Investigate The Conquest of Land by Animals Flashcards

1
Q

Due to trace fossils being common from about 450MYA, what does that suggest about invertebrates and vertebrates?

A

It suggests that invertebrates colonised the land long before our vertebrate ancestors

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1
Q

What is the first accepted evidence for animals occupying terrestrial environments?

A

The footprints & tracks of myriapods (a group with elongated bodies & numerous leg-bearing segments): Millipedes and eurypterids.

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2
Q

What are Terrestrial Vertebrates?

A

(animals with a backbone) who spend the majority of their lives on land. While terrestrial vertebrates form a minor proportion of all invasive species, their impacts are often disproportionately high.

First ventured on land during the middle of the Devonian period. During this period vertebrate fish diversified and became a dominant group of oceanic animals.

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3
Q

Advantages of life on land?

A

-Sunlight is stronger ( water filters out parts of the colour spectrum within the first two meters).

-More Carbon Dioxide in the atmosphere THAN in the ocean (good for photosynthesis = plants)

-Mineral nutrients are plentiful in the soil (good for plants)

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4
Q

Disadvantages/Challenges of Life on Land:

A

-Less available water

-No support against gravity (plants need some form of structure support)

-Gas exchange (having to utilise AIR rather than WATER)

-Reproduction (simply releasing sperm or eggs into the water will no longer work so a new system needs to be developed)

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5
Q

sameas other

How did fish ancestors come out of water?

A

Converting their FINS to LIMBS
&
breathing UNDER-WATER to AIR-BREATHING

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6
Q

How did animals move from water to land?

A

A STRONG pelvic girdle and laterally positioned, forward-facing legs allowed them to walk.

AND

The evolution of lungs allowed the amphibians to move away from the water for extended periods of time

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7
Q

How did CYANOBACTERIA affect the GEOSPHERE?

A

-The formation of BIF’S

-The increase in oxygen levels was also creating additional oxidation in some of the surface minerals.

-Hydroxide & oxide minerals INCREASED clay-based rocks from the Proterozoic Eon.

-Great Oxygenation Event

-Carbon dioxide removed

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8
Q

How did CYANOBACTERIA affect the ATOMOSPHERE?

A

-Fundamental shift in the composition of the atmosphere.

-Reduction of Co2 & CH4 from atmosphere (may have lead to global cooling = SNOWBALL EARTH)

-Ozone developed

-Co2 combines to create new organic molecules

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9
Q

How did CYANOBACTERIA affect the HYDROSPHERE?

A

-The cyanobacteria were in the shallow waters of the ocean, which means the oxygen levels in the hydrosphere changed first.

-Snowball earth covered oceans in ice

-Co2 removal in oceans decreases pH

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10
Q

What is a mould formation?

A

The imprint LEFT BY THE ORGANISM on the material that surrounded it. ( 2D + Inside Shell)

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11
Q

What is a cast formation?

A

A mould fossil that is FILLED IN WITH MINERALS that harden over time. (3D + Outside Shell)

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12
Q

What are Trace Fossils?

A

Trace Fossils are the tracks, trails, impact marks and footprints that organisms made when they were alive.

These fossils have the ability to capture an event that only lasted a few seconds and that occurred about 100 million years ago.

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13
Q

What do footprints of trace fossils show?

A

-Type of organism?
-How tall?
-How fast?
-How many?
-How heavy?
-Which direction?

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14
Q

What do coprolites (feces) of trace fossils show?

A

-Type of organism?
-What diet?
-What features about the digestion?
-What environment?

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15
Q

What is an index fossil used for?

A

Date rocks. The presence of an index fossil in a sedimentary rock indicates that it was formed during a particularly short period.

16
Q

A good index fossil has these 5 characteristics:

A

1) Distinct
2) Globally widespread
3) Abundant
4) Limited to a particular geological time
5) Robust & Preserves well

17
Q

How is absolute dating conducted?

A

It is based on the fact that living organisms—like trees, plants, people, and animals—absorb carbon-14 into their tissue. When they die, the carbon-14 starts to change into other atoms over time. Scientists can estimate how long the organism has been dead by counting the remaining carbon-14 atoms. Therefore if we know what those are, we can collect uncontaminated samples, and then we receive an understanding of the sample’s age.

18
Q

What is relative dating? and how is it done?

A

The process of determining if one rock or geologic event is older or younger than the other, without knowing their specific ages.

(Less detailed)

Done through: Stratigraphic correlation and Superposition.

19
Q

What is bracketing?

A

Occurs when you have similar fossils, where there is some sort of overlap in time.

20
Q

Conquest of land for animals:

A

arthropods developed exoskeletons, amphibians developed limbs, amniotic egg

21
Q

Conquest of land for plants:

A

developed vascular systems, roots, waxy cuticles and seeds

22
Q

Conditions in forming fossils:

A

-Sinks to water bead
-Quickly buried
-Sediment turned to rock
-Minerals dissolve
-Exposure of fossil

23
Q
A