GENBIO Flashcards
One billion years
Gigaannum
are the longest portions of geologic time
Eons
These divisions are called geochronological units
EONS ERAS PERIODS
divides up the history of the earth based on life-forms that have existed during specific times since the creation of the planet.
The geologic time scale
Subdivision of eons
HEDEAN ARCHEAN PROTEROZOIC PHANEROZOIC
Subdivision of eons ( PRECAMBRIAN SUPEREON )
HEDEAN ARCHEAN PROTEROZOIC
Subdivision of eons ( CAMBRIAN PERIOD )
Phanerozoic
was the “Age of Early Life.” -continents formed and our modern atmosphere developed, while early life evolved and flourished 4.5 billion to 540 million years ago when earth was an ocean of magma.
Precambrian
Events in the hadean Eon
Earth coalesced from a cloud of dust into a planet.
The Big Bang created all matter in the universe.
A magnetic field forms
Earth meet moon
-named after the Greek god and ruler of the underworld Hades, is the oldest eon and dates from 4.5–4.0 billion years ago. This time represents Earth’s earliest history, during which the planet was characterized by a partially molten surface, volcanism, and asteroid impacts
Hadean Eon
an older sources sometimes called the Archaeozoic, is the second of the four geologic eons of Earth’s history, preceded by the Hadean Eon and followed by the Proterozoic.
Archean (beginning or primitive)
that were active in the Archean eon (before approximately 2500 million years ago) in Precambrian time.
Volcanoes
also called also called Cyanobacteriota or Cyanophyta,are a phylum of autotrophic gram-negative bacteria that can obtain biological energy via photosynthesis.
Cyanobacteria
is a domain of single-celled organisms. These microorganisms lack cell nuclei and are therefore prokaryotic.
Archea
is the most recent division of the Precambrian. It is also the longest geologic eon, beginning 2.5 billion years ago and ending 541 million years ago.
Proterozoic
is the current and the latest of the four geologic eons in the Earth’s geologic time scale, covering the time period from 538.8 million years ago to the present.
Phanerozoic
three eras of the phanerozoic
Paleozoic, Mesozoic and Cenozoic eras.
means ‘ancient life.’ The oldest animals on Earth appeared just before the start of this era in the Ediacaran Period, but scientists had not yet discovered them when the geologic timescale was made.
Paleozoic (541-252 million years ago)
marks an important point in the history of life on Earth; it is the time when most of the major groups of animals first appear in the fossil record. This event is sometimes called the “Cambrian Explosion,” because of the relatively short time over which this diversity of forms appears. It was once thought that Cambrian rocks contained the first and oldest fossil animals, but these are now found in the earlier
Cambrian Period
which lived in shells resembling those of clams or cockles, and animals with jointed, external skeletons known as arthropods the ancestors of insects, spiders, and crustaceans.
Brachiopods
is a geologic period and system, the second of six periods of the Paleozoic Era spans 41.6 million years from the end of the Cambrian Period 485.4 Ma to the start of the Silurian Period 443.8 Ma
Ordovician Period
the most remarkable biological event was the evolution and diversification of fish
Silurian Period
was a time of major evolutionary innovation in the marine realm ‘Age of Fishes‘ 419.2 million years ago
Devonian
creatures in Silurian period
trilobites graptolites conodonts corals, stromatoporoids, mollusks.