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Esquema de las eras geológicas, Esquemas y mapas conceptuales de Antropología Física

Asignatura: Antropología (Física y Biológica), Profesor: Josefina Zapata Crespo, Carrera: Biología, Universidad: UMU

Tipo: Esquemas y mapas conceptuales

2013/2014

Subido el 29/09/2014

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60 April /mAy 2009, GS A ToDAy
J.D. Walker, Department of Geology, 1475 Jayhawk
Boulevard, University of Kansas, Lawrence, Kansas 66045,
USA
J.W. Geissman*, Department of Earth and Planetary Sciences,
MSC 03 2040, Northrop Hall, 1 University of New Mexico,
Albuquerque, New Mexico 87131-0001, USA
Last year marked the 25th anniversary of the first Geologi-
cal Society of A merica Geologic Time Scale (Palmer, 1983).
The effort to prepare the first Society time scale was concur-
rent with the preparation of the 27 volumes of The Geology
of North America to celebrate the Decade of North American
Geology (DNAG). In 1982, an ad hoc time scale advisory
committee was formed by the DNAG steering committee to
encourage “uniformity among DNAG authors in the citation
of numerical ages for chronostratigraphic units of the geo-
logic time scale” (Palmer, 1983). The Time Scale Advisory
Committee consisted of Z.E. Peterman (chairman), J.E. Har-
rison, R.L. Armstrong, and W.A. Berggren. Allison (Pete)
Palmer, as centennial science program coordinator for GSA,
was given the charge of compiling the committee’s efforts.
The goal of the then-unique layout of the GSA-DNAG Geo-
logic Time Scale, with each Phanerozoic era given identical
column length, along with the Precambrian, was to provide a
compact, succinctly organized yet suitably detailed (e.g., in-
cluding uncertainties in ages of chronostratigraphic boundar-
ies) compilation of our current knowledge of geologic time.
In a recent communication to the second author, Pete wrote,
I do remember that I hand-drafted it at 2 or 3 times
publication scale and pasted up the words. I also had to
figure out how to format it so that it would all fit on one
sheet (thus changing the scale for the numerical ages as
things got older). I think the small plastic cards came
later. I also think I consulted with various geochronolo-
gists to see which of several published numerical time
scales was considered the most reliable, so none of the
compilation was original—I just cribbed existing infor-
mation. Fortunately, the stage-level nomenclature was a
bit less messy than it is now…
Just think of how much has changed in 25 years (!), as re-
cent and future modifications to the GSA Geologic Time Scale
have and will continue to be done in a moment, in front of a
com puter.
Work on the current time scale started in 2007, and revision
efforts focused on three aspects. The first was to update
names and boundaries to capture changes documented in
Gradstein et al. (2004) and to reflect more recent results of
the many working groups of the International Commission
on Stratigraphy. Other relevant work was also incorporated as
needed (e.g., new publications on the Triassic time scale).
Second, we updated the boundary ages using whatever
sources were available. Last, the magnetic polarity time scale
was extensively modified, especially for the early Mesozoic,
in particular from the earliest Jurassic to the Permian-Triassic
boundary. Some aspects of the GSA Geologic Time Scale do
not conform to the recommendations of the International
Commission on Stratigraphy. The names “Tertiary” and “Pre-
cambrian” were not dropped on the new time scale. The
Quaternary, the status and boundaries of which are still be-
ing debated, was modified to reflect some of the pending
recommendations. These differences were retained to best
reflect the needs of GSA members and Divisions.
The compilers plan to keep the GSA Geologic Time Scale
more up-to-date by having yearly reviews of important
changes adopted by the International Commission on Stratig-
raphy, new publications, and information made available
through other efforts, such as the Earth-Time Initiative. Loren
Babcock (Ohio State University) will join us as a Geologic
Time Scale compiler for the next revision. In the past, the
time scale has been static for 10 years at a time, but we now
anticipate more frequent updates. The time scale will be giv-
en a posting date and be available online, in both color and
black-and-white versions.
GSA encourages the use of the time scale, boundar y ages,
and its terminology in all publications; strict enforcement,
however, is not planned. The time scale will be kept as cur-
rent as possible. Constructive comments are encouraged and
should be addressed to [email protected].
REFERENCES CITED
Gradstein, F., Ogg , J., Smith, A., et al., 2004, A Geologic Time Scale
2004: Cambridge University Press, 589 p.
Palmer, A.R., 1983, The Decade of Nor th American Geology 1983 Geo-
logic Time Scale: Geology, v. 11, p. 503–504, doi: 10.1130/0091
-7613(1983)11<503:TDONAG>2.0 .CO;2.
Commentary
2009 GSA Geologic Time Scale
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60 April/mAy 2009, GSA ToDAy

J.D. Walker, Department of Geology, 1475 Jayhawk

Boulevard, University of Kansas, Lawrence, Kansas 66045,

USA

_J.W. Geissman,_* Department of Earth and Planetary Sciences,

MSC 03 2040, Northrop Hall, 1 University of New Mexico,

Albuquerque, New Mexico 87131-0001, USA

Last year marked the 25th anniversary of the first Geologi-

cal Society of America Geologic Time Scale (Palmer, 1983).

The effort to prepare the first Society time scale was concur-

rent with the preparation of the 27 volumes of The Geology

of North America to celebrate the Decade of North American

Geology (DNAG). In 1982, an ad hoc time scale advisory

committee was formed by the DNAG steering committee to

encourage “uniformity among DNAG authors in the citation

of numerical ages for chronostratigraphic units of the geo-

logic time scale” (Palmer, 1983). The Time Scale Advisory

Committee consisted of Z.E. Peterman (chairman), J.E. Har-

rison, R.L. Armstrong, and W.A. Berggren. Allison (Pete)

Palmer, as centennial science program coordinator for GSA,

was given the charge of compiling the committee’s efforts.

The goal of the then-unique layout of the GSA-DNAG Geo-

logic Time Scale, with each Phanerozoic era given identical

column length, along with the Precambrian, was to provide a

compact, succinctly organized yet suitably detailed (e.g., in-

cluding uncertainties in ages of chronostratigraphic boundar-

ies) compilation of our current knowledge of geologic time.

In a recent communication to the second author, Pete wrote,

I do remember that I hand-drafted it at 2 or 3 times

publication scale and pasted up the words. I also had to

figure out how to format it so that it would all fit on one

sheet (thus changing the scale for the numerical ages as

things got older). I think the small plastic cards came

later. I also think I consulted with various geochronolo-

gists to see which of several published numerical time

scales was considered the most reliable, so none of the

compilation was original—I just cribbed existing infor-

mation. Fortunately, the stage-level nomenclature was a

bit less messy than it is now…

Just think of how much has changed in 25 years (!), as re-

cent and future modifications to the GSA Geologic Time Scale

have and will continue to be done in a moment, in front of a

computer.

Work on the current time scale started in 2007, and revision

efforts focused on three aspects. The first was to update

names and boundaries to capture changes documented in

Gradstein et al. (2004) and to reflect more recent results of

the many working groups of the International Commission

on Stratigraphy. Other relevant work was also incorporated as

needed (e.g., new publications on the Triassic time scale).

Second, we updated the boundary ages using whatever

sources were available. Last, the magnetic polarity time scale

was extensively modified, especially for the early Mesozoic,

in particular from the earliest Jurassic to the Permian-Triassic

boundary. Some aspects of the GSA Geologic Time Scale do

not conform to the recommendations of the International

Commission on Stratigraphy. The names “Tertiary” and “Pre-

cambrian” were not dropped on the new time scale. The

Quaternary, the status and boundaries of which are still be-

ing debated, was modified to reflect some of the pending

recommendations. These differences were retained to best

reflect the needs of GSA members and Divisions.

The compilers plan to keep the GSA Geologic Time Scale

more up-to-date by having yearly reviews of important

changes adopted by the International Commission on Stratig-

raphy, new publications, and information made available

through other efforts, such as the Earth-Time Initiative. Loren

Babcock (Ohio State University) will join us as a Geologic

Time Scale compiler for the next revision. In the past, the

time scale has been static for 10 years at a time, but we now

anticipate more frequent updates. The time scale will be giv-

en a posting date and be available online, in both color and

black-and-white versions.

GSA encourages the use of the time scale, boundary ages,

and its terminology in all publications; strict enforcement,

however, is not planned. The time scale will be kept as cur-

rent as possible. Constructive comments are encouraged and

should be addressed to [email protected].

REFERENCES CITED

Gradstein, F., Ogg, J., Smith, A., et al., 2004, A Geologic Time Scale

2004: Cambridge University Press, 589 p.

Palmer, A.R., 1983, The Decade of North American Geology 1983 Geo-

logic Time Scale: Geology, v. 11, p. 503–504, doi: 10.1130/

-7613(1983)11<503:TDONAG>2.0.CO;2.

Commentary

*[email protected]

2009 GSA Geologic Time Scale

Walker, J.D., and Geissman, J.W., compilers, 2009, Geologic Time Scale: Geological Society of America, doi: 10.1130/2009.CTS004R2C. ©2009 The Geological Society of America.

2009 GEOLOGIC TIME SCALE

PALEOZOIC

PERMIAN DEVONIAN SILURIAN ORDOVICIAN

MISSIS-

SIPPIAN

PENNSYL-

VANIAN

CARBONIFEROUS CAMBRIAN*

AGE(Ma)

EPOCH

AGE

PICKS

(Ma)

PERIOD

GZELIAN

KASIMOVIAN

MOSCOVIAN

BASHKIRIAN

SERPUKHOVIAN

VISEAN

TOURNAISIAN

FAMENNIAN

FRASNIAN

GIVETIAN

EIFELIAN

EMSIAN

PRAGHIAN

LOCKHOVIAN

PRECAMBRIAN

PROTEROZOIC ARCHEAN

AGE(Ma)

EON

ERA

BDY.

AGES

(Ma)

L

M M

E E E E

Furon-

gian

Series 3Series 2

Terre-

neuvian

L L L

M M

MESOZOIC

CRETACEOUS JURASSIC TRIASSIC

AGE(Ma)

EPOCH

AGE

PICKS

(Ma)

MAGNETIC

POLARITY

PERIOD

PERIOD

HIST.

ANOM.

CHRON.

LATE

EARLY

LATE

EARLY MIDDLE

LATE

EARLY MIDDLE

MAASTRICHTIAN

CAMPANIAN

SANTONIAN

CONIACIANTURONIAN

CENOMANIAN

ALBIAN

APTIAN

BARREMIAN

HAUTERIVIANVALANGINIAN

BERRIASIAN

TITHONIAN

KIMMERIDGIAN

OXFORDIAN

CALLOVIAN

BATHONIAN

BAJOCIAN

AALENIAN

TOARCIAN

PLIENSBACHIAN

SINEMURIANHETTANGIAN

NORIAN

RHAETIAN

CARNIANLADINIAN

ANISIAN

OLENEKIAN

INDUAN

C31C32 C

31

32 33

M0rM

M M3 M10M12M14M16M18M20M22M25M

RAPID POLARITY CHANGES

30

C30 C

34

CENOZOIC

AGE(Ma)

EPOCH

AGE

PICKS

(Ma)

MAGNETICPOLARITY

PERIOD

HIST.

ANOM.

CHRON.

QUATER-

NARY

PLEISTOCENE

MIOCENE OLIGOCENE EOCENE PALEOCENE

PLIOCENE

PIACENZIAN

L

E

L

M E

L

M E M E

L

ZANCLEANMESSINIAN

TORTONIAN

SERRAVALLIAN

LANGHIAN

BURDIGALIAN

AQUITANIAN

CHATTIAN

RUPELIAN

PRIABONIAN

BARTONIAN

LUTETIAN

YPRESIAN

DANIAN

THANETIANSELANDIAN

CALABRIAN

HOLOCENE

TERTIARY

NEOGENE PALEOGENE

1

C1C C2A

C C3A

C C4A

C C6AC6BC6C

C7C8C C

C11C12 C C15C

C C18C19 C

C C

C23 C C

C C7A C27C28C

C C5A C5BC5CC5DC5E

2

2A

3

3A

4

4A

5 5A 5B5C

6

6A6B

7 8

9

101112 13151617 18 19 20 21 22 2324 25 26 2829

27 5D5E 6C7A 30

C

GELASIAN

CHANGHSINGIAN

WORDIANROADIAN

WUCHIAPINGIAN

CAPITANIAN

KUNGURIAN

ASSELIAN

ARTINSKIANSAKMARIAN

PRIDOLIAN

LUDFORDIAN

GORSTIANHOMERIAN

RHUDDANIAN

TELYCHIANAERONIAN

SHEINWOODIAN

HIMANTIAN

SANDBIAN

KATIAN

DARRIWILIAN

DAPINGIAN

STAGE 10

STAGE 9PAIBIAN

GUZHANGIAN

DRUMIAN

STAGE 5STAGE 4STAGE 3STAGE 2

FORTUNIAN

FLOIAN

TREMADOCIAN

EDIACARAN

CRYOGENIAN

TONIAN

STENIAN

ECTASIAN

CALYMMIAN

STATHERIAN

OROSIRIAN

RHYACIAN

SIDERIAN

NEOPRO-

TEROZOIC

MESOPRO-

TEROZOIC

PALEOPRO-

TEROZOIC

NEOARCHEAN

MESO-

ARCHEAN

PALEO-

ARCHEAN

EOARCHEAN

HADEAN

*International ages have not been fully established. These are current names as reported by the International Commission on Stratigraphy.Sources for nomenclature and ages are primarily from Gradstein, F., Ogg, J., Smith, A., et al., 2004, A Geologic Time Scale 2004: Cambridge University Press, 589 p. Modifications tothe Triassic after: Furin, S., Preto, N., Rigo, M., Roghi, G., Gianolla, P., Crowley, J.L., and Bowring, S.A., 2006, High-precision U-Pb zircon age from the Triassic of Italy: Implications forthe Triassic time scale and the Carnian origin of calcareous nannoplankton and dinosaurs: Geology, v. 34, p. 1009–1012, doi: 10.1130/G22967A.1; and Kent, D.V., and Olsen, P.E.,2008, Early Jurassic magnetostratigraphy and paleolatitudes from the Hartford continental rift basin (eastern North America): Testing for polarity bias and abrupt polar wander inassociation with the central Atlantic magmatic province: Journal of Geophysical Research, v. 113, B06105, doi: 10.1029/2007JB005407.