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Factors controlling vegetation structure in peatland lakes-Two conceptual models of plant zonation

机译:泥炭地湖泊植被结构控制因素-两种植物分区概念模型

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Two conceptual models of plant zonation in peatland lakes are given. The first represents vegetation on slightly sloping substrate (N<0.2) in shallow and relatively large lakes. The vegetation is not diverse (H' = 0.0+/-0.01). The frequency and biomass of the dominant (Sphagnum denticulatum) correlate positively with lake size, and negatively with depth and substrate slope. They are also correlated with water transparency and water color (r = -0.53), concentrations of total organic carbon (r = -0.43), Ca2+ (r = 0.40) and humic acids (r = -0.46), and redox potential (r = 0.44). The second model represents vegetation on steep peat walls (N>0.3) in deep, usually small lakes. Plants occur only on the upper part of the peat wall or form a multispecies curtain hanging from the lip of peat at the top. Species diversity in this scenario is higher (H' = 0.18+/-0.17). The curtains usually are composed of mosses such as Warnstorfia exannulata, S. cuspidatum and S. riparium, and vascular plants are rare. The frequency and biomass of bryophytes in this type of structure are related to substrate slope (r = 0.56), lake depth (r = 0.56), Ca2+ concentration (r = -0.69) and water color (r = -0.51). In both models, plant biomass is correlated with temperature (r = -0.78), irradiance (r = -0.64) and water oxygenation (r = -0.54). (C) 2011 Elsevier B.V. All rights reserved.
机译:给出了泥炭地湖泊植物区划的两个概念模型。第一个代表浅水和较大湖泊中略微倾斜的基底上的植被(N <0.2)。植被不多样化(H'= 0.0 +/- 0.01)。优势树(Sphagnum denticulatum)的频率和生物量与湖泊大小正相关,与深度和底物坡度负相关。它们还与水的透明度和水的颜色(r = -0.53),总有机碳的浓度(r = -0.43),Ca2 +(r = 0.40)和腐殖酸(r = -0.46)以及氧化还原电位(r = 0.44)。第二种模型代表了深湖(通常是小湖)中陡峭的泥炭墙上的植被(N> 0.3)。植物仅出现在泥炭壁的上部,或在顶部的泥炭唇上形成悬挂的多物种窗帘。在这种情况下,物种多样性更高(H'= 0.18 +/- 0.17)。窗帘通常是由苔藓组成的,例如花环线虫(Warnstorfia exannulata),虎杖(S. cuspidatum)和剑兰(S. riparium),而维管植物却很少。苔藓植物在这种结构中的频率和生物量与底物斜率(r = 0.56),湖泊深度(r = 0.56),Ca2 +浓度(r = -0.69)和水色(r = -0.51)有关。在这两个模型中,植物生物量都与温度(r = -0.78),辐照度(r = -0.64)和水的氧化(r = -0.54)相关。 (C)2011 Elsevier B.V.保留所有权利。

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