Deep sea environment Flashcards

1
Q

Deep sea characteristics

A

75% of all ocean water is deep sea
-Between 1000m-6000m
-consists of:
-low temp
-high pressure
-low nutrient levels
-Complete darkness such that photosynthesis relying on sunlight is impossible and must be chemotrophic

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2
Q

Pressure adaptions

A

-Outer membrane protein H: It is a porin that makes it easier to extract nutrients from the environment
-Cell membrane is composed of unsaturated fatty acid tails that increases the fluidity of membrane: useful for high pressure and cold as it prevents membrane from hardening and freezing
-proteins are predominantely made from alpha helices to give increased felxibility

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3
Q

type of microbes

A

piezophillic or piezotolerant
There are also psychrophilic and phsychrotoelrant as well as thermophilic and thermotolerant

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4
Q

Archaea high temp adaptions

A

Ether linkages in membrane instead of ester linkages which makes them more stable

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5
Q

Molecular effects of high pressure

A

-Piezophiles have mulitple pressure-detecting systems and pressure-regulated genes that are only expressed at high pressure
-Enzymes do not require high pressure to function, only genes
-gram negative piezophiles regulate expression of porins based on pressure

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6
Q

Culture these bacteria

A

must used specialised growth chambers that simulate high pressure and cold

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7
Q

Deep-sea sediment samples

A

-Archaeal and bacterial pop occur at depths greater than 2000m
-Samples are harvested by drilling ocean floor
-There are fewer deep-sea microbes at greater depths than are found closer to the surface of the rock layer as sub-seafloor ecosystems contain 4*10^15g of microbial cellular carbon

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8
Q

Phylogenetic diversity of marine sediment Pro

A

-Proteabacteria dominate
-Bacteroidetes and unclassified/minor groups also present
-minor amounts of cyanobacteria (sulphur-reducing)
-Novel phyla of Archaea unrelated to cultured representatives (not related to any other Archaeal species) are widespread in deep subsurface

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9
Q

-Hydrothermal vent formation

A

Occur due to fissure in earth’s crust or when tectonic plates collide which releases heat from molten rock
-Hydrothermal fluid rich in: Fe, Cu, Ca, S, SO3

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10
Q

Warm vent formation

A

Occur when hydrothermal fluids combine with water before they leave, which causes warm water to be released

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11
Q

Hot vent formation

A

Occur when hydrothermal fluid directly leaves vents in ocean

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12
Q

Hydrothermal vents M type

A

-Chemolithotrophs B predominate at vent
-Thermophiles and hyperthermophiles are present
-Chemolithotrophic Pro utilise inorganic materials from vents

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13
Q

Phylogenetic diversity at hydrothermal vents

A

-Detected by FISH staining
-Pyrolobus and Pyrodictium are thermophillic sulfur-reducing M
-Most M are Proteobacteria such as Alpha, Gamma, Delta and Epsilon
-limited Archae

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14
Q

Difference between pelagibacter and anoxygenic aerobic phototrophs

A

Pelagibacter are primarily chemo organotrophic, using organic carbon for energy and carbon source
-They supplement their diets using light to produce ATP in order to survive in nutrient scarce environments
Aerobic anoxygenic phototrophs- are phototoheterotrophic and use only light as their energy source, in presence of oxygen, and use organic carbon as carbon source

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