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Faunal Succession

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Submitted By akshaybobby1
Words 2536
Pages 11
Extinction Happens

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Thomas Henry De La Beche (1796‐1855), sketch of life in ancient Dorset, 1830

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A few unfortunate but widely-recognized facts about the history of science (and society and religion and...)
• rich, old, straight* white guys are (mostly) everywhere
• the participation of women was (in many cases) actively discouraged or discounted
• the participation of non-white guys and all poor guys was (in most cases) actively discouraged and/or discounted
• some aspects of scientific discovery have been highly exploitative, of both nature and of local cultures
• scientific ideas have been hijacked and inappropriately used to justify many things, both good and bad
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* or so they claimed…

Ph.D.s

full-time faculty 7

8

State Revenue Contribution ($Billion)

1.2

+3%

+14%

tuition + scale

0.9

0.6

state contribution negative scale

0.3

0

2015

Sources: http://nicic.gov/statestats/?st=WI 2016

http://doc.wi.gov/Home https://www.wisconsin.edu/about-the-uw-system/

http://www.doa.state.wi.us/Documents/DEBF/Budget/Biennial%20Budget/2015-17%20Executive%20Budget/2015-17_Executive_Budget.pdf

There is no extinction, There is no evolution, it’s all EVOLUTION! it’s all EXTINCTION!

“Goal” is towards God, man created in his image
(Lamarck)

Catastrophic changes in Earth cause extinction of created forms.
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(Cuvier)

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Homologous structures

• anatomical parts which share similarities that are not functionally necessary
• pre-Darwinian explanations involved the “plan of god”
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Homologous structures

• anatomical parts which share similarities that are not functionally necessary
• pre-Darwinian explanations involved the “plan of god”
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Homologous structures

human

chimpanzee

gibbon

• anatomical parts which share similarities that are not functionally necessary
• pre-Darwinian explanations involved the “plan of god”
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Homologous structures

hair is a homologous trait shared by all mammals
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Analogous structures

• anatomical parts with functionally similar forms that are constructed in different ways
• NB: can be hierarchical (e.g., bird and bat wing homologous as limbs, but not wings)

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Vestigial structures

snake legs!

• features of organisms that have no apparent purpose or function, often resembling parts that are in use by other organisms
• often greatly reduced in size, modified from the original form
• perplexing to pre-Darwinian scholars because seemed to imply waste by creator

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Vestigial structures

ajolote

• features of organisms that have no apparent purpose or function, often resembling parts that are in use by other organisms
• often greatly reduced in size, modified from the original form
• perplexing to pre-Darwinian scholars because seemed to imply waste by creator

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Vestigial structures human tail parts

• features of organisms that have no apparent purpose or function, often resembling parts that are in use by other organisms
• often greatly reduced in size, modified from the original form
• perplexing to pre-Darwinian scholars because seemed to imply waste by creator

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Embryology: the “evolution” of an individual

• individuals undergo profound change in morphology during development
• development was original meanings of the word “evolution”

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Embryology: the “evolution” of an individual

• early developmental stages of organisms that are very different as adults are very similar
• traits appear in embryos that are not part of adult
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Embryology: the “evolution” of an individual
24 day dolphin embryo

48 day dolphin embryo

hind limb bud

• early developmental stages of organisms that are very different as adults are very similar
• traits appear in embryos that are not part of adult
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Embryology: the “evolution” of an individual
24 day dolphin embryo

48 day dolphin embryo

hind limb bud

48 day human embryo

hind limb bud

• early developmental stages of organisms that are very different as adults are very similar
• traits appear in embryos that are not part of adult
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Geoffroy St. Hilaire
(1772-1844)

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Geoffroy St. Hilaire
(1772-1844)

“There is nothing fixed in nature”

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What about the origin of species and the “driver” of evolution?

‘The inference, we think, is inevitable, that the watch must have had a maker; that there must have existed, at some time, and at some place or other, an artificer or artificers who formed it for the purpose which we find it actually to answer; who comprehended its construction, and designed its use.’
William Paley (1743-1805)
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The Archetype

“For the Divine mind which planned the Archetype also foreknew all its modifications...we learn from the past history of our globe, that Nature has advanced with slow and stately steps, guided by the archetypal light amidst the wreck of worlds, from the first embodiment of the vertebrate idea, under its old ichtyhic vestment, until it became arranged in the glorious garb of the human form”
Richard Owen, 1849
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Some take-home points


Steno’s proof that fossils were organic remains of once living things raised the possibility of extinction, which posed many conceptual challenges to our view of life and its history



Cuvier used comparative anatomy to study large terrestrial mammals; fossils of large extinct animals proved extinction beyond all reasonable doubt



the fact of extinction required explanation; Cuvier argued there was NO evolution, all extinction, Lamarck argued there was NO extinction, all evolution



homologous, analogous, and vestigial structures, embryo development and developmental anomalies all pointed to the mutability of species and change in species over time
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Homologous characters _________.
A) include hair and forelimbs in mammals
B) exhibit similarities during embryo development
C) are useful for classifying organisms
D) all of the above
E) none of the above
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Faunal succession and geologic time

Sedgwick: defined “Cambrian” and “Devonian” periods

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INTERNATIONAL CHRONOSTRATIGRAPHIC CHART

Thanetian
Selandian
Danian
Maastrichtian

11.63
13.82
15.97
20.44

Mesozoic
Cretaceous

Turonian
Cenomanian

33.9
37.8
41.2
47.8
56.0
59.2
61.6

89.8 ±0.3
93.9
100.5
~ 113.0
~ 125.0

Barremian
Valanginian

31

Berriasian

~ 129.4
~ 132.9

Ladinian

Lopingian

Anisian
Olenekian
Induan
Changhsingian
Wuchiapingian
Capitanian

72.1 ±0.2

Guadalupian

Wordian
Roadian
Kungurian

Cisuralian

Artinskian
Sakmarian

~ 139.8
~ 145.0

Middle

Asselian
Gzhelian
Kasimovian
Moscovian

Lower

Bashkirian

Upper

Upper

Serpukhovian

Middle

182.7 ±0.7

Middle

Lower

265.1 ±0.4
268.8 ±0.5
272.3 ±0.5

Wenlock

407.6 ±2.6
410.8 ±2.8
419.2 ±3.2

Ludfordian
Gorstian
Homerian
Sheinwoodian
Telychian
Aeronian
Rhuddanian
Hirnantian

Middle

423.0 ±2.3
425.6 ±0.9
427.4 ±0.5
430.5 ±0.7
433.4 ±0.8
438.5 ±1.1
440.8 ±1.2
443.8 ±1.5
445.2 ±1.4

Darriwilian

Sandbian

Dapingian
Lower

Floian

453.0 ±0.7
458.4 ±0.9

Stage 10

Furongian

298.9 ±0.15

Series 3

Jiangshanian
Paibian
Guzhangian
Drumian
Stage 5
Stage 4

Series 2

477.7 ±1.4
485.4 ±1.9
~ 489.5
~ 494
~ 497
~ 500.5
~ 504.5
~ 509
~ 514

Stage 3

330.9 ±0.2

Mesoproterozoic

GSSP
GSSA

Ectasian
Calymmian
Statherian

Terreneuvian

Tournaisian

1000
1200
1400
1600
1800

Paleoproterozoic

2050

Rhyacian
Siderian

Neoarchean

2300
2500
2800

Mesoarchean
3200

Paleoarchean
3600

Eoarchean

Hadean
~ 4600
Units of all ranks are in the process of being defined by Global
Boundary Stratotype Section and Points (GSSP) for their lower boundaries, including those of the Archean and Proterozoic, long defined by Global Standard Stratigraphic Ages (GSSA). Charts and detailed information on ratified GSSPs are available at the website http://www.stratigraphy.org. The URL to this chart is found below.
Numerical ages are subject to revision and do not define units in the Phanerozoic and the Ediacaran; only GSSPs do. For boundaries in the Phanerozoic without ratified GSSPs or without constrained numerical ages, an approximate numerical age (~) is provided.
Numerical ages for all systems except Lower Pleistocene,
Permian,Triassic, Cretaceous and Precambrian are taken from
‘A Geologic Time Scale 2012’ by Gradstein et al. (2012); those for the Lower Pleistocene, Permian, Triassic and Cretaceous were provided by the relevant ICS subcommissions.
Coloring follows the Commission for the
Geological Map of the World (http://www.ccgm.org)

~ 529

Chart drafted by K.M. Cohen, S.C. Finney, P.L. Gibbard
(c) International Commission on Stratigraphy, January 2015

Fortunian

358.9 ±0.4

~ 720

Orosirian

~ 521

Stage 2
346.7 ±0.4

Stenian

~ 635

4000
467.3 ±1.1
470.0 ±1.4

Tremadocian

295.0 ±0.18

323.2 ±0.4

393.3 ±1.2

Katian

290.1 ±0.26

315.2 ±0.2

Pragian

Upper

283.5 ±0.6

303.7 ±0.1
307.0 ±0.1

Eifelian

Pridoli
Ludlow

Llandovery

259.8 ±0.4

Tonian

387.7 ±0.8

Lochkovian

~ 208.5

247.2
251.2
252.17 ±0.06
254.14 ±0.07

Givetian

numerical age (Ma)
~ 541.0 ±1.0

Cryogenian

382.7 ±1.6

Emsian

199.3 ±0.3
201.3 ±0.2

~ 242

Neoproterozoic

Frasnian

190.8 ±1.0

~ 237

System / Period

Ediacaran

372.2 ±1.6

Visean

Lower

GSSP

GSSP

Eo no the
Er
ath m / E on em
Sy
ste / Era m /P erio d

174.1 ±1.0

~ 227

Carnian

Lower

83.6 ±0.2
86.3 ±0.5

163.5 ±1.0
166.1 ±1.2
168.3 ±1.3
170.3 ±1.4

Norian

Upper

Middle

66.0

Albian

Hauterivian

Rhaetian

28.1

Aptian
Lower

Hettangian

Paleozoic

Upper

Sinemurian

23.03

Campanian
Santonian
Coniacian

Toarcian
Pliensbachian

Lower

Eonothem
/ Eon Erathem / Era

Precambrian
Proterozoic

7.246

Upper

157.3 ±1.0

Devonian

5.333

Middle

numerical age (Ma)
358.9 ± 0.4

Silurian

Jurassic

3.600

Ypresian
Paleocene

Eo no the
Er
ath m / E on em
Sy
ste / Era m /P erio d

2.58

Stage / Age

Famennian

Archean

Lutetian

1.80

Series / Epoch

~ 145.0

Cambrian

Bartonian
Eocene

Oxfordian
Callovian
Bathonian
Bajocian
Aalenian

numerical age (Ma)

152.1 ±0.9

Phanerozoic
Paleozoic
Ordovician

Priabonian

0.781

Triassic

Rupelian

Kimmeridgian

Upper

0.126

Permian

Chattian

Stage / Age

Tithonian

Carboniferous

Paleogene

Serravallian
Langhian
Burdigalian
Aquitanian

Oligocene

Series / Epoch

0.0117

Mississippian Pennsylvanian

Cenozoic
Neogene

Tortonian
Miocene

numerical age (Ma)

v 2015/01

International Commission on Stratigraphy

present

Upper
Middle
Calabrian
Gelasian
Piacenzian
Zanclean
Messinian

Mesozoic

Pleistocene

Pliocene

Phanerozoic

Stage / Age

Holocene

Phanerozoic

Quaternary

Series / Epoch

GSSP

Eo no the
Er
ath m / E on em
Sy
ste / Era m /P erio d

www.stratigraphy.org

541.0 ±1.0

To cite: Cohen, K.M., Finney, S.C., Gibbard, P.L. & Fan, J.-X. (2013; updated)
The ICS International Chronostratigraphic Chart. Episodes 36: 199-204.
URL: http://www.stratigraphy.org/ICSchart/ChronostratChart2015-01.pdf

To know:
• Order of Eons (3)
• Order of Phanerozoic Eras (3)
• Order of Phanerozoic Periods (12)
• 4 dates: base of Phanerozoic (541 Ma), end of Paleozoic
(252 Ma), end of Mesozoic (66 Ma), age of earth (~4.6 Ga)

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Two methods of dating...

5

9 Myr
4

• Relative - age of events/rocks expressed in rank order relative to one another (i.e., first a then b) you know this now!

3

• Numerical - age of events/rocks expressed in units of time (i.e. a happened x years ago, b happened y years ago) - later in course
2

12 Myr
1
33

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What about fossils?

William Smith
(1769-1839)

• poor working man, little formal education, no family connections.
Spent time in debtors’ prison!
• on-site ‘foreman’ for canal digging projects during early stages of industrial revolution in England
• spent countless hours studying rocks and fossils for practical economic reasons (needed to predict how long it would take to complete a canal project)
36

William Smith’s field work

• focused on collection and documentation of fossils and their position in strata
• strictly empirical observation of fossils and the sedimentary rocks in which the occur

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38

39

40

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First large-scale geologic map
(1815)

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How did the map
“change the world”?
• demonstrated large-scale ORDER of strata in the geologic record
• used geologic field DATA to PREDICT the distribution of rock types, both on the surface and in the subsurface • established a whole new approach to studying and characterizing the geologic record

43

How did Smith make the map?

If sedimentary rocks were always perfectly flat and everywhere the same and never repeated, it would be relatively easy....

44

45

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How did Smith make the map?
• extensive observational field work; Smith looked at and documented properties and distribution of rocks across large areas of (present day) UK
• measured physical ORIENTATION of strata and their
THICKNESS
• systematically collected FOSSILS and noted their
ORDER of occurrence in strata

“Fossils have been long studied as great curiosities, collected with great pains, treasured with great care and at a great expense, and shown and admired with as much pleasure as a child’s hobby-horse is shown and admired because it is pretty; and this has been done by thousands who have never paid the least regard to that wonderful order and regularity with which nature has disposed of these singular productions, and assigned to each class its peculiar stratum.”
William Smith, notes, 5 January 1796
47

“Strata identified by organized fossils”
William Smith 1816

• rock type alone has little or no relative age utility (a sandstone is a sandstone, no matter its age)
• the same fossils species can occur in many different rock types
• TEMPORAL ORDER of fossils is what is consistent and similarly repeated everywhere, no matter what rock looks like
48

Principle of Faunal Succession
(1816)
• ideas and work initially ripped off by connected elites who plagiarized and undersold his work
• Smith only formally recognized in 1831 by
Geological Society with the first Wollaston Medal
49

Cuvier and Brongniart (1811-1822)

• french paleontologists/geologists that independently and nearly simultaneously recognized similar principles
• identified change in fossils over time & faunal succession
(Cuvier explained this by “revolutions” that caused extinction of created forms)
• made geologic maps that matched nearly perfectly across the channel!
50

Smith

Alexandre Brongniart

Cuvier
Brongniart

51

So what was the big deal??

$$$$$$

• industrial revolution powered by geological resources (we still are...)
• Smith’s work provided the PREDICTIVE framework for resource acquisition and infrastructure planning
52

Georges Cuvier

strata = time

Faunal succession = relative aging tool

what is age of rock containing this fossil assemblage?
53

Biostratigraphy
(based on Smith’s principle of faunal succession)

• DEFINITION: correlation of strata and determination of relative ages based on INDEX FOSSILS
• Biostratigraphic framework is constantly being updated and revised as new data are assembled.
This is a strength as a working hypothesis!
54

55

Faunal succession is a FACT!!
EVOLUTION is an amazingly good explanation, but faunal succession does NOT assume evolution!

The hypothesis of biostratigraphy really works!
Energy industry uses it extensively
$$$$$$

56

A short review of some highlights...
Cuvier proves extinction Galileo shows that
Earth is not center of universe
Steno proves that some
“fossil objects” were once living things
1609

1669

1735

Hutton uses uniformitarianism to prove that Earth is
Lamarck evolution very old
1788 1796 1816

Linnaeus establishes classification scheme that uses continuity of form in nature

Steno proves that the rock record preserves a history

1859
Origin of
Species

Linnaeus abandons fixed species concept

Smith documents faunal succession in fossil record
57

Steno’s laws, Hutton’s geology, Smith’s biostratigraphy were original basis for subdivision of geologic time
“visible life”
“ancient life”

Cambrian

Phanerozoic
Paleo zoic
Ordovician
Silurian

named after places and tribes in Great Britain
58

Eonothem

Devonian

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