Ramesh D. Gulati Egor S. Zadereev Andrei G. Degermendzhi Editors Ecology of Meromictic Lakes Ecological Studies
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An Analysis of Primary and Secondary Production in Lake Kariba in a Changing Climate
AN ANALYSIS OF PRIMARY AND SECONDARY PRODUCTION IN LAKE KARIBA IN A CHANGING CLIMATE MZIME R. NDEBELE-MURISA A thesis submitted in partial fulfillment of the requirements for the degree of Doctor Philosophiae in the Department of Biodiversity and Conservation Biology, University of the Western Cape Supervisor: Prof. Charles Musil Co-Supervisor: Prof. Lincoln Raitt May 2011 An analysis of primary and secondary production in Lake Kariba in a changing climate Mzime Regina Ndebele-Murisa KEYWORDS Climate warming Limnology Primary production Phytoplankton Zooplankton Kapenta production Lake Kariba i Abstract Title: An analysis of primary and secondary production in Lake Kariba in a changing climate M.R. Ndebele-Murisa PhD, Biodiversity and Conservation Biology Department, University of the Western Cape Analysis of temperature, rainfall and evaporation records over a 44-year period spanning the years 1964 to 2008 indicates changes in the climate around Lake Kariba. Mean annual temperatures have increased by approximately 1.5oC, and pan evaporation rates by about 25%, with rainfall having declined by an average of 27.1 mm since 1964 at an average rate of 6.3 mm per decade. At the same time, lake water temperatures, evaporation rates, and water loss from the lake have increased, which have adversely affected lake water levels, nutrient and thermal dynamics. The most prominent influence of the changing climate on Lake Kariba has been a reduction in the lake water levels, averaging 9.5 m over the past two decades. These are associated with increased warming, reduced rainfall and diminished water and therefore nutrient inflow into the lake. The warmer climate has increased temperatures in the upper layers of lake water, the epilimnion, by an overall average of 1.9°C between 1965 and 2009. -
Pond and Lake Ecosystems a Pond Or Lake Ecosystem Includes Biotic
Pond and Lake Ecosystems A pond or lake ecosystem includes biotic (living) plants, animals and micro-organisms, as well as abiotic (nonliving) physical and chemical interactions. Pond and lake ecosystems are a prime example of lentic ecosystems. Lentic refers to stationary or relatively still water, from the Latin lentus, which means sluggish. A typical lake has distinct zones of biological communities linked to the physical structure of the lake. (Figure below) The littoral zone is the near shore area where sunlight penetrates all the way to the sediment and allows aquatic plants (macrophytes) to grow. Light levels of about 1% or less of surface values usually define this depth. The 1% light level also defines the euphotic zone of the lake, which is the layer from the surface down to the depth where light levels become too low for photosynthesizers. In most lakes, the sunlit euphotic zone occurs within the epilimnion. However, in unusually transparent lakes, photosynthesis may occur well below the thermocline into the perennially cold hypolimnion. For example, in western Lake Superior near Duluth, MN, summertime algal photosynthesis and growth can persist to depths of at least 25 meters, while the mixed layer, or epilimnion, only extends down to about 10 meters. Ultra-oligotrophic Lake Tahoe, CA/NV, is so transparent that algal growth historically extended to over 100 meters, though its mixed layer only extends to about 10 meters in summer. Unfortunately, inadequate management of the Lake Tahoe basin since about 1960 has led to a significant loss of transparency due to increased algal growth and increased sediment inputs from stream and shoreline erosion. -
Bright Peaks, Dark Shadows 20 February 2012, by Jason Major
Bright peaks, dark shadows 20 February 2012, by Jason Major Amaral's "blue" peaks seen in a color-enhanced global image acquired Jan. 14, 2008. Its central peaks also attracted astronomers' MESSENGER image of Mercury's Amaral crater interest, as they were seen to possess a striking blue hue in color-enhanced images that likely indicates rocks with different composition from the surrounding surface. The 68-mile (109-km) -wide Amaral crater on Mercury reveals its brightly-tipped central peaks in Amaral's peaks resemble those of the slightly larger this image, acquired by NASA's MESSENGER crater Eminescu, which is now known to contain spacecraft on Feb. 4, 2012. Long shadows are recently-discovered features called hollows. It's not cast by the crater's peaks and rugged rim (north is yet known if Amaral also contains hollows, but it's to the left.) suspected that they may be present on the tips of the peaks. The image was acquired as a high-resolution targeted observation with MESSENGER's Narrow- The crater is named after Brazilian artist Tarsila do Angle Camera (NAC) on its Mercury Dual Imaging Amaral. She lived from 1886 to 1973 and is System (MDIS). considered to be one of the leading Latin American modernist painters. Amaral's bright peaks were first spotted during MESSENGER's first flyby of Mercury in Jan. 2008. With a smooth floor, visible ejecta and small Source: Universe Today secondary craters, Amaral appeared noticeably younger than the heavily cratered surface around it. 1 / 2 APA citation: Bright peaks, dark shadows (2012, February 20) retrieved 26 September 2021 from https://phys.org/news/2012-02-bright-peaks-dark-shadows.html This document is subject to copyright. -
Estimates of Hypolimnetic Oxygen Deficits in Ponds
Aquacullure and Fisheries Management 1989, 20, 167-172 Estimates of hypolimnetic oxygen deficits in ponds W. Y. B. CHANG Center for Great Lakes and Aquatic Sciences, University of Michigan, Ann Arbor, Michigan, USA Abstract. Shallow tropical integrated culture ponds in the Pearl River Delta. China, have been found to stratify almost daily, with high organic loadings and dense algal growth. The dissolved oxygen (DO) concentration is super-saturated in the epilimnion and is under 2 mg/l in the hypolimnion (>lm). The compensation depth corresponds to twice the Secchi disk depth ranging from 50 to 80cm. As a result, little or no net oxygen is produced in the hypolimnion (> 1 m). The low DO concentration in the hypolimnion causes organic materials, such as unused organic wastes and senescent algae cells, to be incompletely oxidized, since the rate of oxygen consumption by oxidable matter in water is dependent on the dissolved oxygen concentration in water. This material becomes the source of hypolimnetic oxygen deficits (HOD) which can drive whole pond DO to a dangerously low level, should sudden destratification occur. An improved estimate of hypolimnetic oxygen deficits is introduced in this article, and the advantages of this method are discussed. Introduction Oxygen is an important parameter in fish culture, and adequate levels of dissolved oxygen (DO) are essential for maintaining optimum fish growth. Inadequate dissolved oxygen and poor water quality are frequently found in ponds receiving organic wastes and can lead to many serious problems for fish culture in ponds. Problems of low dissolved oxygen are particularly prevalent in ponds during the night and early morning when there are high densities of fish and large additions of organic wastes and feeds (Schroeder 1974; Boyd 1982; Chang 1986). -
Evidence for Thermal-Stress-Induced Rockfalls on Mars Impact Crater Slopes
Icarus 342 (2020) 113503 Contents lists available at ScienceDirect Icarus journal homepage: www.elsevier.com/locate/icarus Evidence for thermal-stress-induced rockfalls on Mars impact crater slopes P.-A. Tesson a,b,*, S.J. Conway b, N. Mangold b, J. Ciazela a, S.R. Lewis c, D. M�ege a a Space Research Centre, Polish Academy of Science, Wrocław, Poland b Laboratoire de Plan�etologie et G�eodynamique UMR 6112, CNRS, Nantes, France c School of Physical Sciences, The Open University, Walton Hall, Milton Keynes MK7 6AA, UK ARTICLE INFO ABSTRACT Keywords: Here we study rocks falling from exposed outcrops of bedrock, which have left tracks on the slope over which Mars, surface they have bounced and/or rolled, in fresh impact craters (1–10 km in diameter) on Mars. The presence of these Thermal stress tracks shows that these rocks have fallen relatively recently because aeolian processes are known to infill Ices topographic lows over time. Mapping of rockfall tracks indicate trends in frequency with orientation, which in Solar radiation � � turn depend on the latitudinal position of the crater. Craters in the equatorial belt (between 15 N and 15 S) Weathering exhibit higher frequencies of rockfall on their north-south oriented slopes compared to their east-west ones. � Craters >15 N/S have notably higher frequencies on their equator-facing slopes as opposed to the other ori entations. We computed solar radiation on the surface of crater slopes to compare insolation patterns with the spatial distribution of rockfalls, and found statistically significant correlations between maximum diurnal inso lation and rockfall frequency. -
Molecular Biogeochemistry, Lecture 8
12.158 Lecture Pigment-derived Biomarkers (1) Colour, structure, distribution and function (2) Biosynthesis (3) Nomenclature (4) Aromatic carotenoids ● Biomarkers for phototrophic sulfur bacteria ● Alternative biological sources (5) Porphyrins and maleimides Many of the figures in this lecture were kindly provided by Jochen Brocks, RSES ANU 1 Carotenoid pigments ● Carotenoids are usually yellow, orange or red coloured pigments lutein β-carotene 17 18 19 2' 2 4 6 8 3 7 9 16 1 5 lycopenelycopene 2 Structural diversity ● More than 600 different natural structures are known, ● They are derived from the C40 carotenoid lycopene by varied hydrogenation, dehydrogenation, cyclization and oxidation reaction 17 18 19 2' 2 4 6 8 3 7 9 16 1 5 lycopene neurosporene α-carotene γ -carotene spirilloxanthin siphonaxanthin canthaxanthin spheroidenone 3 Structural diversity Purple non-sulfur bacteria peridinin 7,8-didehydroastaxanthin okenone fucoxanthin Biological distribution ● Carotenoids are biosynthesized de novo by all phototrophic bacteria, eukaryotes and halophilic archaea ● They are additionally synthesized by a large variety of non-phototrophs ● Vertebrates and invertebrates have to incorporate carotenoids through the diet, but have often the capacity to structurally modifiy them 4 Carotenoid function (1) Accessory pigments in Light Harvesting Complex (LHC) (annual production by marine phytoplancton alone: 4 million tons) e.g. LH-II Red and blue: protein complex Green: chlorophyll Yellow: lycopene (2) Photoprotection (3) photoreceptors for phototropism -
Mito-Nuclear Sequencing Is Paramount to Correctly Identify Sympatric Hybridizing Fishes
ACTA ICHTHYOLOGICA ET PISCATORIA (2018) 48 (2): 123–141 DOI: 10.3750/AIEP/02348 MITO-NUCLEAR SEQUENCING IS PARAMOUNT TO CORRECTLY IDENTIFY SYMPATRIC HYBRIDIZING FISHES Carla SOUSA-SANTOS1*, Ana M. PEREIRA1, Paulo BRANCO2, Gonçalo J. COSTA3, José M. SANTOS2, Maria T. FERREIRA2, Cristina S. LIMA1, Ignacio DOADRIO4, and Joana I. ROBALO1 1 MARE—Marine and Environmental Sciences Centre, ISPA—Instituto Universitário, Lisboa, Portugal 2 CEF—Forest Research Centre, Instituto Superior de Agronomia, Universidade de Lisboa, Lisboa, Portugal 3 Computational Biology and Population Genomics Group (CoBiG2), Centre for Ecology, Evolution and Environmental Changes (CE3C), Faculdade de Ciências, Universidade de Lisboa, Lisboa, Portugal 4 Department of Biodiversity and Evolutionary Biology, Museo Nacional de Ciencias Naturales, CSIC, Madrid, Spain Sousa-Santos C., Pereira A.M., Branco P., Costa G.J., Santos J.M., Ferreira M.T., Lima C.S., Doadrio I., Robalo J.I. 2018. Mito-nuclear sequencing is paramount to correctly identify sympatric hybridizing fishes. Acta Ichthyol. Piscat. 48 (2): 123–141. Background. Hybridization may drive speciation and erode species, especially when intrageneric sympatric species are involved. Five sympatric Luciobarbus species—Luciobarbus sclateri (Günther, 1868), Luciobarbus comizo (Steindachner, 1864), Luciobarbus microcephalus (Almaça, 1967), Luciobarbus guiraonis (Steindachner, 1866), and Luciobarbus steindachneri (Almaça, 1967)—are commonly identified in field surveys by diagnostic morphological characters. Assuming that i) in loco identification is subjective and observer-dependent, ii) there is previous evidence of interspecific hybridization, and iii) the technical reports usually do not include molecular analyses, our main goal was to assess the concordance between in loco species identification based on phenotypic characters with identifications based on morphometric indices, mtDNA only, and a combination of mito-nuclear markers. -
Water Resources Report
MMINNEAPOLISINNEAPOLIS PPARKARK && RRECREATIONECREATION BBOARDOARD 20122012 WWATERATER RRESOURCESESOURCES RREPORTEPORT Environmental Stewardship Water Resources Management www.minneapolisparks.org January 2015 2012 WATER RESOURCES REPORT Prepared by: Minneapolis Park & Recreation Board Environmental Stewardship 3800 Bryant Avenue South Minneapolis, MN 55409-1029 612.230.6400 www.minneapolisparks.org January 2015 Funding provided by: Minneapolis Park & Recreation Board City of Minneapolis Public Works Copyright © 2015 by the Minneapolis Park & Recreation Board Material may be quoted with attribution. TABLE OF CONTENTS Page Abbreviations ............................................................................................................................. i Executive Summary ............................................................................................................... iv 1. Monitoring Program Overview .............................................................................................. 1-1 2. Birch Pond .............................................................................................................................. 2-1 3. Brownie Lake ......................................................................................................................... 3-1 4. Lake Calhoun ......................................................................................................................... 4-1 5. Cedar Lake ............................................................................................................................ -
Residence Time and Physical Processes in Lakes
Papers from Bolsena Conference (2002). Residence time in lakes:Science, Management, Education J. Limnol., 62(Suppl. 1): 1-15, 2003 Residence time and physical processes in lakes Walter AMBROSETTI*, Luigi BARBANTI and Nicoletta SALA1) CNR Institute of Ecosystem Study, L.go V. Tonolli 50, 28922 Verbania Pallanza, Italy 1)University of Italian Switzerland- Academy of Architecture, Mendrisio (TI) *e-mail corresponding author: [email protected] ABSTRACT The residence time of a lake is highly dependent on internal physical processes in the water mass conditioning its hydrodynam- ics; early attempts to evaluate this physical parameter emphasize the complexity of the problem, which depends on very different natural phenomena with widespread synergies. The aim of this study is to analyse the agents involved in these processes and arrive at a more realistic definition of water residence time which takes account of these agents, and how they influence internal hydrody- namics. With particular reference to temperate lakes, the following characteristics are analysed: 1) the set of the lake's caloric com- ponents which, along with summer heating, determine the stabilizing effect of the surface layers, and the consequent thermal stratifi- cation, as well as the winter destabilizing effect; 2) the wind force, which transfers part of its momentum to the water mass, generat- ing a complex of movements (turbulence, waves, currents) with the production of active kinetic energy; 3) the water flowing into the lake from the tributaries, and flowing out through the outflow, from the standpoint of hydrology and of the kinetic effect generated by the introduction of these water masses into the lake. -
Protist Phylogeny and the High-Level Classification of Protozoa
Europ. J. Protistol. 39, 338–348 (2003) © Urban & Fischer Verlag http://www.urbanfischer.de/journals/ejp Protist phylogeny and the high-level classification of Protozoa Thomas Cavalier-Smith Department of Zoology, University of Oxford, South Parks Road, Oxford, OX1 3PS, UK; E-mail: [email protected] Received 1 September 2003; 29 September 2003. Accepted: 29 September 2003 Protist large-scale phylogeny is briefly reviewed and a revised higher classification of the kingdom Pro- tozoa into 11 phyla presented. Complementary gene fusions reveal a fundamental bifurcation among eu- karyotes between two major clades: the ancestrally uniciliate (often unicentriolar) unikonts and the an- cestrally biciliate bikonts, which undergo ciliary transformation by converting a younger anterior cilium into a dissimilar older posterior cilium. Unikonts comprise the ancestrally unikont protozoan phylum Amoebozoa and the opisthokonts (kingdom Animalia, phylum Choanozoa, their sisters or ancestors; and kingdom Fungi). They share a derived triple-gene fusion, absent from bikonts. Bikonts contrastingly share a derived gene fusion between dihydrofolate reductase and thymidylate synthase and include plants and all other protists, comprising the protozoan infrakingdoms Rhizaria [phyla Cercozoa and Re- taria (Radiozoa, Foraminifera)] and Excavata (phyla Loukozoa, Metamonada, Euglenozoa, Percolozoa), plus the kingdom Plantae [Viridaeplantae, Rhodophyta (sisters); Glaucophyta], the chromalveolate clade, and the protozoan phylum Apusozoa (Thecomonadea, Diphylleida). Chromalveolates comprise kingdom Chromista (Cryptista, Heterokonta, Haptophyta) and the protozoan infrakingdom Alveolata [phyla Cilio- phora and Miozoa (= Protalveolata, Dinozoa, Apicomplexa)], which diverged from a common ancestor that enslaved a red alga and evolved novel plastid protein-targeting machinery via the host rough ER and the enslaved algal plasma membrane (periplastid membrane). -
Coupled Reductive and Oxidative Sulfur Cycling in the Phototrophic Plate of a Meromictic Lake T
Geobiology (2014), 12, 451–468 DOI: 10.1111/gbi.12092 Coupled reductive and oxidative sulfur cycling in the phototrophic plate of a meromictic lake T. L. HAMILTON,1 R. J. BOVEE,2 V. THIEL,3 S. R. SATTIN,2 W. MOHR,2 I. SCHAPERDOTH,1 K. VOGL,3 W. P. GILHOOLY III,4 T. W. LYONS,5 L. P. TOMSHO,3 S. C. SCHUSTER,3,6 J. OVERMANN,7 D. A. BRYANT,3,6,8 A. PEARSON2 AND J. L. MACALADY1 1Department of Geosciences, Penn State Astrobiology Research Center (PSARC), The Pennsylvania State University, University Park, PA, USA 2Department of Earth and Planetary Sciences, Harvard University, Cambridge, MA, USA 3Department of Biochemistry and Molecular Biology, The Pennsylvania State University, University Park, PA, USA 4Department of Earth Sciences, Indiana University-Purdue University Indianapolis, Indianapolis, IN, USA 5Department of Earth Sciences, University of California, Riverside, CA, USA 6Singapore Center for Environmental Life Sciences Engineering, Nanyang Technological University, Nanyang, Singapore 7Leibniz-Institut DSMZ-Deutsche Sammlung von Mikroorganismen und Zellkulturen, Braunschweig, Germany 8Department of Chemistry and Biochemistry, Montana State University, Bozeman, MT, USA ABSTRACT Mahoney Lake represents an extreme meromictic model system and is a valuable site for examining the organisms and processes that sustain photic zone euxinia (PZE). A single population of purple sulfur bacte- ria (PSB) living in a dense phototrophic plate in the chemocline is responsible for most of the primary pro- duction in Mahoney Lake. Here, we present metagenomic data from this phototrophic plate – including the genome of the major PSB, as obtained from both a highly enriched culture and from the metagenomic data – as well as evidence for multiple other taxa that contribute to the oxidative sulfur cycle and to sulfate reduction. -
Altitudinal Zonation of Green Algae Biodiversity in the French Alps
Altitudinal Zonation of Green Algae Biodiversity in the French Alps Adeline Stewart, Delphine Rioux, Fréderic Boyer, Ludovic Gielly, François Pompanon, Amélie Saillard, Wilfried Thuiller, Jean-Gabriel Valay, Eric Marechal, Eric Coissac To cite this version: Adeline Stewart, Delphine Rioux, Fréderic Boyer, Ludovic Gielly, François Pompanon, et al.. Altitu- dinal Zonation of Green Algae Biodiversity in the French Alps. Frontiers in Plant Science, Frontiers, 2021, 12, pp.679428. 10.3389/fpls.2021.679428. hal-03258608 HAL Id: hal-03258608 https://hal.archives-ouvertes.fr/hal-03258608 Submitted on 11 Jun 2021 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. fpls-12-679428 June 4, 2021 Time: 14:28 # 1 ORIGINAL RESEARCH published: 07 June 2021 doi: 10.3389/fpls.2021.679428 Altitudinal Zonation of Green Algae Biodiversity in the French Alps Adeline Stewart1,2,3, Delphine Rioux3, Fréderic Boyer3, Ludovic Gielly3, François Pompanon3, Amélie Saillard3, Wilfried Thuiller3, Jean-Gabriel Valay2, Eric Maréchal1* and Eric Coissac3* on behalf of The ORCHAMP Consortium 1 Laboratoire de Physiologie Cellulaire et Végétale, CEA, CNRS, INRAE, IRIG, Université Grenoble Alpes, Grenoble, France, 2 Jardin du Lautaret, CNRS, Université Grenoble Alpes, Grenoble, France, 3 Université Grenoble Alpes, Université Savoie Mont Blanc, CNRS, LECA, Grenoble, France Mountain environments are marked by an altitudinal zonation of habitat types.