carbon entersthe soil frombeneath viaroots &mycorrhizalfungicarbonsequestration isthe intake andstorage of theelement carbonthe carboncompounds thatremain in the soil overthe long term havebeen produced byfungi and othermicrobes, not byplantsectomycorrhizalfungi arecommon in highlatitudesystemsreduced fungalabundanceafter wildfirescan persist forseveral yearstrees & plantsabsorb carbondioxide andproduce oxygtwo groups ofmychorrhizalfungi, ericoidandectomycorrhizalfungihypae die,thecarbon in theirtssues could bedecomposed byother soilmicrobesdead fungaltissues decayfaster infrequentlyburned borealforests soilmycorrhizal fungimake smallercontributions tosoil carbon inmore frequentlyburned borealforestsduringphotosynthesis,treesand plants storecarbon as theyabsorb carbondioxidethe longer themycorrhizal carbonremains in the soil,the greatercontribution to soilcarbon sequestrationericoid fungidominatethe deepersoilscarbon storedin soil can helpthe release ofgreenhousegases to theatmospheremycorrhizalfungi removeatmosphericCO2 by theirplant hostthe extent to whichmycorrhizal fungiimprove plant growthcan also determine howmuch carbon isdeposited in the soil viadead plant material50 to 70% of storedcarbon in achronosequence ofboreal forestedislands derives fromroots and root-associatedmicroorganismshyphae die, thecarbon in theirtissues couldremain in thesoil for years ordecadesectomycorrhizalfungi tend todecline afternitrogenenrichmentwildfiresdecrease theabundance ofectomycorrhizalfungithe borealforest biomecovers 11%of the landsurfaceboreal forestbiome contains16% of thecarbon stocksequestered insoilsmycorrhizal fungiare a dominantcomponent of themicrobialcommunity in soilsplants soak up thecarbon that wouldotherwise rise upand trap heat inthe atmospherecarbon entersthe soil frombeneath viaroots &mycorrhizalfungicarbonsequestration isthe intake andstorage of theelement carbonthe carboncompounds thatremain in the soil overthe long term havebeen produced byfungi and othermicrobes, not byplantsectomycorrhizalfungi arecommon in highlatitudesystemsreduced fungalabundanceafter wildfirescan persist forseveral yearstrees & plantsabsorb carbondioxide andproduce oxygtwo groups ofmychorrhizalfungi, ericoidandectomycorrhizalfungihypae die,thecarbon in theirtssues could bedecomposed byother soilmicrobesdead fungaltissues decayfaster infrequentlyburned borealforests soilmycorrhizal fungimake smallercontributions tosoil carbon inmore frequentlyburned borealforestsduringphotosynthesis,treesand plants storecarbon as theyabsorb carbondioxidethe longer themycorrhizal carbonremains in the soil,the greatercontribution to soilcarbon sequestrationericoid fungidominatethe deepersoilscarbon storedin soil can helpthe release ofgreenhousegases to theatmospheremycorrhizalfungi removeatmosphericCO2 by theirplant hostthe extent to whichmycorrhizal fungiimprove plant growthcan also determine howmuch carbon isdeposited in the soil viadead plant material50 to 70% of storedcarbon in achronosequence ofboreal forestedislands derives fromroots and root-associatedmicroorganismshyphae die, thecarbon in theirtissues couldremain in thesoil for years ordecadesectomycorrhizalfungi tend todecline afternitrogenenrichmentwildfiresdecrease theabundance ofectomycorrhizalfungithe borealforest biomecovers 11%of the landsurfaceboreal forestbiome contains16% of thecarbon stocksequestered insoilsmycorrhizal fungiare a dominantcomponent of themicrobialcommunity in soilsplants soak up thecarbon that wouldotherwise rise upand trap heat inthe atmosphere

Untitled Bingo - Call List

(Print) Use this randomly generated list as your call list when playing the game. There is no need to say the BINGO column name. Place some kind of mark (like an X, a checkmark, a dot, tally mark, etc) on each cell as you announce it, to keep track. You can also cut out each item, place them in a bag and pull words from the bag.


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  1. carbon enters the soil from beneath via roots & mycorrhizal fungi
  2. carbon sequestration is the intake and storage of the element carbon
  3. the carbon compounds that remain in the soil over the long term have been produced by fungi and other microbes, not by plants
  4. ectomycorrhizal fungi are common in high latitude systems
  5. reduced fungal abundance after wildfires can persist for several years
  6. trees & plants absorb carbon dioxide and produce oxyg
  7. two groups of mychorrhizal fungi, ericoid and ectomycorrhizal fungi
  8. hypae die,the carbon in their tssues could be decomposed by other soil microbes
  9. dead fungal tissues decay faster in frequently burned boreal forests soil
  10. mycorrhizal fungi make smaller contributions to soil carbon in more frequently burned boreal forests
  11. during photosynthesis,trees and plants store carbon as they absorb carbon dioxide
  12. the longer the mycorrhizal carbon remains in the soil, the greater contribution to soil carbon sequestration
  13. ericoid fungi dominate the deeper soils
  14. carbon stored in soil can help the release of greenhouse gases to the atmosphere
  15. mycorrhizal fungi remove atmospheric CO2 by their plant host
  16. the extent to which mycorrhizal fungi improve plant growth can also determine how much carbon is deposited in the soil via dead plant material
  17. 50 to 70% of stored carbon in a chronosequence of boreal forested islands derives from roots and root-associated microorganisms
  18. hyphae die, the carbon in their tissues could remain in the soil for years or decades
  19. ectomycorrhizal fungi tend to decline after nitrogen enrichment
  20. wildfires decrease the abundance of ectomycorrhizal fungi
  21. the boreal forest biome covers 11% of the land surface
  22. boreal forest biome contains 16% of the carbon stock sequestered in soils
  23. mycorrhizal fungi are a dominant component of the microbial community in soils
  24. plants soak up the carbon that would otherwise rise up and trap heat in the atmosphere