Introduction to Freshwater Ecology
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Freshwater Ecosystems and Biodiversity
Network of Conservation Educators & Practitioners Freshwater Ecosystems and Biodiversity Author(s): Nathaniel P. Hitt, Lisa K. Bonneau, Kunjuraman V. Jayachandran, and Michael P. Marchetti Source: Lessons in Conservation, Vol. 5, pp. 5-16 Published by: Network of Conservation Educators and Practitioners, Center for Biodiversity and Conservation, American Museum of Natural History Stable URL: ncep.amnh.org/linc/ This article is featured in Lessons in Conservation, the official journal of the Network of Conservation Educators and Practitioners (NCEP). NCEP is a collaborative project of the American Museum of Natural History’s Center for Biodiversity and Conservation (CBC) and a number of institutions and individuals around the world. Lessons in Conservation is designed to introduce NCEP teaching and learning resources (or “modules”) to a broad audience. NCEP modules are designed for undergraduate and professional level education. These modules—and many more on a variety of conservation topics—are available for free download at our website, ncep.amnh.org. To learn more about NCEP, visit our website: ncep.amnh.org. All reproduction or distribution must provide full citation of the original work and provide a copyright notice as follows: “Copyright 2015, by the authors of the material and the Center for Biodiversity and Conservation of the American Museum of Natural History. All rights reserved.” Illustrations obtained from the American Museum of Natural History’s library: images.library.amnh.org/digital/ SYNTHESIS 5 Freshwater Ecosystems and Biodiversity Nathaniel P. Hitt1, Lisa K. Bonneau2, Kunjuraman V. Jayachandran3, and Michael P. Marchetti4 1U.S. Geological Survey, Leetown Science Center, USA, 2Metropolitan Community College-Blue River, USA, 3Kerala Agricultural University, India, 4School of Science, St. -
Ecoregions of New England Forested Land Cover, Nutrient-Poor Frigid and Cryic Soils (Mostly Spodosols), and Numerous High-Gradient Streams and Glacial Lakes
58. Northeastern Highlands The Northeastern Highlands ecoregion covers most of the northern and mountainous parts of New England as well as the Adirondacks in New York. It is a relatively sparsely populated region compared to adjacent regions, and is characterized by hills and mountains, a mostly Ecoregions of New England forested land cover, nutrient-poor frigid and cryic soils (mostly Spodosols), and numerous high-gradient streams and glacial lakes. Forest vegetation is somewhat transitional between the boreal regions to the north in Canada and the broadleaf deciduous forests to the south. Typical forest types include northern hardwoods (maple-beech-birch), northern hardwoods/spruce, and northeastern spruce-fir forests. Recreation, tourism, and forestry are primary land uses. Farm-to-forest conversion began in the 19th century and continues today. In spite of this trend, Ecoregions denote areas of general similarity in ecosystems and in the type, quality, and 5 level III ecoregions and 40 level IV ecoregions in the New England states and many Commission for Environmental Cooperation Working Group, 1997, Ecological regions of North America – toward a common perspective: Montreal, Commission for Environmental Cooperation, 71 p. alluvial valleys, glacial lake basins, and areas of limestone-derived soils are still farmed for dairy products, forage crops, apples, and potatoes. In addition to the timber industry, recreational homes and associated lodging and services sustain the forested regions economically, but quantity of environmental resources; they are designed to serve as a spatial framework for continue into ecologically similar parts of adjacent states or provinces. they also create development pressure that threatens to change the pastoral character of the region. -
Ecosystem Services Generated by Fish Populations
AR-211 Ecological Economics 29 (1999) 253 –268 ANALYSIS Ecosystem services generated by fish populations Cecilia M. Holmlund *, Monica Hammer Natural Resources Management, Department of Systems Ecology, Stockholm University, S-106 91, Stockholm, Sweden Abstract In this paper, we review the role of fish populations in generating ecosystem services based on documented ecological functions and human demands of fish. The ongoing overexploitation of global fish resources concerns our societies, not only in terms of decreasing fish populations important for consumption and recreational activities. Rather, a number of ecosystem services generated by fish populations are also at risk, with consequences for biodiversity, ecosystem functioning, and ultimately human welfare. Examples are provided from marine and freshwater ecosystems, in various parts of the world, and include all life-stages of fish. Ecosystem services are here defined as fundamental services for maintaining ecosystem functioning and resilience, or demand-derived services based on human values. To secure the generation of ecosystem services from fish populations, management approaches need to address the fact that fish are embedded in ecosystems and that substitutions for declining populations and habitat losses, such as fish stocking and nature reserves, rarely replace losses of all services. © 1999 Elsevier Science B.V. All rights reserved. Keywords: Ecosystem services; Fish populations; Fisheries management; Biodiversity 1. Introduction 15 000 are marine and nearly 10 000 are freshwa ter (Nelson, 1994). Global capture fisheries har Fish constitute one of the major protein sources vested 101 million tonnes of fish including 27 for humans around the world. There are to date million tonnes of bycatch in 1995, and 11 million some 25 000 different known fish species of which tonnes were produced in aquaculture the same year (FAO, 1997). -
Spatial Variation in Fish Assemblages Across a Beaver-Influenced Successional Landscape
Ecology, 81(5), 2000, pp. 1371±1382 q 2000 by the Ecological Society of America SPATIAL VARIATION IN FISH ASSEMBLAGES ACROSS A BEAVER-INFLUENCED SUCCESSIONAL LANDSCAPE ISAAC J. SCHLOSSER1,3 AND LARRY W. K ALLEMEYN2 1Department of Biology, Box 9019, University Station, Grand Forks, North Dakota 58202 USA 2United States Geological Survey, Columbia Environmental Research Center, International Falls Biological Station, 3131 Highway 33, International Falls, Minnesota 56649 USA Abstract. Beavers are increasingly viewed as ``ecological engineers,'' having broad effects on physical, chemical, and biological attributes of north-temperate landscapes. We examine the in¯uence of both local successional processes associated with beaver activity and regional geomorphic boundaries on spatial variation in ®sh assemblages along the Kabetogama Peninsula in Voyageurs National Park, northern Minnesota, USA. Fish abun- dance and species richness exhibited considerable variation among drainages along the peninsula. Geological barriers to ®sh dispersal at outlets of some drainages has reduced ®sh abundance and species richness. Fish abundance and species richness also varied within drainages among local environments associated with beaver pond succession. Fish abun- dance was higher in upland ponds than in lowland ponds, collapsed ponds, or streams, whereas species richness was highest in collapsed ponds and streams. Cluster analyses based on ®sh abundance at sites classi®ed according to successional environment indicated that four species (northern redbelly dace, Phoxinus eos; brook stickleback, Culaea incon- stans; ®nescale dace, P. neogaeus; and fathead minnow, Pimephales promelas), were pre- dominant in all successional environments. Several less abundant species were added in collapsed ponds and streams, with smaller size classes of large lake species (e.g., black crappie, Pomoxis nigromaculatus; smallmouth bass, Micropertus dolomieui; yellow perch, Perca ¯avescens; and burbot, Lota lota) being a component of these less abundant species. -
Carbon Stocks and Soil Sequestration Rates of Riverine Mangroves and Freshwater Wetlands” by M
Open Access Biogeosciences Discuss., 12, C614–C618, 2015 www.biogeosciences-discuss.net/12/C614/2015/ Biogeosciences © Author(s) 2015. This work is distributed under Discussions the Creative Commons Attribute 3.0 License. Interactive comment on “Carbon stocks and soil sequestration rates of riverine mangroves and freshwater wetlands” by M. F. Adame et al. Anonymous Referee #1 Received and published: 15 March 2015 General comments: In this manuscript, Adame and colleagues measured carbon pools in vegetation, downed wood, and soils of seven mangrove sites, one peat swamp for- est, and one herbaceous marsh within Mexico’s La Encrucijada Biosphere Reserve (LEBR). They also measured soil N pools at all sites and rates of soil C sequestra- tion at the mangrove sites. The peat swamp and marsh sites appear to have been included only for the sake of making casual (rather than statistical) comparisons, since there was just one of each of those site types. The primary hypothesis was that soil C and N stocks and soil C sequestration rates would be higher in upland vs. lowland mangroves. This is a very descriptive place-based study. Although the authors made some sugges- tions about why some sites store more carbon than others (e.g., perhaps it is related C614 to geomorphology or the dominant tree species), this manuscript didn’t leave me with any new ideas or insights about how wetlands “work.” I didn’t feel that it told me any- thing more than some specific information about one specific location, and I think that will limit its appeal to the diverse readership of Biogeosciences. -
Chapter 3 M-32 & Old 27 / I-75 Business Loop Corridor Study
M-32 & Old 27 / I-75 Business Loop Corridor Study Environmental Analysis The wealth of natural resources within Otsego County is important to the overall health and vigor of the community; these resources are an economic anchor and play a key role in the quality of life for county residents. The study area traverses rolling hills, forestlands, farmlands, open spaces and high quality water resources, presenting an ever changing array of scenic vistas. Natural resources within the 1/2 mile wide corridor are connected to much larger regional landscape features, and as a result, activities within the study area can have far reaching effects. The natural resources addressed in this chapter include forests, wetlands, farmlands, soils and water. A soils based analysis of development constraints will also be included in this chapter. Natural Resources Forests In addition to the scenic characteristics of woodlands, forested areas provide habitat for wildlife, protect the soil from erosion, filter air pollutants and act as a noise buffer along heavily traveled highways. Public and privately owned forested lands can be found throughout the corridor study area. Forest lands were mapped as a part of the existing land use analysis in Chapter 2. As noted in Chapter 2, woodland areas, both upland and lowland forest types, cover over 32 percent of the study area. Figure 3.1 is a map depicting the location of woodlands and wetlands within the study corridor. The dominant forest associations in the corridor study area are northern hardwoods (sugar maple, American beech and basswood); aspen/white birch; red and white oak and red pine plantations in the upland areas. -
Lake Superior Phototrophic Picoplankton: Nitrate Assimilation
LAKE SUPERIOR PHOTOTROPHIC PICOPLANKTON: NITRATE ASSIMILATION MEASURED WITH A CYANOBACTERIAL NITRATE-RESPONSIVE BIOREPORTER AND GENETIC DIVERSITY OF THE NATURAL COMMUNITY Natalia Valeryevna Ivanikova A Dissertation Submitted to the Graduate College of Bowling Green State University in partial fulfillment of the requirements for the degree of DOCTOR OF PHILOSOPHY May 2006 Committee: George S. Bullerjahn, Advisor Robert M. McKay Scott O. Rogers Paul F. Morris Robert K. Vincent Graduate College representative ii ABSTRACT George S. Bullerjahn, Advisor Cyanobacteria of the picoplankton size range (picocyanobacteria) Synechococcus and Prochlorococcus contribute significantly to total phytoplankton biomass and primary production in marine and freshwater oligotrophic environments. Despite their importance, little is known about the biodiversity and physiology of freshwater picocyanobacteria. Lake Superior is an ultra- oligotrophic system with light and temperature conditions unfavorable for photosynthesis. Synechococcus-like picocyanobacteria are an important component of phytoplankton in Lake Superior. The concentration of nitrate, the major form of combined nitrogen in the lake, has been increasing continuously in these waters over the last 100 years, while other nutrients remained largely unchanged. Decreased biological demand for nitrate caused by low availabilities of phosphorus and iron, as well as low light and temperature was hypothesized to be one of the reasons for the nitrate build-up. One way to get insight into the microbiological processes that contribute to the accumulation of nitrate in this ecosystem is to employ a cyanobacterial bioreporter capable of assessing the nitrate assimilation capacity of phytoplankton. In this study, a nitrate-responsive biorepoter AND100 was constructed by fusing the promoter of the Synechocystis PCC 6803 nitrate responsive gene nirA, encoding nitrite reductase to the Vibrio fischeri luxAB genes, which encode the bacterial luciferase, and genetically transforming the resulting construct into Synechocystis. -
Factors Affecting Distribution of Wood, Detritus, and Sediment in Headwater Streams Draining Managed Young-Growth Red Alder - Conifer Forests in Southeast Alaska
Factors affecting distribution of wood, detritus, and sediment in headwater streams draining managed young-growth red alder - conifer forests in southeast Alaska Takashi Gomi, Adelaide C. Johnson, Robert L. Deal, Paul E. Hennon, Ewa H. Orlikowska, and Mark S. Wipfli Abstract: Factors (riparian stand condition, management regimes, and channel properties) affecting distributions of wood, detritus (leaves and branches), and sediment were examined in headwater streams draining young-growth red alder (Alnus rubra Bong.) - conifer riparian forests (40 years old) in southeast Alaska. More riparian red alder were found along streams affected by both timber harvesting and mass movement than in streams affected by timber harvest- ing alone. Young-growth stands produced little large wood material (diameter >10 cm) and had little effect on altering the size distribution of functional large wood in channels, although more alder wood pieces were found in streams with greater numbers of riparian alder trees. Legacy wood pieces (>40 years old) remained in channels and provided sites for sediment and organic matter storage. Despite various alder-conifer mixtures and past harvesting effects, the abun- dance of large wood, fine wood, and detritus accumulations significantly decreased with increasing channel bank-full width (0.5-3.5 m) along relatively short channel distances (up to 700 m). Changes in wood, detritus, and sediment ac- cumulations together with changes in riparian stand characteristics create spatial and temporal variability of in-channel -
Assessment of the Trophic Status at Al-Sabil River Using the Trophic Indices in Al-Shinafiya District, Southern Iraq
EurAsian Journal of BioSciences Eurasia J Biosci 14, 5661-5667 (2020) Assessment of the trophic status at Al-Sabil River using the trophic indices in Al-Shinafiya district, Southern Iraq Khitam Abbas Marhoon 1, Eman Mohammed Hussain 2, Salwan Ali Abed 3, Salam Hussein Ewaid 4, Mudhafar A. Salim 5, Nadhir Al-Ansari 6 1,3 Environment Department, College of Science, University of Al-Qadisiyah, IRAQ 2 Biology Department, College of Science, University of Al-Qadisiyah, IRAQ 4 Technical Institute of Shatra, Southern Technical University, IRAQ 5 Arab Regional Center for World Heritage, Manama, BAHRAIN. 6 Luleå University of Technology, Luleå, SWEDEN *Corresponding author: [email protected] ; [email protected] Abstract The current study was conducted to determine the quality of the water of Al- Sabil River in Al-Shinafiya district, Province of Al- Diwaniyah, for the period from September 2018 to August 2019. Three sites were selected along the river, a quantitative and qualitative study of the diatoms as well as its indices to assess the quality of water in the river, such as trophic diatom Index (TDI), Trophic State Index (TSI), Diatomic Index (DI), and General Diatoms Index (GDI). The current study was diagnosed about 136 species of diatoms at three sites, where the central diatoms was 12 species while the pannals diatoms reached 124 species, and recorded total numbers of diatoms (35453.8, 29447.2 and 36504.76) cell*310/L, and rates (2954.48, 2453.93 and 3042.06) cells*310/L for the three locations respectively, as shown by the results of the trophic diatom Index(TDI) values ranged from (23.33 to 55.54) and the values of Trophic State Index (TSI) ranged from (0.07 to 0.81) and the Diatomic Index (DI) values ranged from (9.08 to 16.20) and the values of the General Diatoms Index (GDI) ranged from (2.23 to 3.17). -
Shifting Mineral and Redox Controls on Carbon Cycling in Seasonally flooded Mineral Soils
Biogeosciences, 16, 2573–2589, 2019 https://doi.org/10.5194/bg-16-2573-2019 © Author(s) 2019. This work is distributed under the Creative Commons Attribution 4.0 License. Shifting mineral and redox controls on carbon cycling in seasonally flooded mineral soils Rachelle E. LaCroix1, Malak M. Tfaily2, Menli McCreight1, Morris E. Jones1, Lesley Spokas1, and Marco Keiluweit1 1School of Earth & Sustainability and Stockbridge School of Agriculture, University of Massachusetts, Amherst, MA, USA 2Soil, Water and Environmental Science Department, University of Arizona, Tucson, AZ, USA Correspondence: Marco Keiluweit ([email protected]) and Rachelle E. LaCroix ([email protected]) Received: 4 October 2018 – Discussion started: 12 October 2018 Revised: 5 June 2019 – Accepted: 12 June 2019 – Published: 4 July 2019 Abstract. Although wetland soils represent a relatively small land soils, yet Feo had no predictive power in lowland soils. portion of the terrestrial landscape, they account for an esti- Instead, our model showed that Eh and oxalate-extractable Al mated 20 %–30 % of the global soil carbon (C) reservoir. C (Alo, a proxy of protective Al phases) became significantly stored in wetland soils that experience seasonal flooding is stronger predictors in the lowland soils. Combined, our re- likely the most vulnerable to increased severity and duration sults suggest that low redox potentials are the primary cause of droughts in response to climate change. Redox conditions, for C accumulation in seasonally flooded surface soils, likely plant root dynamics, and the abundance of protective mineral due to selective preservation of organic compounds under phases are well-established controls on soil C persistence, anaerobic conditions. -
Chapter 3: Refuge Environment
Chapter 3: Refuge Environment Chapter 3: Refuge Environment Introduction Tamarac NWR encompasses 42,738 acres of land and waters in the glacial lake area of northwestern Minnesota. The Refuge is located in Becker County, 18 miles northeast of Detroit Lakes, in the heart of one of the most diverse ecological transition zones in North America, where northern hardwood forests, coniferous forest and tall grass prairie converge. Between 10,000 and 10,500 years ago, receding gla- ciers left behind the rolling ridges and deep depres- sions that became a woodland area complemented by lakes, rivers, bogs and marshes and is now Tama- rac NWR. The primary ecological drivers influenc- ing the plant and wildlife populations of the Refuge are the climate, hydrology, and natural disturbances Frog. Photo Credit: Michele Gedgaud such as fire, disease and wind events. Other Units Administered and after the Refuge’s establishment, particularly from agriculture, timber harvest, roads, and water Wilderness Area control. Although Tamarac NWR cannot be The Tamarac Wilderness Area was established described as pristine, it is largely an intact, health by law in 1976. The Wilderness Area is managed and functioning ecosystem that just does not meet under the provisions of the 1964 Wilderness Act as a the strict definition of suitable lands. unit of the National Wilderness Preservation Sys- tem. That is, it is “an area where the earth and its Areas of Special Designation community of life are untrammeled by man, where The Research Natural Areas were designated in man himself is a visitor who does not remain” (The 1972 with some general management and protection Wilderness Act, September 3, 1964; (16 U.S.C. -
Aquatic Ecosystems Bibliography Compiled by Robert C. Worrest
Aquatic Ecosystems Bibliography Compiled by Robert C. Worrest Abboudi, M., Jeffrey, W. H., Ghiglione, J. F., Pujo-Pay, M., Oriol, L., Sempéré, R., . Joux, F. (2008). Effects of photochemical transformations of dissolved organic matter on bacterial metabolism and diversity in three contrasting coastal sites in the northwestern Mediterranean Sea during summer. Microbial Ecology, 55(2), 344-357. Abboudi, M., Surget, S. M., Rontani, J. F., Sempéré, R., & Joux, F. (2008). Physiological alteration of the marine bacterium Vibrio angustum S14 exposed to simulated sunlight during growth. Current Microbiology, 57(5), 412-417. doi: 10.1007/s00284-008-9214-9 Abernathy, J. W., Xu, P., Xu, D. H., Kucuktas, H., Klesius, P., Arias, C., & Liu, Z. (2007). Generation and analysis of expressed sequence tags from the ciliate protozoan parasite Ichthyophthirius multifiliis BMC Genomics, 8, 176. Abseck, S., Andrady, A. L., Arnold, F., Björn, L. O., Bomman, J. F., Calamari, D., . Zepp, R. G. (1998). Environmental effects of ozone depletion: 1998 assessment. Journal of Photochemistry and Photobiology B: Biology, 46(1-3), 1-108. doi: Doi: 10.1016/s1011-1344(98)00195-x Adachi, K., Kato, K., Wakamatsu, K., Ito, S., Ishimaru, K., Hirata, T., . Kumai, H. (2005). The histological analysis, colorimetric evaluation, and chemical quantification of melanin content in 'suntanned' fish. Pigment Cell Research, 18, 465-468. Adams, M. J., Hossaek, B. R., Knapp, R. A., Corn, P. S., Diamond, S. A., Trenham, P. C., & Fagre, D. B. (2005). Distribution Patterns of Lentic-Breeding Amphibians in Relation to Ultraviolet Radiation Exposure in Western North America. Ecosystems, 8(5), 488-500. Adams, N.