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废弃高位沼泽泥炭挖掘地的植被恢复

Revegetation of peat excavations in a derelict raised bog.

作者信息

Jane Smart P, Wheeler B D, Willis A J

机构信息

Department of Animal and Plant Sciences, University of Sheffield, Sheffield S10 2TN, UK.

出版信息

New Phytol. 1989 Apr;111(4):733-748. doi: 10.1111/j.1469-8137.1989.tb02369.x.

Abstract

Thorne Waste, S. Yorkshire, is a large raised bog, subject to extensive commercial peat extraction, which retains some re-flooded, revegetated peat cuttings. The composition of the vegetation of some of these cuttings (96 sampled quadrats, each of 25 m ) has been related to a number of environmental variables. Revegetation sequences in the abandoned cuttings (all less than 60 years old and with less than 20 cm peat infill) were established by stratigraphical analyses. In some cuttings a basal layer of ericaceous peat apparently marks temporarily drier conditions preceding deeper inundation. Some former mire species (e.g. Sphagnum imbricatum have not survived the peat-cutting period even on uncut surfaces (baulks) but these have been much drained and burnt. The revegetated cuttings contained species typical of poor-ten (e.g. Carex curta) as well as of ombrotrophic mires (e.g. Andromeda polifolia); chemical analyses indicated weakly minerotrophic peat water. This may favour such species as Sphagnum recurvum. There was no indication of chemical enrichment from inflow from surrounding farmland, from underlying mineral ground or from the clay-lined canals excavated across the bog. Release of cations following drainage and re-flooding may provide some explanation. Only soluble reactive phosphorus (SRP) concentration in peat water samples showed consistent and significant seasonal variation, with the lowest values in summer. There were also only a few consistent differences in water chemistry amongst most of the vegetation units identified by TWINSPAN. Nodum 4 (Eriophorum-Sphagnum) stands (richest in ombrotrophic species) occupied the least minerotrophic conditions. One culling, dominated by Juncus, effuses, had no ombrotrophic species (nodum 6). Water concentrations of Ca , Na , K NH , SO and SRP were significantly larger here than in other cuttings and peat fertility (estimated phytometrically) and K, N and P concentrations in peat extracts were significantly greater than in a Sphagnum-dominated cutting. The J. effuses samples had strong negative loadings on axis 2 of a Principal Components Analysis (PCA) of the Adriatic data; concentrations of NH , Na and SO in the water showed significant negative correlation with axis 2 ordination scores. Seasonal fluctuation of water level was similar in most cuttings (the J. effuses cutting was exceptional) but variation in depth relative to the peat surface (caused by excavation to different depths) was related to floristic variation. PCA axis 1 may reflect a water-table gradient with TWINSPAN noda 2 (Calluna Sphagnum recurvum) and particularly 1 (Pteridium Campylopus) occupying drier conditions than the others. The wetter cuttings (except the J. effusus site) supported most ombrotrophic and poor-fen species. They were not readily segregated into discrete vegetation types and the two TWINSPAN classes (noda 3 and 4) that accommodated them showed much overlap on the PCA ordination. Nodum 4 samples tended to have higher loadings on PCA axis 2 and to be more species-rich than nodum 3 samples. Species-richness was strongly positively correlated with PCA axis 2. This may reflect, in part, stand maturity, vegetation with most species having been disturbed least recently.

摘要

南约克郡的索恩荒原是一片大型高位沼泽,遭受着大规模的商业泥炭开采,不过仍保留了一些重新被水淹没、重新植被化的泥炭采掘地。其中一些采掘地(96个采样样方,每个样方25平方米)的植被组成与许多环境变量相关。通过地层分析确定了废弃采掘地(均小于60年且泥炭填充层小于20厘米)的植被恢复序列。在一些采掘地中,一层石南科泥炭的底层显然标志着在更深的水淹之前暂时较干燥的状况。一些以前的泥炭沼泽物种(如泥炭藓)即使在未开采的表面(泥炭埂)也未能在泥炭开采期存活下来,不过这些地方已大量排水并遭焚烧。植被恢复的采掘地包含贫养泥炭地典型的物种(如短叶苔草)以及雨养泥炭沼泽典型的物种(如小叶仙女木);化学分析表明泥炭水呈弱矿质营养型。这可能有利于诸如曲泥炭藓等物种。没有迹象表明来自周围农田、下层矿质土地或穿过沼泽挖掘的黏土衬砌运河的水流会导致化学物质富集。排水和重新水淹后阳离子的释放可能提供了一些解释。只有泥炭水样中的可溶性活性磷(SRP)浓度呈现出一致且显著的季节性变化,夏季值最低。在TWINSPAN识别出的大多数植被单元中,水化学方面也只有少数一致的差异。节点4(羊胡子草 - 泥炭藓)群落(雨养物种最丰富)所处的矿质营养条件最差。一个以灯心草为主的采掘地没有雨养物种(节点6)。这里的水中钙、钠、钾、铵、硫酸根和SRP的浓度明显高于其他采掘地,泥炭肥力(通过植物测量法估算)以及泥炭提取物中的钾、氮和磷浓度明显高于以泥炭藓为主的采掘地。灯心草样本在亚得里亚海数据的主成分分析(PCA)的第2轴上有很强的负载荷;水中铵、钠和硫酸根的浓度与第2轴排序得分呈显著负相关。大多数采掘地的水位季节性波动相似(灯心草采掘地除外),但相对于泥炭表面的深度变化(由挖掘到不同深度引起)与植物区系变化相关。PCA第1轴可能反映了地下水位梯度,TWINSPAN节点2(石楠 - 曲泥炭藓)群落,特别是节点1(蕨 - 弯叶曲柄藓)群落比其他群落占据更干燥的条件。较湿润的采掘地(灯心草生长地除外)支持了大多数雨养和贫养泥炭地物种。它们不容易被划分为离散的植被类型,容纳它们的两个TWINSPAN类别(节点3和4)在PCA排序上有很大重叠。节点4的样本在PCA第2轴上往往有更高的载荷,且物种比节点3的样本更丰富。物种丰富度与PCA第2轴呈强烈正相关。这可能部分反映了群落成熟度,物种最多的植被最近受到的干扰最少。

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