%
% --------------------------------------------
% Evolutionary/Geological Timeline Version 1.1
% --------------------------------------------
%
% This is a copy of an evolutionary/geological timeline that I have
% been making.
%
% This is a plain TEX file and does not require any TEX macro
% files. One should only need to edit out the usenet/email header
% information and then the file should be able to be passed
% through TEX. You do not need to edit out this information
% and I would appreciate it if you would not so that if
% later you give this file to someone else they will be
% able to send me their ideas. The TEX page size variables are
% currently set for American sized paper and may have to be changed 
% for other sizes of paper.
%
% I would be grateful for factual, spelling, and grammar
% corrections. I would be grateful for suggestions as to how to
% better word specific entries so as to make them clearer. I am
% also keen to add interesting events to the timeline and would
% appreciate suggestions.
%
% Please send any suggestions to me via email.
%
% An XMOSAIC page has been created for my timelines and scales of measurement
% list. The URL is the following:
%
%     http://www.astro.psu.edu/users/niel/scales/scales.html
%
% If you are not able to obtain one of my lists via the WWW or usenet, please
% send me an email request and I will email you the list you want. Please
% specify desired format (ASCII or TEX).
%
% Niel Brandt
% niel@astro.psu.edu
%
% This document is copyright Niel Brandt 1994. You are allowed to copy,
% distribute, and edit this document at will without any obligation as long
% as you do not remove the above header. Reproduction and distribution for
% personal profit is not permitted.

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\noindent {\bf EVOLUTIONARY/GEOLOGICAL TIMELINE}

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\halign{
\hbox{#}&\quad\hbox{#}\cr
Time (Myr ago) & Event\cr
               &      \cr
4600           & Formation of the approximately homogeneous solid Earth by planetesimal accretion\cr
4300           & Melting of the Earth due to radioactive and gravitational heating which leads to its differentiated interior structure as\cr
               & well as outgassing of molecules such as water, methane, ammonia, hydrogen, nitrogen, and carbon dioxide\cr
4300           & Atmospheric water is photodissociated by ultraviolet light to give oxygen atoms which are incorporated into an ozone\cr
               & layer and hydrogen molecules which escape into space\cr
4300           & First minerals (zircons) crystalize on the molten Earth\cr 
4000           & Bombardment of the Earth by planetesimals stops\cr
3800           & The Earth's crust solidifies---formation of the oldest rocks found on Earth\cr
3800           & Condensation of atmospheric water into oceans\cr
3500--2800     & Prokaryotic cell organisms develop\cr
3500--2800     & Beginning of photosynthesis by blue-green algae which releases oxygen molecules into the atmosphere and steadily works to\cr
               & strengthen the ozone layer and change the Earth's chemically reducing atmosphere into a chemically oxidizing one\cr
2400           & Rise in the concentration of oxygen molecules stops the deposition of uraninites (since they are soluble when combined\cr
               & with oxygen) and starts the deposition of banded iron formations\cr
2000           & The Oklo natural fission reactors in Gabon go into operation and run for about 1 Myr\cr
2000           & The Magellanic Clouds tidally interact with the Milky Way thereby starting the Magellanic Stream (MNRAS 198, 710)\cr
1600           & The last reserves of reduced iron are used up by the increasing atmospheric oxygen---last banded iron formations\cr
1500           & Eukaryotic cell organisms develop\cr
1500--600      & Rise of multicellular organisms\cr
1100           & Formation of the supercontinent Rodinia\cr
700            & Break-up of the supercontinent Rodinia\cr
580--545       & Fossils of Ediacaran organisms are made\cr
550            & Formation of Gondwana \cr
545            & Cambrian explosion of hard-bodied organisms\cr
528--526       & Fossilization of the Chengjiang site\cr
517--515       & Fossilization of the Burgess Shale\cr
500--450       & Rise of the fish---first vertebrates\cr
440            & Ordovician mass extinction\cr
430            & Waxy coated algae begin to live on land\cr
420            & Millipedes have evolved---first land animals\cr
375            & The Appalachian mountains are formed via a plate tectonic collision between North America, Africa, and Europe\cr
375            & Appearance of primitive sharks\cr
365            & Devonian mass extinction\cr
350--300       & Rise of the amphibians\cr
350            & Primitive insects have evolved\cr
350            & Primitive ferns evolve---first plants with roots\cr
300--200       & Rise of the reptiles\cr
300            & Winged insects have evolved\cr
280            & Beetles and weevils have evolved\cr
250            & Permian period mass extinction\cr
230            & Roaches and termites have evolved\cr
225            & Modern ferns have evolved\cr
225            & Bees have evolved\cr
210            & Triassic mass extinction\cr
200            & Pangaea starts to break apart\cr
200            & Primitive crocodiles have evolved\cr
200            & Appearance of mammals\cr
145            & Archaeopteryx walks the Earth\cr
136            & Primitive kangaroos have evolved\cr
100            & Primitive cranes have evolved\cr
90             & Modern sharks have evolved\cr
65             & The Chicxulub impact occurs\cr
65             & K-T Boundary---extinction of the dinosaurs and beginning of the reign of mammals\cr
60             & Rats, mice, and squirrels have evolved\cr
60             & Herons and storks have evolved\cr
55             & Rabbits and hares have evolved\cr
50             & Primitive monkeys have evolved\cr
28             & Koalas have evolved\cr
20             & Parrots and pigeons have evolved\cr
20--12         & The chimpanzee and hominid lines evolve\cr
10--4          & Ramapithecus exist\cr
4              & Development of hominid bipedalism\cr
4--1           & Australopithecus exist\cr
3.5            & The Australopithecus Lucy walks the Earth\cr
2              & Widespread use of stone tools\cr
2--0.01        & Most recent ice age\cr
1.6--0.2       & Homo erectus exist\cr
1--0.5         & Homo erectus tames fire\cr
0.3            & Geminga supernova explosion at a distance of roughly 60 pc---roughly as bright as the Moon\cr
0.2--0.03      & Homo sapiens neanderthalensis exist\cr
0.05--0        & Homo sapiens sapiens exist\cr
0.04--0.012    & Homo sapiens sapiens enter Australia from southeastern Asia and North America from northeastern Asia\cr
0.025--0.01    & Most recent glaciation---an ice sheet covers much of the northern United States\cr
0.02           & Homo sapiens sapiens paint the Altamira cave and the Chauvet cave\cr
0.017          & Homo sapiens sapiens paint the Lascaux cave\cr
0.012          & Homo sapiens sapiens have domesticated dogs in Kirkuk, Iraq\cr
0.01           & First permanent homo sapiens sapiens settlements\cr
0.01           & Homo sapiens sapiens learn to use fire to cast copper and harden pottery\cr
0.006          & Writing is developed in Sumeria\cr
0.0046         & Oldest known Bristlecone Pine tree starts to grow\cr
}

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\halign{
\hbox{#}&\quad\hbox{#}\cr
Time (Myr ago) & Event\cr
               &      \cr
5000--1500     & Archeozoic (Archean) era\cr
%
1500--545      & Proterozoic era\cr
%
               & Paleozoic era ``Ancient life''\cr

545--505       & \hskip 0.2 in Cambrian period\cr
505--438       & \hskip 0.2 in Ordovician period\cr
438--410       & \hskip 0.2 in Silurian period\cr
410--355       & \hskip 0.2 in Devonian period\cr
355--290       & \hskip 0.2 in Carboniferous (Mississippian/Pennsylvanian) period\cr
290--250       & \hskip 0.2 in Permian period\cr
%
               & Mesozoic era ``Middle Life''\cr
%
250--205       & \hskip 0.2 in Triassic period\cr
205--135       & \hskip 0.2 in Jurassic period\cr
135--65        & \hskip 0.2 in Cretaceous period\cr
%
               & Cenozoic era ``Recent Life''\cr
%
               & \hskip 0.2 in Tertiary (Paleogene/Neocene) period\cr
%
65--55         & \hskip 0.4 in Paleocene epoch\cr
55--38         & \hskip 0.4 in Eocene epoch\cr
38--26         & \hskip 0.4 in Oligocene epoch\cr
26--6          & \hskip 0.4 in Miocene epoch\cr
6--1.8         & \hskip 0.4 in Pliocene epoch\cr
%
               & \hskip 0.2 in Quaternary period\cr
%
1.8--0.01      & \hskip 0.4 in Pleistocene epoch\cr
%
0.50--0.25     & \hskip 0.6 in Lower Paleolithic\cr
0.25--0.06     & \hskip 0.6 in Middle Paleolithic\cr
0.06--0.01     & \hskip 0.6 in Upper Paleolithic\cr
%
0.01--0        & \hskip 0.4 in Holocene epoch\cr
}

\end
