Floodplain succession pattern along Budhi-Rapti River bank, Chitwan, Nepal

Dhiraj Chhetri Kunwar, C. Baniya
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Abstract

 Riverine floodplain is one of the most productive lowland ecosystems in Nepal. However, floodplain ecology is less understood due to its fluctuation. Budhi-Rapti River in Chitwan, central Nepal formed a floodplain along the Khorsor zone of Barandabhar corridor. This study was carried out to understand the floodplain ecosystem development after plant succession. The space for time substitution method of vegetation sampling was adopted in order to sample the floodplain created at different chronosequence. The floodplain that lies perpendicular to and 200 m away from the Budhi-Rapti river was sampled. Systematic sampling was done along two parallel transects, almost 200 m apart from each other. Sampling along the transect started right after 200 m away from the Budhi-River bank. Initial position of these transects towards Budhi-Rapti river was believed to be the youngest floodplain, which slowly getting older after passing away from the river. Abundance of vascular plant species was recorded in sample plots of 20 × 20 m each subdivided equally into 4 subplots (each of 100 m2). Along each transect, vegetation data was recorded from a series of 20 plots, placed 50 m apart from each other. Successional scores were calculated and utilized as environmental variables after applying non-metric multi-dimensional scaling (NMDS) through metaMDS. Total and life form (herbs, shrubs and trees) richness patterns were calculated. Altogether, 158 species of vascular plants under 60 families and 136 genera were recorded. Gramineae was the richest family followed by Leguminosae, Asteraceae and Cyperaceae. Total species richness showed significant negative correlation with the NMDS1 and NMDS2, which justified a convergent pattern of succession. Herb, orchid and shrub species richness also showed significant declining pattern with NMDS1. Persicaria barbata, Parthenium hysterophorus, Ageratum conyzoides and Typha angustifolia were early succession indicator species; whereas Albizia lucidior, Miliusa velutina, Ficus hispida, Bauhinia purpurea and Brassaiopsis glomerulata were the late succession tree species. This study agreed with the convergent model of succession.Botanica Orientalis – Journal of Plant Science (2017) 11: 12–26
尼泊尔奇旺Budhi-Rapti河岸洪泛区演替格局
河流泛滥平原是尼泊尔最多产的低地生态系统之一。然而,由于其波动性,人们对河漫滩生态学的了解较少。尼泊尔中部Chitwan的Budhi-Rapti河沿着Barandabhar走廊的Khorsor区形成了一个洪泛区。本研究旨在了解植物演替后河漫滩生态系统的发展情况。为了对不同时间序列形成的河漫滩进行采样,采用了植被采样的空间代替时间法。在与布达拉普蒂河垂直且距离布达拉普蒂河200米的漫滩上取样。系统采样沿着两条平行的横断面进行,彼此相距近200米。沿着样带的采样开始于距布达河岸200米的地方。这些面向Budhi-Rapti河的横断面的初始位置被认为是最年轻的洪泛区,在离开河流后慢慢变老。样地面积为20 × 20 m,每个样地平均划分为4个样地(每个样地面积为100 m2),记录维管植物种类丰度。沿着每个样带,记录了一系列20个样地的植被数据,这些样地彼此间隔50米。通过metaMDS应用非度量多维尺度(NMDS)计算连续得分,并将其作为环境变量。计算了植物、灌木和乔木的总丰富度格局和生活型丰富度格局。共记录到维管植物60科136属158种。最丰富的科是禾本科,其次是豆科、菊科和苏科。总物种丰富度与NMDS1和NMDS2呈显著负相关,表明群落演替呈收敛模式。草本、兰花和灌木物种丰富度也随NMDS1的变化呈显著下降趋势。巴贝桃、虎耳草、鹰嘴舌草和麻叶霉是早期演替指示种;而绿豆、柳杉、无花果、紫荆和芸苔则是晚演替树种。研究结果与演替趋同模型一致。植物学报(2017)11:12-26
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