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1.
秦岭细鳞鲑栖息地环境特征研究   总被引:3,自引:0,他引:3  
为研究秦岭细鳞鲑(Brachymystax lenok tsinlingensis)的栖息地环境选择偏好,对陕西陇县秦岭细鳞鲑国家级自然保护区和甘肃秦州珍稀水生野生动物国家级自然保护区内25个样点进行了鱼类采样和生境测量。共采集到130尾秦岭细鳞鲑样本,样点的平均分布密度为(0.10±0.07)尾/m,两个保护区内秦岭细鳞鲑的密度存在显著性差异(P < 0.05)。与秦岭细鳞鲑密度分布呈正相关的因子依次为坡度、跌水区密度、海拔、粗糙度、遮蔽度、底栖动物生物量和流速,与密度呈负相关的环境因子依次为河宽、水深和溶氧。冗余性分析(RDA)筛选了坡度、粗糙度、遮蔽度、海拔和跌水区5个关键环境因子。基于关键环境因子的实测值建立了栖息地适合度曲线,秦岭细鳞鲑分布的最适坡度范围为5%-10%,海拔分布范围为1500-2000 m,粗糙度范围0.3-0.4;跌水区密度范围12-18个/100 m,遮蔽度在0.5以上。  相似文献   
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In the context of ongoing climatic warming, certain landscapes could be near a tipping point where relatively small changes to their fire regimes or their postfire forest recovery dynamics could bring about extensive forest loss, with associated effects on biodiversity and carbon‐cycle feedbacks to climate change. Such concerns are particularly valid in the Klamath Region of northern California and southwestern Oregon, where severe fire initially converts montane conifer forests to systems dominated by broadleaf trees and shrubs. Conifers eventually overtop the competing vegetation, but until they do, these systems could be perpetuated by a cycle of reburning. To assess the vulnerability of conifer forests to increased fire activity and altered forest recovery dynamics in a warmer, drier climate, we characterized vegetation dynamics following severe fire in nine fire years over the last three decades across the climatic aridity gradient of montane conifer forests. Postfire conifer recruitment was limited to a narrow window, with 89% of recruitment in the first 4 years, and height growth tended to decrease as the lag between the fire year and the recruitment year increased. Growth reductions at longer lags were more pronounced at drier sites, where conifers comprised a smaller portion of live woody biomass. An interaction between seed‐source availability and climatic aridity drove substantial variation in the density of regenerating conifers. With increasing climatic water deficit, higher propagule pressure (i.e., smaller patch sizes for high‐severity fire) was needed to support a given conifer seedling density, which implies that projected future increases in aridity could limit postfire regeneration across a growing portion of the landscape. Under a more severe prospective warming scenario, by the end of the century more than half of the area currently capable of supporting montane conifer forest could become subject to minimal conifer regeneration in even moderate‐sized (10s of ha) high‐severity patches.  相似文献   
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高寒草甸植被下的草毡表层能够发挥水土保持、水源涵养等生态环境效益,是高寒草甸植被生态功能发挥的核心,认识草毡表层发育程度的空间分异及环境影响因子有利于深入理解高寒草甸在高原生态系统中的作用。本研究以祁连山中段高寒草甸分布区为研究区,依据根系体积并结合草毡层厚度以及土壤容重,将草毡表层划分为弱发育、中等发育以及强发育草毡。分析了不同发育程度草毡的地形、植被、气候等环境特征,并采用支持向量机模型对其分布进行了空间制图。结果表明:祁连山中段发育程度较高的草毡表层趋向于分布在水分条件较好的低海拔、缓坡,低坡位以及北向坡的位置,以嵩草属植物为主,中等以上发育程度的草毡地表植被及水分条件都较好;发育程度较高的草毡表层年均温较高,各发育程度草毡表层降水量差异不显著。空间分布结果整体与现有的高寒草甸植被类型分布具有高度的一致性,但空间分辨率更为详细,并且实现了不同发育程度草毡表层的空间细分。  相似文献   
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Each year severe winter storms (≈ice storms) damage trees throughout the southern USA. Arkansas and Oklahoma have a history of severe winter storms. To extend that history back beyond the reach of written records, a distinctive tree ring pattern or signature is needed. Storm-caused breakage, branch loss and bending stress provide that signature. We found a severe storm signature in shortleaf pine (Pinus echinata). We used three published site chronologies, a set of five new site chronologies from a growth-and-yield study conducted by Oklahoma State University and the unpublished Shortleaf Canyon chronology from a master’s thesis at the University of Arkansas. Our method is based on two ring width values for the first and second growing seasons after the storm standardized to the ring widths of the seven growing seasons after the storm. Concordance between storm years predicted by tree ring patterns and actual storm years was tested using Cohen’s Kappa. Concern about confounding of ice storm signals by droughts led us to test concordance between severe storms and drought in July, August and September; results were inconclusive but stand as a warning that these two phenomena cannot be distinguished with certainty in the tree ring record. Damaging severe storms occurred in about 2.8% of all years. Two out of three storms identified as “severe” produced glaze icing.  相似文献   
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Climatic harshness is expected to increase at higher elevations; however, elevational trends of tree radial growth response of high-elevation forests to climate change need to be investigated at different locations because of existing local variability in site-specific climatic conditions. We developed tree-ring width chronologies of Yunnan fir (Abies georgei) along elevation gradients at two sites in the central Hengduan Mountains (HM). High-elevation forests of A. georgei showed growth synchronicity and common growth signals along elevation gradients, indicating a common climatic forcing, although tree radial growth rates decreased with increasing elevation. Radial growth of Yunnan fir showed positive correlations with summer temperatures and February precipitation and moisture availability, but were negatively correlated with spring temperatures. The strongest positive relationship indicated summer (July) mean and minimum temperatures are the most important growth determining climatic factors for tree radial growth in the cold environment of HM, and this relationship revealed a clear elevational trend with stronger correlations at higher altitudes. In contrast, tree radial growth was negatively correlated with June precipitation and moisture availability. The whole study period 1954–2015 was split in two sub-periods of equal length. Comparing the early sub-period (1954–1984) to the later sub-period (1985–2015), tree growth response to the summer temperatures strongly increased, while it became weaker to June precipitation and moisture availability. High-elevation Yunnan fir forests in the HM currently benefit from elevated growing season temperatures under humid summer conditions. However, increasing temperatures may induce drought stress on tree radial growth if the observed decreasing trend in humidity and precipitation continues.  相似文献   
7.
祁连山典型流域谷地植被斑块演变与土壤性状   总被引:2,自引:0,他引:2  
植物群落演变与土壤性状变化之间的相互作用和过程研究对于认识生态系统结构和功能演变有着重要的意义.对祁连山谷地灌丛草甸退化演变过程中植物群落物种组成、土壤物理和化学性状特征、及土壤与植被的相互作用进行了研究,结果表明,在祁连山谷地阴坡林线以下较小的空间范围,植被斑块由金露梅群落向金露梅-马蔺群落斑块和马蔺群落斑块演变,植被盖度降低,但物种多样性增加.不同植被斑块之间土壤水分有显著的梯度变化,土壤水分的变化导致植被的退化演替.植被斑块的演变导致土壤性状的明显分异,从金露梅灌丛斑块向金露梅-马蔺群落斑块和马蔺群落斑块演变,土壤容重显著增加,土壤团聚体组成由大粒级的大团聚体(》1mm)破碎为小粒级的大团聚体(1-0.25mm)和微团聚体(《0.25mm),团聚体稳定性降低,表明土壤结构的退化;土壤有机碳含量下降了31.2%和55.9%,干筛各粒级土壤团聚体中有机碳含量金露梅-马蔺群落斑块和马蔺群落斑块显著低于金露梅斑块,土壤团聚体平均重量粒径与有机碳含量存在显著相关,植被退化演变中土壤有机碳的损失部分地由于团聚体的破碎引起;土壤全氮和有效氮不同斑块之间也有显著的差异,植被斑块退化演变使氮的有效性降低;但磷、钾养分对植被变化的响应不敏感.植被的退化演变使土壤团聚体破碎、土壤结构退化,有机碳和全氮含量下降,使其抗侵蚀能力和水源涵养功能显著降低,又进一步加速植被的退化演替.在气候变暖的趋势下,马蔺斑块将进一步向林线逼近,灌丛草甸植被将会进一步退化和萎缩.  相似文献   
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Agricultural conversion of tropical forests is a major driver of biodiversity loss. Slowing rates of deforestation is a conservation priority, but it is also useful to consider how species diversity is retained across the agricultural matrix. Here, we assess how bird diversity varies in relation to land use in the Taita Hills, Kenya. We used point counts to survey birds along a land‐use gradient that included primary forest, secondary vegetation, agroforest, timber plantation and cropland. We found that the agricultural matrix supports an abundant and diverse bird community with high levels of species turnover, but that forest specialists are confined predominantly to primary forest, with the matrix dominated by forest visitors. Ordination analyses showed that representation of forest specialists decreases with distance from primary forest. With the exception of forest generalists, bird abundance and diversity are lowest in timber plantations. Contrary to expectation, we found feeding guilds at similar abundances in all land‐use types. We conclude that whilst the agricultural matrix, and agroforest in particular, makes a strong contribution to observed bird diversity at the landscape scale, intact primary forest is essential for maintaining this diversity, especially amongst species of conservation concern.  相似文献   
10.
四川邛崃山系小熊猫分布   总被引:1,自引:0,他引:1  
2000-2002年,对四川邛崃山系11个县(市)的小熊猫分布状况进行了调查.共完成调杏样线2332条,发现有小熊猫痕迹样线130条,分布在9个县,样线平均遇见率为5.57%,样线遇见率最高的是汶川县和崇州市;估算整个山系有小熊猫栖息地面积5107.82km2,以宝兴、汶川和天全3县的面积最大,分别占总面积的34.08%、30.65%和16.61%,这3个县占总面积的81.34%;小熊猫分布密度等级最高的区域是崇州市的四川鞍子河自然保护区.在山系内7个自然保护区中有小熊猫栖息地面积2166.84km2,占栖息地总面积的42.4%.小熊猫空间分布格局极不连续,存在许多空白区域,栖息地存在破碎化趋势,应进一步加强对邛崃山世界遗产地内小熊猫种群的保护.  相似文献   
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