The seasonality of macroinvertebrate β diversity along the gradient of hydrological connectivity in a dynamic river-floodplain system

Anthropogenic disturbance to natural hydrological connectivity, both longitudinal, lateral, and vertical, is threatening the ecological integrity of the freshwater realm. River-floodplain system is particularly adversely affected by the reduction in lateral hydrological connectivity (LHC), represent...

Descripción completa

Guardado en:
Detalles Bibliográficos
Autores principales: Rui Dong, Yuyu Wang, Cai Lu, Guangchun Lei, Li Wen
Formato: article
Lenguaje:EN
Publicado: Elsevier 2021
Materias:
Acceso en línea:https://doaj.org/article/206ba67eac804f45b932b1aaf8b49c88
Etiquetas: Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
id oai:doaj.org-article:206ba67eac804f45b932b1aaf8b49c88
record_format dspace
spelling oai:doaj.org-article:206ba67eac804f45b932b1aaf8b49c882021-12-01T04:35:27ZThe seasonality of macroinvertebrate β diversity along the gradient of hydrological connectivity in a dynamic river-floodplain system1470-160X10.1016/j.ecolind.2020.107112https://doaj.org/article/206ba67eac804f45b932b1aaf8b49c882021-02-01T00:00:00Zhttp://www.sciencedirect.com/science/article/pii/S1470160X20310517https://doaj.org/toc/1470-160XAnthropogenic disturbance to natural hydrological connectivity, both longitudinal, lateral, and vertical, is threatening the ecological integrity of the freshwater realm. River-floodplain system is particularly adversely affected by the reduction in lateral hydrological connectivity (LHC), representing one of major biodiversity hotspots under increasingly pressure. Many studies have demonstrated that LHC has great influence on the spatial variations of flora and fauna communities (i.e. spatial β diversity) through facilitating dispersal. However, to fully understand the impact of anthropogenic disturbances on biodiversity, we must also understand how ecological communities change over time (i.e. temporal β diversity, TBI) and the underlying processes. To evaluate the processes structuring ecological communities, we examined the macroinvertebrate TBI in habitats along the gradient of LHC for an entire hydrological cycle in West Dongting Lake, a Ramsar-listed floodplain wetland at the middle reach of Yangtze River. Our results showed that the total spatial β diversity fluctuated with water level and peaked at high-water phase, and LHC was the driving forcing affecting both species richness and abundance in all hydrological periods. In particular, species richness and abundance were highest in habitats with medium LHC levels for water-rising and high-water periods reflecting the intermediate disturbance hypothesis except for water-recessing, during which there was no clear pattern. While replacement determined β diversity in most sites at water-rising and high-water phases, the contribution of nestedness were high during water-withdrawing phase. From water-rising to high-water, macroinvertebrates from other habitats spread to the modified mudflats, which had the lowest LHC, along with the floods. During water-withdrawing period, β diversity and its turnover component of all habitats were low compared with other hydrological phases. Temporal β diversity analysis illustrated that the species dispersal was the main mechanism underlying the temporal and spatial variations in the observed community patterns. These findings demonstrated that hydrological connectivity was critical to maintaining the ecological integrity of river-floodplain ecosystems.Rui DongYuyu WangCai LuGuangchun LeiLi WenElsevierarticleHydrological connectivityNestednessTurnoverDispersal abilityB-C plotsEcologyQH540-549.5ENEcological Indicators, Vol 121, Iss , Pp 107112- (2021)
institution DOAJ
collection DOAJ
language EN
topic Hydrological connectivity
Nestedness
Turnover
Dispersal ability
B-C plots
Ecology
QH540-549.5
spellingShingle Hydrological connectivity
Nestedness
Turnover
Dispersal ability
B-C plots
Ecology
QH540-549.5
Rui Dong
Yuyu Wang
Cai Lu
Guangchun Lei
Li Wen
The seasonality of macroinvertebrate β diversity along the gradient of hydrological connectivity in a dynamic river-floodplain system
description Anthropogenic disturbance to natural hydrological connectivity, both longitudinal, lateral, and vertical, is threatening the ecological integrity of the freshwater realm. River-floodplain system is particularly adversely affected by the reduction in lateral hydrological connectivity (LHC), representing one of major biodiversity hotspots under increasingly pressure. Many studies have demonstrated that LHC has great influence on the spatial variations of flora and fauna communities (i.e. spatial β diversity) through facilitating dispersal. However, to fully understand the impact of anthropogenic disturbances on biodiversity, we must also understand how ecological communities change over time (i.e. temporal β diversity, TBI) and the underlying processes. To evaluate the processes structuring ecological communities, we examined the macroinvertebrate TBI in habitats along the gradient of LHC for an entire hydrological cycle in West Dongting Lake, a Ramsar-listed floodplain wetland at the middle reach of Yangtze River. Our results showed that the total spatial β diversity fluctuated with water level and peaked at high-water phase, and LHC was the driving forcing affecting both species richness and abundance in all hydrological periods. In particular, species richness and abundance were highest in habitats with medium LHC levels for water-rising and high-water periods reflecting the intermediate disturbance hypothesis except for water-recessing, during which there was no clear pattern. While replacement determined β diversity in most sites at water-rising and high-water phases, the contribution of nestedness were high during water-withdrawing phase. From water-rising to high-water, macroinvertebrates from other habitats spread to the modified mudflats, which had the lowest LHC, along with the floods. During water-withdrawing period, β diversity and its turnover component of all habitats were low compared with other hydrological phases. Temporal β diversity analysis illustrated that the species dispersal was the main mechanism underlying the temporal and spatial variations in the observed community patterns. These findings demonstrated that hydrological connectivity was critical to maintaining the ecological integrity of river-floodplain ecosystems.
format article
author Rui Dong
Yuyu Wang
Cai Lu
Guangchun Lei
Li Wen
author_facet Rui Dong
Yuyu Wang
Cai Lu
Guangchun Lei
Li Wen
author_sort Rui Dong
title The seasonality of macroinvertebrate β diversity along the gradient of hydrological connectivity in a dynamic river-floodplain system
title_short The seasonality of macroinvertebrate β diversity along the gradient of hydrological connectivity in a dynamic river-floodplain system
title_full The seasonality of macroinvertebrate β diversity along the gradient of hydrological connectivity in a dynamic river-floodplain system
title_fullStr The seasonality of macroinvertebrate β diversity along the gradient of hydrological connectivity in a dynamic river-floodplain system
title_full_unstemmed The seasonality of macroinvertebrate β diversity along the gradient of hydrological connectivity in a dynamic river-floodplain system
title_sort seasonality of macroinvertebrate β diversity along the gradient of hydrological connectivity in a dynamic river-floodplain system
publisher Elsevier
publishDate 2021
url https://doaj.org/article/206ba67eac804f45b932b1aaf8b49c88
work_keys_str_mv AT ruidong theseasonalityofmacroinvertebratebdiversityalongthegradientofhydrologicalconnectivityinadynamicriverfloodplainsystem
AT yuyuwang theseasonalityofmacroinvertebratebdiversityalongthegradientofhydrologicalconnectivityinadynamicriverfloodplainsystem
AT cailu theseasonalityofmacroinvertebratebdiversityalongthegradientofhydrologicalconnectivityinadynamicriverfloodplainsystem
AT guangchunlei theseasonalityofmacroinvertebratebdiversityalongthegradientofhydrologicalconnectivityinadynamicriverfloodplainsystem
AT liwen theseasonalityofmacroinvertebratebdiversityalongthegradientofhydrologicalconnectivityinadynamicriverfloodplainsystem
AT ruidong seasonalityofmacroinvertebratebdiversityalongthegradientofhydrologicalconnectivityinadynamicriverfloodplainsystem
AT yuyuwang seasonalityofmacroinvertebratebdiversityalongthegradientofhydrologicalconnectivityinadynamicriverfloodplainsystem
AT cailu seasonalityofmacroinvertebratebdiversityalongthegradientofhydrologicalconnectivityinadynamicriverfloodplainsystem
AT guangchunlei seasonalityofmacroinvertebratebdiversityalongthegradientofhydrologicalconnectivityinadynamicriverfloodplainsystem
AT liwen seasonalityofmacroinvertebratebdiversityalongthegradientofhydrologicalconnectivityinadynamicriverfloodplainsystem
_version_ 1718405829947817984