arbontiuxesmmm
timescale
EastRISD ML
storesoverayearly
exchangeprom
ismomas an xx
nee
one
through b iochemical
carbon
cycle
one
enquiryquestion
photosynthesisisone
one amount
big tax
largest oneto
atmosphere or cozitremovesmomone
Bf
itii
nowdoesthecarbonaceoperatetomaintainpanetans
mean
sedimentaryrocksare the
roarscontainnign
limestone
rationsor
m
carbonate
calcium
concent
a
theatmosphere
thehydrosphere water asdissolvedco
ÉÉ I
beingcompactedovermillionsoryears thelithosphereas carbonates inlimestone 1
limestoneisveryvulnerable to
andfossilfuels
ne y
11,4 1 i É
chemicalweatheringasonerain
dissolvesonecalciumcarbonate
carbonsink southernocean d M effect
mn
estimatedtoaccountfor
251 ordiffusionorconom
theatmosphere tooceans
bycarboninputsfromphotosynthesisand
carbonlossesbyrespiration
healthysoilsare dark
immense asmethaneorco inone
atmospherewhich
traps onesun's
greenhousegasesnaturallyfluctuate
butwe'veenhancedthisthrough
wormscontain crumbly contain burningorfossil
fuelsanddeforestation
organicmatterandsequester
carbon
iT
importance ofdifferentcarbon stores
mangroves growquicklyandsequester
mmmm.mn eventswillbecomecommon increasedflash
flooding which
Perheureeveryyear
icecapsmatand sealevelsrise
tundrasoils much or thesoil intundra eventsandmoreenergy
ecosystems 2080birdhabitatswillbe
by gifford
locksonecarbonin forthousands reducedfromincreasedtemperatures 101 tropicalstormsand
oryears orlandspecies with limitedadaptability
tropicalrainforests carbonmainlystoredintrees faceextinction andlessbiodiversity in
andplants butmagicstoreone
mm Africa
timescale
EastRISD ML
storesoverayearly
exchangeprom
ismomas an xx
nee
one
through b iochemical
carbon
cycle
one
enquiryquestion
photosynthesisisone
one amount
big tax
largest oneto
atmosphere or cozitremovesmomone
Bf
itii
nowdoesthecarbonaceoperatetomaintainpanetans
mean
sedimentaryrocksare the
roarscontainnign
limestone
rationsor
m
carbonate
calcium
concent
a
theatmosphere
thehydrosphere water asdissolvedco
ÉÉ I
beingcompactedovermillionsoryears thelithosphereas carbonates inlimestone 1
limestoneisveryvulnerable to
andfossilfuels
ne y
11,4 1 i É
chemicalweatheringasonerain
dissolvesonecalciumcarbonate
carbonsink southernocean d M effect
mn
estimatedtoaccountfor
251 ordiffusionorconom
theatmosphere tooceans
bycarboninputsfromphotosynthesisand
carbonlossesbyrespiration
healthysoilsare dark
immense asmethaneorco inone
atmospherewhich
traps onesun's
greenhousegasesnaturallyfluctuate
butwe'veenhancedthisthrough
wormscontain crumbly contain burningorfossil
fuelsanddeforestation
organicmatterandsequester
carbon
iT
importance ofdifferentcarbon stores
mangroves growquicklyandsequester
mmmm.mn eventswillbecomecommon increasedflash
flooding which
Perheureeveryyear
icecapsmatand sealevelsrise
tundrasoils much or thesoil intundra eventsandmoreenergy
ecosystems 2080birdhabitatswillbe
by gifford
locksonecarbonin forthousands reducedfromincreasedtemperatures 101 tropicalstormsand
oryears orlandspecies with limitedadaptability
tropicalrainforests carbonmainlystoredintrees faceextinction andlessbiodiversity in
andplants butmagicstoreone
mm Africa
