After midterm Flashcards

(124 cards)

1
Q

French developments

A

George Cuvier and Alexander brongniart developed ideas of faunal succession

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2
Q

Who was the first person to go beyond faunal succession and develop a modern concept of biostrigraphy?

A

Alcide dorbigny

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3
Q

What did dorbigny study?

A

Studied the Jurassic fossils and strata in southern France

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4
Q

Albert Oppel

A

Completed the modernization of bio stratigraphy

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5
Q

What makes a good biostratigraphic indicator fossil?

A
Distinctive
Abundant 
Widespread geological distribution 
Not facies specific 
Rapid evolution 
Short temporal range
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6
Q

Reasons why local first and last appearance data isn’t globl

A

Biogeopgraphic: all species are geographic in origin, may immigrate to other places, suffer local extinction
Preservation
Facies specificity
Uncomformites: no rocks of that age in local sections

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7
Q

Classification of grace fossils

A

Ethnologic or taxonomic

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8
Q

Ethologic

A

Trace fossils are primarily evidence of animal behaviour

Seilacher established a small number of ethologic categories

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9
Q

Categories of ethologics

A
Resting trace: cubichnia
Locomotion trace: Repichnia 
Grazing trace: pascichnia
Feeding traces: Fodinichnia 
Dwelling traces: domichnia 
Traps/farming traces: agrichnia 
Escape traces: Fugichnia
Equilibrium traces: equilibrichnia 
Predation traces: praedichnia 
Nesting traces: calichnia 
Fixation/ anchoring traces: fixichnia 
Death traces: mortichnia
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10
Q

Bio stratigraphy

A

The art and science of telling time from rocks

Based on faunal succession which was first discovered by William smith

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11
Q

Ichnofacies

A

Trace fossil association that recurs throughout geologic time in response to a set of paleoenvironmental conditions

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12
Q

Food resource paradigm

A

Limiting factor of distribution of trace making organisms in shallow marine water

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13
Q

Brackish water trace fossil model

A
  1. Reduced diversity of trace fossils in many cases mono specific
  2. Reduced size of trace fossils compared to their fully marine counterparts
  3. Predominance of simple trace fossils
  4. Sparse bioturbation
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14
Q

Ediacaran kimberella

A

In Russia probably a mollusk

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15
Q

Graphic correlation

A

Quantitative method of biostratigraphy developed by Alan shaw. Works by correlating multiple stratigraphic sections
If correlation is 45 degrees then sections had identical fossil distribution and rock accumulation
If different then one section had sediment accumulating faster then the other section

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16
Q

Biostratigraphic resolution

A

Ideally when using biostrigraphy for correlation we would like to do so with the greatest detail. Subdivide rocks into shorter zones this allows us to discriminate between events that happen closer together in time

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17
Q

Precision

A

+ or - error of an age

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18
Q

Dual biostratigraphy

A

Attempts to take in the spatial distribution of fossils as well as the temporal distribution

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19
Q

Bio facies

A

Biotic stratigraphic unit of environmental significance. How these are identified is you look at the different genera in your fossil collection

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20
Q

Paleoecology

A

Study of the interactions of fossils with each other and with the environment they lived in the geological past

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21
Q

Paleoautecology

A

Relationships of individual organisms to their environment

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22
Q

Palesynecology

A

Relationships of groups of organisms to each other and to their environment

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23
Q

Information potential

A

Life habits of extinct organisms
Nature of ancient communities and ecosystems
Paleoenvironmental reconstruction
Sea level changes

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24
Q

Pelagic

A

Live in the water column

Can be subdivided into plankton (floaters) and nekton (swimmers)

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25
Plankton
Usually passive and goes where the current takes them Plant plankton (diatoms) are called phytoplankton and are mostly microscopic Animal plankton are called zooplankton and are mostly microscopic Include foraminifera and jellyfish
26
Nekton
Mostly invertebrates like fish but can also be vertebrates like Cephalopods
27
Benthos
Epifauna (animals) Epiflora (plants) Infauna (living in and moving through the sediment)
28
Sessile
Stay in one place
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Mobile
Move around or in the sea floor
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Primary producers
Autotrophs Manufacture their own food Consumed by primary consumers which are usually suspension feeders
31
Secondary consumers
Consumer primary consumers so are predators
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Tertiary consumers
Consume secondary consumers
33
Transformers and decomposers
Break down the dead that haven't been consumed into organic material that can be recycled
34
Tiering
Prominent in rain forests. Competition for suspension food leads suspension feeders to grow taller then their substrate
35
K strategists
Slow reproductive and growth rates Large bodies Long lived
36
R strategists
Fast reproductive and growth rates Small bodies Short life spans
37
Limiting factors in species distribution
``` Light Food supply Oxygen Salinity Energy Temperature Substrate Water depth ```
38
Light
Promotes photosynthesis | Limiting factor in deep sea
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Food supply
Food greatest at photic zone or near shorelines | Limiting factor in deep marine environments
40
Oxygen
Increase in need of oxygen with increase in size almost all metazoans need oxygen Limiting factor on continental slope and in stagnant zones in the deep ocean
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Salinity
Lower diversity with higher salinity | Limiting factor in hypersaline and brackish environments
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Energy
High energy conditions promote suspension feeders because the wave currents keep organic material suspended within the water Limiting factor in subtidal and coastal areas
43
Temperature
Most fish don't regulate their body temperature but are the same temperature as the water Limiting factor for nearshore environments where the water is subject to seasonal changes in temp
44
Substrate
Composition, mobility, and degree of consolidation play a major role in benthic Faunas
45
Water depth
Effects experienced through increase in hydrostatic pressure Limiting factor in deep marine environments
46
How do trace fossils differ from body fossils
1. Trace fossils usually represent evidence of behaviour 2. The same organism may produce more then one ichnotaxon 3. Same ichnotaxon may be produced by more then one organism 4. Multiple arichtects may produce a single structure 5. Producers are usually soft bodied animals that don't preserve as well 6. Trace fossils are commonly preserved in rock units that are otherwise unfossiliferous 7. The same biogenic structure may be differentially preserved in various substrates 8. Trace fossils commonly have long stratigraphic ranges 9. Trace fossils commonly have narrow environmental ranges 10. Trace fossils are rarely transported
47
Ichnology
Study of traces produced by organisms on or within a substrate
48
Cambrian explosion
Raid diversification Origin of many body plans Fauna: Arthropods trilobites But also echinoderms brachiopods and molluscs
49
Cambrian explosion simple artifact or real event?
Physical changes in the environment Biological changes Reflecting intrinsic evolutionary change
50
Physical changes in the environment
Increase in oxygen levels Widespread transgression Aftermath of snowball earth
51
Biological changes in the environment
Biotic feedbacks that caused or aided the explosion Evolutionary changes underway in the ediacaran Coupling of benthos and plankton
52
Ordivician radiation
Diversification of early bryozoans, brachiopods and stalked Crinoids As well as bivalves and Gastropods
53
4 major taxonomic components of ordivician
Bryozoans Brachiopods Corals Echinoderms
54
Timing of ordivician radiation
Even lasted 25 myr Maintained global diversification characteristic of the Cambrian Diversification of Paleozoic started in the late arenig Ordivician radiation seems to have slowed down by the llanvirn
55
Alpha diversity
Refers to the richness of taxa within a habitat Increased during ordivician radiation Example brachiopods went from having 10 genera within a community in the late Cambrian to 30 by the late ordivician
56
Beta diversity
Refers to taxonomic differentiation within among habitats | Also increased during ordivician
57
Gamma diversity
Records the total (alpha plus beta) for a landscape | Alpha and beta increased so the overall diversity increased
58
Tiering in ordivian
Was an increase in this during this time
59
Carbonate dominated facies (ordivician)
Dominated by articulate brachiopods and sponges
60
Siliclastic dominated facies
Dominated by trilobites and molluscs
61
Ordivician vs Cambrian
Cambrian was more for body plans | Whereas ordivian diversified within groups and families
62
Carboniferous world
``` Ice world Continents were all one mass Large forests source of coal Tropics were wet and warm where the coal swamps were No flowering plants ```
63
What tree dominated most in the coal swamps of the carboniferious?
Lycopods were over 30 m tall possibly 50 m They dominated because they were mostly pole like for their lives and grew their branches last so it allowed them to grow taller then other plants
64
First plants in carboniferious to make an appearance
Seed plants- earliest type was a group called seed ferns | First conifers
65
Carboniferous environment
All of the trees would have led to decreased levels of co2 in the environment This would have led to global cooling Would have led to relative increase in oxygen About 50% higher then it was today
66
Arthropds in the carboniferious
Arthropods in the carboniferious were very large Largest terrestrial Arthropods ever known Why this happened has long been a question Some think it is due to the increase in oxygen levels Or the absence of predators could have attributed to the size
67
Arthropleura
Large millipedes probably 2.5 m long. Trace fossils are found more then their body fossils Found in eastern North America and Scotland Carboniferious
68
Meganeura
Largest insect ever Wing spans of 65 cm carnivores ate insects and possibly small amphibians Carboniferious
69
Amphibians
Large increase in the terrestrial vertebrates Early carboniferious they were pretty diverse and ranged in size from small mouses to pretty large Late carboniferious there was another great radiation. Some became large predators that looked like crocodiles
70
Evolution of amniotes
Group of amphibians known as reptilomorphs | Evolved the ability to lay eggs
71
Earliest known amniotes
Hylonomus from Nova Scotia | Ammoniotes started in the carboniferious but don't start appearing in great numbers until the Permian
72
Mazon creek
Upper carboniferious | Illinois
73
Mazon creek fossilization
Fossils preserved in siderite concretions Fossils are small When these are broken open see 3d moulds The fact that the fossils are 3d and the surrounding siltstone is compressed suggest early formation of the concretions Also since the concretions mirror the shape of the organism suggests the organism played a role in the concretion formation
74
MaZon creek biota
Northern (braidwood biota) terrestrial and freshwater in composition and dominated by plants Southern (Essex biota) fully marine in composition and dominated by invertebrates
75
Terrestrial and aquatic animals for Mazon creek
Terrestrial: Arthropods, insects, arachnids, mryiapods Aquatic: bivalves, jellyfish, tully monster swimming invertebrate predators
76
Joggins
Nova Scotia Incredible tides expose more and more fossils Trees in upright positions
77
Plants and fauna of joggins
Plants: lycopods and spore trees like that in the coal swamp Fauna: hylonomus found in stumps of trees Many amphibians: crocodile sizes predators Arthropods: horse shoe crab traces, whip spiders
78
Permian
Synapsids became the most dominant | Synapsids broken up into paraphyletic pelycosaur and therapsids later
79
Sails
Spines were connected by tough layering of skins and that there were many blood vessels in the sails Been suggested that these were used for thermoreagulation by giving them an advantage in cool mornings, and also needing to cool down later in the day
80
Cynodonts
In the Triassic became more and more mammal like
81
What is one of the key evolutionary transitions for mammal like synapsids?
The reduction of the number of bones in the lower jaw and their migration to the inner ear
82
Mesosaurs
First fully aquatic amniotes | Teeth suggest they ate fish or Arthropods
83
Protolophonids
Late Permian to late Triassic anapids | Either herbivores or insectivores
84
Triassic beginning vs end
Beginning was Dominanted by synapsids but by the end was dominated by diapsids most popular of which are archosaurs
85
Archosaurs
Group of dilapidated amniotes which include non avian dinosaurs, pterosaurs, birds and crocodiles
86
Two divisions of archosaurs
Crurotarsi- lead to crocodiles and their ancestors | Avemetatarsalia- lead to dinosaurs and birds
87
Permo triassic mass extinction
83% of all genera disappeared Marine invertebrates suffered the most losses Terrestrial plants see reorganization
88
Why were the basal archosaurs so successful?
Posture: moving from a sprawling position to an upright stance Uris acid rather then urea: different mechanisms for excretion of ammonia favored by diapsids during the Triassic
89
Archosaurs posture
Having an erect posture is metabolically expensive and requires more energy Suggests that they had higher metabolism and higher body temperatures and would need more food and oxygen
90
Waste removal
Triassic was arid compared to the Permian | Archosaurs had a different mechanisms for excreting ammonia (uric acid) rather then synapsids (urea)
91
After permo Triassic extinction
Archosaurs diversified after this, and took over niches that were formerly occupied by synapsids Archosaurs were probably endothermic, meaning crocodiles reverted back to ectothermy Birds retain endothermy
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Ophiacodon
Synapsids Permian First large amniote Carnivore
92
Caseids
Synapsid Largest herbivore Permian
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Sailed back two division
Edaphasuarids: herbivores Sphenacodonids: carnivores
92
Dinocpehalians
Permian Therapsids Herbivores and carnivores
92
Dicynodonts
Herbivores | Therapsids
93
Gorgonopsians
Therapsids | Carnivores
94
Phytosaurs
Archosaurs: crurotarsi | Mid late Triassic
95
Postosuchus
Erect gait Largest of Triassic Archosaurs: crurotarsi
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Sphenosuchus
Archosaurs: crurotarsi | Late Triassic
97
Crocodiles
Jurassic to Cretaceous
98
Pterosaurs
Archosaurs: avemetatarsalia | Earliest known vertebrates to have evolved flight
99
Lagosuchus
Dinosauromorphs Middle Triassic Sister taxa to dinosaurs Share many characteristic with them
100
Dinosauria
First arose in the late Triassic and dominated until the Cretaceous Became successful in the Jurassic and Cretaceous before Going extinct at the Cretaceous/tertiary boundary 65 mya
101
Dinosaurs
Generally described as archosaurs with limbs held erect beneath the body
102
Ceratopsidae
Upper Cretaceous Quadrupedal herbivores Characterized by horns frills shearing teeth
103
Hadrosauridae
Known for duck bill | Skeleton adapt for running not swimming
104
Auditory signalling
Hadrosauridae | Resonating chambers to produce sound
105
Sexual signalling
Significant differences between males and females of the same species
106
Stegosauridae
Jurassic to Cretaceous Characterized by plates on their back Probably slow moving because their front legs were dramatically shorter then their back
107
Sauropods
Jurassic to Cretaceous Neck elongated Achieved size through air sacs and hollowing of bones
108
Theropods
Bipedal carnivorous dinosaurs
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tyrannosaurids
``` Jurassic to Cretaceous Only found in asia and North America Alex predators Fastest of the large theropods Coelurosaurs ```
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dromaesauridae
``` Raptors Travelled in packs Active fast predators Theropods Coelurosaurs ```
111
avialae
Containing their only representative: birds Defined as all dinosaurs possessing feathers used in flapping flight Coelurosaurs
112
Ornithischians
``` Hadrosaurs Ceratopsians Stegosaurus Ankylosaurus Pachycephalsaurus ```
113
Saurischians
Sauropods and theropods
114
Who used brooding? And what was it
Hadrosaurs, ceratopsians and theropods are to have cared for their young
115
Turtles
Triassic to recent Bony shell In diapsids
116
Turtles divided into two groups based on what
Necks Cryptodires Pleurodires
117
Plesiosaurs
``` Jurassic to Cretaceous Evolved from crocodile like ancestor Retained limbs that were modified into flippers Sauropterygia Reptiles ```
118
Ichthyosaurs
Triassic to Cretaceous Air breathing, fast swimmers Dolphin like body Example of convergent evolution
119
Squamates
Lizards and snakes Evolving in the Permian Mobility Venom
120
Mesosaurs
Cretaceous Evolved form semi aquatic squamates Apex predator outcompeting ichthyosaurs and plesiosaurs