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The forests of Nothofagus pumilio have historically been affected by forest fires. The effects of fire on certain above and belowground, biotic and abiotic components of these ecosystems have been previously documented, albeit belowground components have received much less attention. It has been suggested that the effects observed in the short-term after a fire usually differ from the longer-term effects. The long-term effects of fire (i.e. >5 years after burning) on belowground components in Nothofagus forests are currently unknown. In the present study we evaluated the long-term effect of fire on ectomycorrhiza (ECM) colonization and morphotype composition in N. pumilio roots, as well as soil chemical properties in temperate forests in Patagonia. Sampling was conducted in three mature monospecific forests. In each, nearby burned and unburned sites were selected. The time since the occurrence of fires differed between areas (i.e. 6-10 years). Within each site, 3 transects of 40 m were established randomly along which 5 samples of roots and soil were collected in spring and autumn. The main results were: (1) in comparison with the unburned site, ECM colonization was lower in the burned site in the area with the shorter time length since fire occurrence and no effects in the other two areas were observed; (2) richness and diversity were not significantly affected by fire but there was a significant effect of season for both parameters, being higher in spring; (3) ECM dominance was significantly higher in the unburned than in the burned site in Tronador, while in Challhuaco the opposite was observed, mainly in autumn; (4) in general carbon, nitrogen and phosphorous decreased while pH increased in the burned sites; (5) ECM colonization positively correlated with NH4+ and phosphorus and negatively with pH but was not significantly correlated with organic matter or any other soil variable. Altogether the results suggest that effects of fire on ectomycorrhiza and soil properties in N. pumilio forests are probably related to the time elapsed since fire occurrence combined with site characteristics. In addition, the direct and indirect effects of fire in these forest systems may persist for more than 10 years.  相似文献   
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本文论述了孟加拉国吉大港大学校园里,不同年龄(5、10、20年)的羯布罗香(Dipterocarpus turbinatus Gaertn. F)人工林内,距树木基部不同距离(1、2、3、4米)处,外生侵染菌根的水平分布状况.在山的3个部位(顶部、中部和下部)对各人工林外生侵染菌根的侵染进行了测定.在不同水平分布距离处的树下采集了1000cm3的根际土壤样本,不同距离和山高处的外生侵染菌根浸染率差异显著.在5年和10年林龄的人工林内,浸染率随着距树的距离的增加而快速下降,而在20年林龄的人工林内,浸染率随着距树基部距离的增加而急剧增加.山下部20年生人工林内距树4m处的浸染率最高(81.3%),山顶部5年生人工林内距树4m处的浸染率最低(55.33%).图6参32.  相似文献   
3.
文章根据国内外的菌根文献资料,综述了外生菌根形成对宿主树木的影响.外生菌根对宿主树木的主要作用包括:外生菌根能扩大树木根系的吸收面积和吸收范围,增强宿主树木对营养元素的吸收和利用,菌根菌还能通过合成植物激素来调节共生双方,菌根还能提高宿主树木的抗病性和抗逆性.  相似文献   
4.
Ultramafic soils have naturally high concentrations of metals and are often low in major plant nutrients. Plant species of non-ultramafic origin, such as Dryobalanops lanceolata (Dipterocarpaceae), generally grow less well on these soils. I found minimal changes in growth, but a 17% reduction in foliar potassium, when seedlings of D. lanceolata were grown in a non-native ultramafic soil when compared with a ‘normal’ tropical ultisol. There were, however, marked changes in the ectomycorrhizal community structure on the roots of D. lanceolata. Cenococcum geophilum was at least 10 times more common and Inocybe sp. was one and a half times more common in non-ultramafic soils, whereas Boletales sp. was over 30 times more common in the non-ultramafic soil. These changes may have been brought about by a number of edaphic differences between the two soil types, including high metal concentrations and differences in organic matter content.  相似文献   
5.
本文论述了孟加拉国吉大港大学校园里,不同年龄(5、10、20年)的羯布罗香(DipterocarpusturbinatusGaertn.F)人工林内,距树木基部不同距离(1、2、3、4米)处,外生侵染菌根的水平分布状况。在山的3个部位(顶部、中部和下部)对各人工林外生侵染菌根的侵染进行了测定。在不同水平分布距离处的树下采集了1000cm3的根际土壤样本,不同距离和山高处的外生侵染菌根浸染率差异显著。在5年和10年林龄的人工林内,浸染率随着距树的距离的增加而快速下降,而在20年林龄的人工林内,浸染率随着距树基部距离的增加而急剧增加。山下部20年生人工林内距树4m处的浸染率最高(81.3%),山顶部5年生人工林内距树4m处的浸染率最低(55.33%)。  相似文献   
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