Carbon at a variety of scales Flashcards
(on a local scale) trees act as …
biological sequestrators (storing carbon in stems and leaves)
explain the carbon cycle of a tree
coverts atmospheric co2 into organic molecules (vital for growth) through photosynthesis. co2 then descends through the root of the tree and is released into the soil through root cell respiration and the death of roots. co2 is also marginally released through plant respiration and when leaf litter falls and decomposes. decomposed leaf litter can also sink into soil- carbon stored in leaves transferred to soil
what is a ‘sere’
is a vegetation succession (a sequence of changes) that relate to a specific environment
lithosere definition
vegetation succession that occurs on bare rock
hydrosere definition
water/pond
halosere definition
salt marsh
psamosere definition
coastal/ sand dunes
first stage of vegetation succession in the lithosere
rock is exposed for the first time (eg after glacial retreat, tectonic uplift)
second stage of vegetation succession in the lithosere (weathering)
rock is slowly weathered and carbon can be released (dissolved in water)– links to the water cycle as it gets transferred to other stores
third stage of vegetation succession in the lithosere (vegetation)
vegetation (eg lichen and moss) starts to grow on bare rock and carbon exchange (photosynthesis) occurs
fourth stage of vegetation succession in the lithosere (soil)
as organic matter (leaf litter) is added to broken rock, a soil develops= wider range of plants
fifth stage of vegetation succession in the lithosere (why soil is important)
soil is very important as it can absorb and store carbon over long periods
sixth stage of vegetation succession in the lithosere (why more carbon is better)
more carbon in soil = different habitats established and range of wildlife
seventh (final) stage of vegetation succession in the lithosere
is reached when environmental equilibrium is achieved — climatic climax
carbon cycle at a continental scale (long– talk about weathering, oceans, tectonic uplift, volcanoes, etc)
acid rain reacts with minerals–slowly dissolves through chemical weathering–carbon left in water–carried by surface water to ocean–settles in the form of calcium carbonate–used by shells and corals (coral respiring released co2)– dead ones sink and become buried–turned to limestone–tectonic uplift exposes limestone–tectonic forces mean oceanic plate subducts beneath continental–deposits then subject to convection currents–rise back to surface through volcanic eruptions–co2 released back into atmosphere where it is dissolved in water. GOES BACK TO BEGINNING