GEOLOGIC HISTORY OF NEW YORK STATE F
H
G
J
I
K
Valcouroceras Tetragraptus Eucalyptocrinus Centroceras Cryptolithus Ctenocrinus Dicellograptus Manticoceras Phacops Elliptocephala Hexameroceras
Era
Period
Epoch
Life on Earth
Millions of years ago
MESOZOIC CRETACEOUS
V
Important Geologic Events in New York
EARLY MISSISSIPPIAN
DEVONIAN
323
LATE EARLY LATE
Oldest microfossils
Earliest reptiles Extensive coal-forming forests
MIDDLE
418 LATE
SILURIAN EARLY
C
F
Earliest insects Earliest land plants and animals Peak development of eurypterids
E
LATE
ORDOVICIAN
Invertebrates dominant – mollusks become abundant Diverse coral and echinoderms
MIDDLE
490
Estimated time of origin of Earth and solar system
LATE
CAMBRIAN
Graptolites abundant Earliest fish Algal reefs Burgess shale fauna Earliest chordates, diverse trilobites Earliest trilobites Earliest marine animals with shells
EARLY
G I
443
Oldest known rocks
Passive Margin Rifting
Appalachian (Alleghanian) Orogeny caused by collision of North America and Africa along transform margin, forming Pangea
B
D
H K
N
M
Q
P
Earth’s first coral reef
X
Z
V Y
U
T
W
J
A
1300
Earth Science Reference Tables — 2001 Edition (Revised November 2006)
Rifting
Passive Margin
Ediacaran fauna
Soft-bodied organisms
59 million years ago
CRETACEOUS
119 million years ago
TRIASSIC
232 million years ago
Catskill Delta forms Erosion of Acadian Mountains
R
544 580
TERTIARY
Earth’s first forest
362
EARLY
Geochemical evidence for oldest biological fixing of carbon
Abundant sharks and amphibians Large and numerous scale trees and seed ferns Earliest amphibians, ammonoids, sharks Extinction of armored fish, other fish abundant
Inferred Position of Earth’s Landmasses
Extensive erosion
Transform Collision
LATE PENNSYLVANIAN
Z
Intrusion of Palisades sill Pangea begins to break up
Continental Collision
290
Y
Initial opening of Atlantic Ocean North America and Africa separate
BRACHIOPODS
EARLY
GASTROPODS
PERMIAN
L
CORALS
Transition to atmosphere containing oxygen
Modern coral groups appear Earliest dinosaurs and mammals with abundant cycads and conifers Extinction of many kinds of marine animals, including trilobites First mammal-like reptiles
X
Development of passive continental margin
VASCULAR PLANTS
PALEOZOIC
LATE MIDDLE EARLY 251 LATE
W
Sands and shales underlying Long Island and Staten Island deposited on margin of Atlantic Ocean
PLACODERM FISH
TRIASSIC
206
MIDDLE
8
U
Advance and retreat of last continental ice Uplift of Adirondack region
Earliest birds Abundant dinosaurs and ammonoids
MIDDLE
EARLY 4600
S
Subduction
E A R L Y
T
142
EURYPTERIDS
M I D D L E
Tectonic Events Affecting Northeast North America
LATE
JURASSIC
E A R L Y
Earliest flowering plants Decline of brachiopods Diverse bony fishes
EARLY
First appearance of sexually reproducing organisms
Beluga Whale
A
O
S
R
Q
Bothriolepis Naples Tree Lichenaria Pleurodictyum Mucrospirifer Platyceras Cooksonia Aneurophyton Condor Eospirifer Maclurites Cystiphyllum
Time Distribution of Fossils Rock Record (Including Important Fossils of New York) in Lettered circles indicate the approximate time of existence of a specific NYS index fossil (e.g. Fossil lived at the end of the Early Cambrian).
CRINOIDS
PROTEROZOIC
PALEOGENE
P
O
Stylonurus Eurypterus Mastodont
GRAPTOLITES
4000
NEOGENE
Coelophysis
HOLOCENE 0 0.01 PLEISTOCENE 1.6 Humans, mastodonts, mammoths PLIOCENE 5.3 Large carnivores Abundant grazing mammals MIOCENE 24 Earliest grasses OLIGOCENE Large running mammals EOCENE 33.7 Many modern groups of mammals 54.8 PALEOCENE 65 Extinction of dinosaurs and ammonoids Earliest placental mammals LATE Climax of dinosaurs and ammonoids
EARLY
L A T E
ARCHEAN
P R E C A M B R I A N
3000
M I D D L E
Oldest multicellular life
TERTIARY
L A T E
1000
2000
QUATERNARY
CENOZOIC
CARBONIFEROUS
500
PHANEROZOIC
Millions of years ago 0
N
M
AMMONOIDS
Eon
L
BIRDS
E
MAMMALS
D
NAUTILOIDS
C
TRILOBITES
B
A
DINOSAURS
(Fossils not drawn to scale)
Acadian Orogeny caused by collision of North America and Avalon and closing of remaining part of Iapetus Ocean
DEVONIAN/MISSISSIPPIAN 362 million
years ago
Salt and gypsum deposited in evaporite basins
Erosion of Taconic Mountains; Queenston Delta forms Taconian Orogeny caused by closing of western part of Iapetus Ocean and collision between North America and volcanic island arc
ORDOVICIAN
458 million years ago
Iapetus passive margin forms Rifting and initial opening of Iapetus Ocean Erosion of Grenville Mountains Grenville Orogeny: Ancestral Adirondack Mtns. and Hudson Highlands formed
Stromatolites 96-001TN (rev) 11/2006
Earth Science Reference Tables — 2001 Edition (Revised November 2006)
9