Monitoring and Conservation of tropical lakes, using trophic cascading interrelationship : analysis of aquatic communities with reference to climate changes.
2021 May
Dr. Asma Ali ( Ecologist)
Introduction :
Aquatic ecosystem functioning depends on multiple interactions between physical, chemical and biological determinants. Indeed, ecosystem processes (productivity and nutrient recycling) result directly from the diversity of functional traits in the biotic communities, which is in turn determined by the species composition and diversity (Kelly and Haves 2005, Zanden and Fetzer 2007, Adandedjan et al. 2010). This species diversity results from both biotic interaction and environmental pressures. As a result, changes in biodiversity in response to environmental selection , particularly in the event of drastically changing global climate scenario.
However large tropical man made water body, such as the Upper Lake of Bhopal, have not at all been subjected to a food web interrelationship analysis. Thus there is no information available on the comparative assessment of climate change scenarios based on aquatic food web modeling, resulting in a rapid eutrophication of this largest man made lake.
In an aquatic ecosystem, each species either invertebrate or vertebrate has the pressures that tend to have a direct impact on the ecosystem process. Thus these intricate relationships between aquatic biodiversity and ecosystem functioning have been the focus of numerous researches for several potential to perform an essential role in the persistence of the aquatic food web and the ecosystem and that species may remain as the sole representative of a particular functional group. At some level where each species is unique, overlapping in resource use among species is not unusual, especially in freshwater food webs.
Many benthic invertebrates are predators, that control numbers, locations and sizes of their prey. Benthic invertebrates supply food for both aquatic and terrestrial vertebrate consumers e.g. fishes, turtles and birds, finally benthic organism accelerate nutrient transferred to overlaying open waters of lakes as well as to adjacent riparian zones of streams (Abell et al., 2008, Heino et al. 2009, Matthews and Wickel 2009).
The extent of understanding the effect of aquatic fauna and flora in a freshwater ecosystem food web process varies with the type of fresh water system. Food chain length is a measure of the number of energy transfer or trophic link between primary producers and the top predators in an ecosystem also plays an important role in regulating biogeochemical fluxes, fisheries productivity and contaminant bioaccumulation in top predators of any water body.
Climate change is one of the most crucial and influential ecological problems of our age, therefore a large number of investigations is required to deal with this problem which is increasing permanently. Climatic changes and variability can influence aquatic ecosystems in a very sensitive way, so the research of the possible effects of climate change on aquatic ecosystems means an indispensable task.
Global warming and climate change which has caused the ecological systems, biodiversity and human life to control the biggest problem of history have started to show their impacts on all living beings in the aquatic ecosystem from plankton to mammals. Global surface temperature has increased on an average of 0.74 ± 0.18ºC between the start and the end of the 20th century (Abell et al. 2008, Matthews and Wickel 2009, Heino et al. 2009).
Since we do not have the chance to reverse the global warming and climate change phenomena, the only thing that needs to be done is to minimize the foreseen harms in the future. To this end, mankind needs to understand the global warming problem and cooperate on an international level using aquatic model studies of invertebrate and vertebrate species preferably in large tropical water bodies, which are on the brink of eutrophication and extinction. Upper Lake of Bhopal, the largest man made lake built by Raja Bhoj in 1100 is such an example. The present work will be a very important step towards its conservation.
Previous studies of Upper Lake have often dealt with the physico-chemical parameters for taxonomy of flora and fauna of the lake (Durrani 1993, Tiwari 1999), which are clearly important components of food webs, but how their functional relationships respond to changes in species composition are not known at all. Crores of rupees have been spent by Lake Authority Bhopal and other agencies on only physicochemical and limnological studies of the lake with no data available on cascading trophic interactions of invertebrate communities; except for the preliminary work of Parveen et al. (2009), Parveen and Ali (2010), which have shown interesting findings.
In the present research work, we will highlight examples of how some species have a disproportionately large impact on food-web dynamics, how particular species provide essential ecosystem services and how changing climate impacts aquatic biodiversity. These ecosystem functions include sediment mixing; nutrient cycling, cascade prey predator relationship and energy flow through food webs. The present investigation will prepare a working model of lake monitoring and conservation using aquatic food web cascading interrelationships in changing climate factors like temperature, humidity, rainfall and nutrients.
Aims and Objectives :
To determine primary productivity of the Lake with regard to rainfall, temperature, humidity and nutrient.
To determine the number of trophic levels in shoreline ecosystems.
To assess the role of insect fauna in water quality assessment programmes and their importance in aquatic food relationship in the Lake.
To investigate the role of macrophytes with regard to their trophic status for management and conservation of the Lake.
To group the various fish species according to their feeding preferences, for assessing functioning of cascade trophic prey-predator relationship.
To investigate the trophic importance of plankton (phytoplankton and zooplankton) in relation to species richness and pelagic aquatic ecosystem and to focus on the role of benthic invertebrate species in freshwater ecosystem.
Comparative assessment of the alternative climate change scenarios using statistical methods.
Brief Review Of the work done in the field :
Food chain length is a measure of the number of energy transfer or trophic links between primary producers and top predators in an ecosystem, and the importance of food chain for ecosystems and their functioning have been widely documented. For example, the number of trophic levels in a central consideration to the study of the food chain dynamics (Fretwell 1987) and the structuring of the ecosystem via trophic cascades (Kelly and haves 2005, Zanden and Fetzer 2007) as well as mediating the relationship between species diversity and function (Worn 2002, Schmitz 2003, Duffy 2005). Food chain also plays a role in regulating biochemical fluxes, fisheries productivity (Pauly and Christensen 1995) and contaminant bioaccumulation in top predators (Kidd 1995, Winmiller and Layman 2005).
The earliest consideration of the food chain, Elton (1927) speculated that available energy ultimately limits the numbers of trophic levels in ecosystems. A clear prediction is that more productive should have longer food chains. This “productivity hypothesis” has found support in some studies (Kaunzinger and Morin 1998, Thompson and Townsend 2005, Kundzewicz et al., 2008), but not others (Briand and Cohen 1987). Since then, variants of the productivity hypothesis have been forwarded, most notably the productive space hypothesis, which argues that total ecosystem production should best reflect the capacity of an ecosystem to support additional trophic levels and the hypothesis that food chain length should increase with increasing ecosystem size (Post et al. 2000).
In case of aquatic ecosystems the astonishing species richness in phytoplankton communities has stimulated many studies of the importance of competition for light and /or nutrients, or of the intermediate disturbance hypothesis have been reported by several workers such as Elliott et al. (2002) and Schippers et al., (2001). Similarly in case of zooplankton many views have been stressed by several investigators such as Leveque (1997) and Matondo and Msibi (2006), who showed relationship between zooplankton and physico-chemical features of a water body, while Ward (1998) stated that there is no obvious relationship between zooplankton and dissolved nutrients.
In freshwater sediments, benthic invertebrates are diverse and abundant and the integrity of the freshwater supply depends on how various benthic species make their living and contribute to the complex food web.
Furthermore, there are many papers that deal more specifically with the mechanisms involved in the relationships between biodiversity of water bodies and ecosystem functioning. Notably have Yule (1996), Loreau (1998) and Conway (2005). Using a freshwater microbial community Fukami and Morin (2003) found that food web relationships in the different assemblage of species took various forms (U-shaped, hump-shaped) after 30 generations.
Concerning aquatic ecosystems more particularly Dobson et al. (2000) found in their study based on a survey of 33 lakes that for both phytoplankton and fish, the richness-productivity relationship was highly dependent on the area of the lake.
Climate change has and will continue to affect freshwater ecosystems in a variety of ways (Fukamy and Marin 2003, Heino et al.,2009). When flow regimes shift, quantitative and qualitative changes to aquatic habitat result, indirectly influencing ecosystem productivity and biodiversity. Freshwater systems are expected to experience an increase in the frequency and intensity of extreme events, such as droughts and floods ;freshwater species adapted to different, historic flow regimes might be unable to complete their life histories under these conditions.
Climate change-induced air temperature shifts are already altering water temperature and attendant biogeochemical processes, and changes in lake volume and thermal structure are expected (Lake et al. 2000; Mohseni et al. 2003). Coastal wetlands and the lower reaches of most rivers in many regions have been affected by sea-level rise for over a century (Bates et al. 2008).
However there are very few studies on trophic relationships of water bodies and ecosystem functioning, some of these studies which have contributed to the significant advances of our knowledge on this subject in the last ten years and have provided a good overview of the challenges likely to face us in the future.
With this goal in mind, new experiments based on trophic relationships and the food web must be performed at aquatic ecosystems of tropical water bodies, which have variant cycles of trophic interactions due to a large number of environmental factors. Thus in the view of above lacunae, the present study has been taken, where a detailed study of tropical lakes using cascading interrelationship analysis of aquatic communities with reference to climate change.
Aquatic macrophytes are an important component of many watercourses, providing a structure and habitat for fish and invertebrates, offering protection against currents and predators, and forming a substrate for the deposition of eggs. As primary producers, macrophytes represent an important food resource, and they also play a significant role in the oxygen balance and nutrient cycle of many watercourses.
In view of their varying requirements, the composition of macrophyte species in a water body makes it possible to draw conclusions about the local chemical and physical conditions. Species that prefer low nutrient concentrations, in particular, have become much less prevalent. Also in decline are species that are dependent on natural riverbanks with sandy and gravelly substrates.
Aquatic plants are especially sensitive to changes (increases) in nutrient concentrations (notably phosphorus and ammonium) and to organic pollutants. Samples of shoreline macrophytes will be collected from different types of habitat like lake margin and shallow water zones of study area, and will be identified with the help of guidelines given by Haslam (1978) and Britto (1991).
One of the key challenges facing freshwater ecologists is to develop a suite of tools for detecting the impacts of climate change in complex natural systems that can be applied across multiple spatio-temporal scales and levels of organization.
We will also need to integrate long-term, empirical survey data with models and manipulative experiments if we are to develop a truly mechanistic, and hence predictive, understanding of responses to future change.
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