boreal forestbiome contains16% of thecarbon stocksequestered insoilsduringphotosynthesis,treesand plants storecarbon as theyabsorb carbondioxidehypae die,thecarbon in theirtssues could bedecomposed byother soilmicrobesdead fungaltissues decayfaster infrequentlyburned borealforests soilcarbonsequestration isthe intake andstorage of theelement carbonthe carboncompounds thatremain in the soil overthe long term havebeen produced byfungi and othermicrobes, not byplantscarbon storedin soil can helpthe release ofgreenhousegases to theatmospherethe extent to whichmycorrhizal fungiimprove plant growthcan also determine howmuch carbon isdeposited in the soil viadead plant materialreduced fungalabundanceafter wildfirescan persist forseveral yearscarbon entersthe soil frombeneath viaroots &mycorrhizalfungiectomycorrhizalfungi tend todecline afternitrogenenrichmentericoid fungidominatethe deepersoilsplants soak up thecarbon that wouldotherwise rise upand trap heat inthe atmosphereectomycorrhizalfungi arecommon in highlatitudesystemsmycorrhizal fungiare a dominantcomponent of themicrobialcommunity in soils50 to 70% of storedcarbon in achronosequence ofboreal forestedislands derives fromroots and root-associatedmicroorganismsthe longer themycorrhizal carbonremains in the soil,the greatercontribution to soilcarbon sequestrationtwo groups ofmychorrhizalfungi, ericoidandectomycorrhizalfungithe borealforest biomecovers 11%of the landsurfacemycorrhizal fungimake smallercontributions tosoil carbon inmore frequentlyburned borealforestswildfiresdecrease theabundance ofectomycorrhizalfungimycorrhizalfungi removeatmosphericCO2 by theirplant hosttrees & plantsabsorb carbondioxide andproduce oxyghyphae die, thecarbon in theirtissues couldremain in thesoil for years ordecadesboreal forestbiome contains16% of thecarbon stocksequestered insoilsduringphotosynthesis,treesand plants storecarbon as theyabsorb carbondioxidehypae die,thecarbon in theirtssues could bedecomposed byother soilmicrobesdead fungaltissues decayfaster infrequentlyburned borealforests soilcarbonsequestration isthe intake andstorage of theelement carbonthe carboncompounds thatremain in the soil overthe long term havebeen produced byfungi and othermicrobes, not byplantscarbon storedin soil can helpthe release ofgreenhousegases to theatmospherethe extent to whichmycorrhizal fungiimprove plant growthcan also determine howmuch carbon isdeposited in the soil viadead plant materialreduced fungalabundanceafter wildfirescan persist forseveral yearscarbon entersthe soil frombeneath viaroots &mycorrhizalfungiectomycorrhizalfungi tend todecline afternitrogenenrichmentericoid fungidominatethe deepersoilsplants soak up thecarbon that wouldotherwise rise upand trap heat inthe atmosphereectomycorrhizalfungi arecommon in highlatitudesystemsmycorrhizal fungiare a dominantcomponent of themicrobialcommunity in soils50 to 70% of storedcarbon in achronosequence ofboreal forestedislands derives fromroots and root-associatedmicroorganismsthe longer themycorrhizal carbonremains in the soil,the greatercontribution to soilcarbon sequestrationtwo groups ofmychorrhizalfungi, ericoidandectomycorrhizalfungithe borealforest biomecovers 11%of the landsurfacemycorrhizal fungimake smallercontributions tosoil carbon inmore frequentlyburned borealforestswildfiresdecrease theabundance ofectomycorrhizalfungimycorrhizalfungi removeatmosphericCO2 by theirplant hosttrees & plantsabsorb carbondioxide andproduce oxyghyphae die, thecarbon in theirtissues couldremain in thesoil for years ordecades

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