Terrestrial environment Flashcards

1
Q

soil

A

Loose outer material of earth’s surace

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2
Q

Soil layers

A

O horizon
A horizon
B horizon
C horizon

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3
Q

O horizon

A

At the surface, composed of undecomposed plant material

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4
Q

A horizon

A

Most M growth, rich in organic material and nutrients
Plant roots release nutrients in exchange for ecosystem function

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5
Q

B horizon

A

subsoil where organic material leached from A gather, little M activity

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6
Q

C horizon

A

base that is directly above bedrock and forms from bedrock
No O2 and all microbes strictly chemolithotrophs

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7
Q

Soil groups

A

Mineral soil
organic soil

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8
Q

Mineral soil

A

Derived from rock weatherig and other inorganic material

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9
Q

Organic soil

A

Derived from sedimentation in bogs and marshes

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10
Q

soil composition

A

40% inorganic mineral
5% organic matter
50% air and water
5% M and macro organisms

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11
Q

Soil formation

A

Formed by interdependant physical, chemical and biological processes
-CO2 is formed by respiring organisms that form Carbonic acid that breaks down rock
-Physical processes such as freezing and thawing break apart rocks, allowing plant roots to penetrate and form an expanded rhizosphere

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12
Q

Rhizosphere

A

Area around plant roots where plants secrete sugars and other compounds, is rich in organic matter and microbial life

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13
Q

water availibility

A

It is variable and dependant on rainfall, plant coverage, drainage and soil composition

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14
Q

Soil solution

A

Soil water has many dissolved materials

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15
Q

soil and water

A

Well-drained soils have O2 availibility while waterlogged soils are typically anoxic, with O2 being consumed by soil M

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16
Q

Arid soils

A

They are dry, have limited plant growth and are home to M communities specialised for extreme conditions
-Arid soils lose more moisture from evapotranspiration than gained from precipitation
-Make 35% of land mass and are extreme environments with low water availibility and varied temp ( below -24 and above 60)

17
Q

BSC

A

Biological soil crusts are made of photosynthetic cyanobacteria and filamentous fungi that stabilise soil

18
Q

BSC and arid

A

Arid soils are very slow to form and are subject to desertification, where BSC is damaged and soil fertility is decreased

19
Q

Phylogenetic sampling

A

Molecular sampling indicates thousands of different M species

20
Q

Phylotype

A

A species defined by a 16S rRNA sequence that differs from all other sequences by 3%
M diversity varies with soil type and geological location

21
Q

Red well

A

Due to M that convert Fe3+ in soil to Fe2+ that goes into water

22
Q

Most limiting nutrients

A

Nitrogen
Phosphorous

23
Q

Polluted soil

A

-Undisturbed, unpolluted soils support very high Pro diversity
-soil perturbations trigger measurable shifts in community composition toward species that are more competitive
-Polluted soils reduce richness and increase species abundance

24
Q

Climate and disturbance effects on soil M

A

Microbial diversity in any environment is a dynamic entity and will change-sometimes dramatically- in response to environmental changes in conditions and resources

24
Q

Soil subsurface

A

-extend for sevral hundred meters below soil surface
-Archae and B exist here in variable concentrations depending on nutrient availibility
-Usually grows in extremely nutrient limited environment
-small cells common

25
Q

Deep subsurface

A

Home to a group of organisms that may be Archae and are related to Eu, the lokiarcheota
-Generation time can be days, years or centuries depending on nutrients

26
Q

Determine microbe diversity

A

-Suspend soil in sterile liquid and then shake and let settle
-Use DNA extraction kit
-Use 16S ALAnine primers to amplify and then sequence DNA
-Use sequence to determine phylotype of soil M
-If % similarity is lower than 97% of reference genome, it may belong to a new species
-If species can’t be determined than full genome sequencing must be done to discover new species