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peatland (en) ![]() | ||||
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Bayanai | ||||
Ƙaramin ɓangare na |
daji, marsh (en) ![]() ![]() | |||
Yana haddasa |
peat (en) ![]() | |||
Has characteristic (en) ![]() |
carbon sink (en) ![]() | |||
Wuri | ||||
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Gidajen da ke cike da turɓaya sune gandun daji masu zafi inda ƙasa mai ruwa ke hana ganye da itace su lalacewa. A tsawon lokaci, wannan yana haifar da wani nau'i mai zurfi na acidic peat.[1] Ana sare manyan yankuna na waɗannan gandun daji a manyan farashi.
Gidajen da ke cike da turare yawanci suna kewaye da gandun daji masu ruwan sama a kan ƙasa mai kyau, da kuma gandun daji mai ruwan gishiri ko ruwan gishiri kusa da bakin teku.
Su ne wani nau'i na peatland, wanda ke adanawa da tara adadi mai yawa na carbon a matsayin kwayoyin halitta na ƙasa - fiye da gandun daji a kan ƙasa mai ma'adinai (watau wanda ba shine ƙasa) da ke ciki. Tsarin peat shine sink na halitta na carbon; saboda lalacewar kwayoyin halitta yana da jinkiri fiye da yawan samar da shi, raguwa yana tarawa a matsayin peat. Tsayinsu yana da muhimmiyar tasiri ga Canjin yanayi; suna daga cikin manyan wuraren ajiyar carbon na ƙasa.[1] Gidajen da ke da zafi, waɗanda ke da muhimmancin muhalli, suna ɗaya daga cikin waɗanda aka fi barazana, duk da haka ba a yi nazari sosai ba kuma ba a fahimta sosai ba.
Tun daga shekarun 1970s, sare gandun daji na wurare masu zafi da kuma zubar da ruwa sun karu sosai a Kudu maso Gabashin Asiya.[2] Bugu da kari, El Niño Southern Oscillation (ENSO) fari da manyan gobara suna hanzarta lalacewar peatland. Wutar peat, magudanar ruwa da kuma sare daji yana inganta lalacewar kwayoyin ƙasa, yana ƙara sakin carbon da aka adana a cikin yanayi a matsayin carbon dioxide.[3]
Gidajen da ke cikin tsaunuka na wurare masu zafi suna da dubban dabbobi da tsire-tsire, gami da nau'o'in da ba su da yawa kuma suna cikin haɗari kamar Orangutan da Sumatran tiger, waɗanda wuraren zama suna fuskantar barazanar lalacewar tsaunuka.[4]