where is biodiversity ? Flashcards

Lecture 3 - John Spicer

1
Q

species-area relationship

principle pattern

A

as size of geographical area increases so to does the number of species

practical use - predict that as area is reduced, tend to lose species

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2
Q

habitat loss / fragmentation

A

major determinant of modern extinctions

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3
Q

sea/land phyla

A

all animal phyla ( approx 34 ) occur in the sea (one exception - velvet worms (onychophora))

two thirds ( 20 ) almost exclusively marine

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4
Q

marine phyla

A

98 % live in/on the sea floor ( = BENTHIC )

2 % live floating or swimming in the sea ( = PELAGIC )

only 15% of named species are marine

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5
Q

photosynthesis - sea/land comparason

A

sea : very few, large photosynthetic organisms - mainly short lived, microscopic algae

land : dominated by persistant long lived ‘large’ flowering plants

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6
Q

herbivoress - sea/land comparason

A

sea : dominant herbivores - micro (copepods) majority of large animals carnivorous

land : dominant herbivores can be large

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7
Q

grazing - sea/land comparason

A

sea : grazing - ingestion of entire autotroph

land : grazing - rarely removes significant amounts of communities ( indigestible e.g wood )

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8
Q

autotroph

A

an organism that can produce its own food using light, water, carbon dioxide, or other chemicals

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9
Q

food chain - sea/land comparason

A

sea : food chain average 5 links

land : food chain average 3 links

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10
Q

abyssal

A

depths od ocean between 4000-6000m deep

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11
Q

bathyal

A

relating to the zone of the sea between the continental shelf and the abyssal zone (depths 1000 - 4000m)

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12
Q

hadal

A

relating to the zone of the sea greater than 6000 m in depth chiefly oceanic trenches

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13
Q

littoral

A

area of shoreline where land is subject to wave action

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14
Q

sublittoral

A

living, growing, or accumulating near to or just below the shore

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15
Q

endemic species

A

plants and animals that exist only in one geographic region

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16
Q

Alexander Von humboldt

A

latitude - 1799 onwards

Venezuela - Mexico : species identity differs with latitude

17
Q

Alfred Russel Wallace

A

number os species increases as you go from temperate to tropical regions

18
Q

planktonic diversity

A
  • all 3 domains of life
  • overall decline in diversity towards the poles ( saame pattern as on land )
  • driven by decresing water temperatures
19
Q

species richness

A

the number of species within a defined region

20
Q

shallow water - species richness

A
  • coastal marine fish/bacteria - increase in species richness towards the equator
  • coral reef fish - no pattern
  • amphipods/isopods/bivalves - highest before reach the equator
21
Q

deep sea - species richness

A
  • increase in richness towards the equator for number of taxa of bivalves, gastropods and isopods
  • forminiferans - highest before reach the equator ( single celled protists - very simple microorganisms )
22
Q

pelagic - species richness

A
  • increase in richness towards the equator - ostracods, euphausiids (krill), shrimp, fish (N. hemisphere), bacteria,
23
Q

elevation

A

Von Humboldt - number and type of plant species changed as ascended volcano

species richness decreases with increasing elevation

24
Q

life below Earth’s surface

A

endemic cave communities
- chemosynthetic ecosytem (chemosynthesis is the process by which certain microbes create energy by mediating chemical reactions)

25
Q

azoic zone hypothesis

A

Edward Forbes

there was zero life below the azoic zone (550m)

hypothesis was short lived

26
Q

depth : species richness

A

species richness decreases with depth

27
Q

depth ( species richness )

A
  • overall decrease in species richness with increasing depth
  • diversity peaks at intermediate depths ( 0.3 - 4.7 km )
  • pelagic peak - more shallow than benthic
  • pressure and temperatire thought to limit species richness