feet forward for walking
Previously, feet pointed out or back for swimming
A decapitated chicken runs for a while without the brain (spinal cord regulates the locomotion)- in a salamander diagonally opposed limbs move together

Transformations
Ocean plants to Land plants
Fish to Amphibian
Amphibian to Reptile
Reptile to Mammal
Reptile to Bird
Warm-blooded animals
Cold-blooded animals

Ocean plants to Land plants 400 m.y.
Modifications needed:
Resistant to drying
Get roots to obtain nutrients from soil
Ability to transport water from roots to higher parts where photosynthesis occurred
Respire in air
Get strong to support against gravity
First reproduced by spores, which had to go to water to be fertilized

Primitive fish
No fins, no jaws
Armor of thick plates & thick scales
Some are 10 m long, look like armored tanks!
With time the front gills turn into lungs

Fish into Amphibian 370 m.y.: “Not so Great a Change”
Fins turn into limbs
Return to water to lay eggs
Larvae have gills that turn into lungs
Thick, scaly skin to avoid drying out
3-chamber heart to pump blood
Moved eyes from side to top of head
Early amphibians had tail fin like a fish 

Amphibian to Reptile 340 m.y. “A Major Change”
Most important: amniotic egg (leathery shell for protection, contains water, shell allows exchange of gases O2, CO2 – it was like a private pool!
Thicker, scaly skin to protect body against drying
Primitive had limbs on side, later limbs underneath
Hind legs stronger
Front legs lifted off ground later
Tail as balance
Cold-blooded first, some prob. Became warm-blooded
Dinosaurs are advanced land reptiles
Stronger lungs

Reptile to Mammal  200 m.y.
Warm-blooded
Produce milk from sweat glands + suckle young
Live young (“egg” inside mother)
Hairy skin to keep temperature
Complex teeth
Highly active (high metabolism)
Separate passages for air & food (so young could suckle from mother)
Breathing assisted by chest diaphragm
4-chamber heart
Typical mammalian string of sound-conducting bone (originally a reptilian jaw joint)
Large brain / body mass ratio
The marsupials were primitive mammals – the embryo stays in pouch & suckles

Reptiles to Bird   175 m.y.
Hollow bones (hard to fossilize)
Powerful arm muscles to flap wings
Rigid breastbone + vertebrae
Keen vision
Sense of balance
Landing requires retractable feet
Flight requires enormous energy (warm-blooded)
Insulated cover (fur, feathers) to keep body warm
Wings tucked away (Pterosaurs could not do that)

Warm blood?
To protect life during the Ice Ages – must have suffered a lot, so decided to make changes
First it was the dinosaurs who changed
Later was passed on to mammals & birds

Warm-blooded animals: mammals, birds
Temperature at 36.6’ C
Walk upright
Food intake & rate of metabolism is 2 – 10 X that of cold-blooded
Production of heat more efficient
Temperature is maintained by ‘waste’ heat of metabolism
Bones have blood passages
Heat retained by insulation (fat, fur, feathers)
Less difficulty coping with cold weather (shivering produces heat)
Poor radiators (few degrees higher than 36.6’ C is lethal

Cold – blooded animals: fish, amphibians, modern reptiles 
Temperature same as the environment
Legs on the side
Low food intake & low metabolism
½ of energy in food is released
Uses devices like “sail-back” & hibernations
Low blood pressure

Late Paleozoic plants: Group name, features, examples, method of reproduction, height, today
Psilophytes: most primitive, spores, 0.5 m
Lycopsids: “scale trees” leaves directly from trunk, Lepidodendron, spores, 30 m club moss
Pteridosperms: seed ferns, Glossopteris (tongue-leaf), seeds, 12 m, Lowly ferns
Sphenopsids: Jointed stems, Calamites (reed-like), 12 m, spores, Horsetail, Scouring rush
Pteropsids, True ferns, spores, 20 m, ferns
Gymnosperms (means naked seeds): cycads, conifers, Ginkgo, seeds, 30 m, pine, spruce. This was an invention to protect from cold during Ice Ages

Formation of coal & oil/gas
Plants                                            Animals
Get buried                                     Get buried & become
Peat, Lignite shallow                    Tar (asphalt) shallow
Coal deeper                                   Petroleum below 2 km
Anthracite much deeper                Natural gas (methane)
Below 9 km turn into graphite      Below 9 km all are
At 150 km turn into diamonds       destroyed

Coelacanth: Fish with legs : A "Living Fossil"
A “living fossil”
Spotted in fishing market by Mrs. Latimer, 1938 in South Africa. No fridges then, soft parts decayed. Expert came 2 months later
No backbone, empty spine filled with oil under pressure, can swim very deep, low metabolism, needs little food
Gives birth to live young (200 m.y. before mammals appeared!)
Observe lobe fins in motion: like walking
Blue color with blue eyes
At depth lots of oxygen, can’t survive in swallow water
The tail is very distinctive, belongs to the primitive fish
Appeared 350 m.y., closest living relative of the first fish that came ashore to live on land, 360 m.y.
Rarely found in water less that 200 m deep
Still air-breathing, 3-lobe tail, 1.5 m long 45 kg
Covered with white splotches & looks like a sponge (camouflage)
Several rows of pointed teeth
Eyes are lined with reflecting cells that enhance vision, sensory system detects weak electric signals emitted by other life forms
Live young, 5 – 25 babies

Fossil forest underground in Illinois - picture          Primitive fish: Dunkleosteus - picture

Sturgeon: primitive fish in Manitoba
No backbone, but a notochord
First of the ray-finned fishes to appear
No scales, tail like a shark, lives long & produces few offsprings
Commercial fishing in Manitoba stopped in 1992 

Salt lakes in Saskatchewan
Manitou Beach, Watrous lake (name from “Waters Work Wonders”, or “doctors” lake)
You float in the water
Cures fever, clears up skin eruptions, eases pain for arthritis
Slightly oily water puts an end to constipation
From the cured: lumps on skin, then in the lake a burning sensation & they are gone!
A bad paper cut: an hour later could not find it!
Eczema: stings a bit, but went away

World’s Largest trilobite found in Manitoba
Tyndall Stone
Quarry north of Winnipeg
Discovered along CN line
Building stone for Legislature & the Parliament in Ottawa, later all public buildings in Manitoba
Paleozoic Metal deposits   -As in the Precambrian but much less plentiful
Permian Death: mother of mass extinctions
96 % of marine life gone
75 % of land life
Destruction caused by heat?
Extinct: trilobites, most sea urchins, gorgonopsid reptiles, almost all insects
Fluid inclusion evidence: too much oxygen in the air
Possible explanation
Siberian Traps: largest volcanic eruption in earth’s history. Lasted 1 million years. Not violent eruption. Lavas cover an area as large as the USA, 4 km thick, can cover entire planet 3 m deep
The release of sulfur could bring about an ice age – that will drop temp. by 5 degrees C
A Carbon 12 anomaly was due to a methane “burp” that can be responsible for another 5 degrees drop in temp.
Other evidence
Traces of complex organic molecules called fullerines or buckyballs. Have a soccer ball structure with 60 atoms of carbon
Such atoms found in Carbon stars. Could have come with an asteroid collision. Crater invisible today, covered up with lava
Life bounced up 80 m. y later & it was more diverse than ever before

The MESOZOIC: Main events     250 my to 65 my

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