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Notes: CAN 133:212535

61-1


Water

Baruch Marine Laboratory,Georgetown,SC,USA.

Journal

0003-9136



written in English.

7723-14-0 (Phosphorus) Role: BPR (Biological process), BSU (Biological study, unclassified), BIOL (Biological study), PROC (Process) (life strategy and phosphorus relations of cyanobacterium Gloeotrichia echinulata in oligotrophic precambrian shield lake)



Reference Type: Journal Article

Record Number: 142

Author: Srivastava, D. K.

Year: 2000

Title: Cyanobacteria from paddy fields of Durg district of Chhattisgarh state

Journal: Phykos (India)

Volume: 39

Issue: 1-2

Pages: 125-129

Accession Number: 5206666

Keywords: Aquatic plants; Dominant species; Cysts; Cyanophyta; India,

Chhattisgarh, Durg Dist.

rice fields

Freshwater

Q1 01221 General

Abstract: During the survey of paddy fields of Durg district, Chhattisgarh, India, 36 species of Cyanobacteria were collected, identified and unialgal cultures of 12 species raised in Chu-10 medium. Out of these, 24 forms were non-heterocytous and rest was heterocystous forms. The dominant cyanobacteria were Aphanothece, Anabaena, Calothrix, Gloeotrichia, Lyngbya, Oscillatoria, Phormidium and Nostoc.

Notes: 2000.

English


Journal Article

Author Address: Department of Botany, Government Pt. J.L.V. Arts & Science College Bemetara Dist-Durg (Chhattisgarh) 491 335 India
Reference Type: Book

Record Number: 143

Author: Laugaste, R.

Year: 2000

Title: The dominant species of phytoplankton of L. Peipsi

Series Editor: Mols, T.; Haberman, J.; Kongo, L.

City: Tallinn

Publisher: Estonian Academy Publishers

Number of Pages: 97-121. [Eesti Looduseuur. Seltsi Aastaraam./Yearb. Est. Nat. Soc.]. 2000.

ISBN: 0135-2431

998550268X



Original Publication: Peipsi jarve futoplanktoni dominandid

Accession Number: 5355578

Keywords: Dominant species; Phytoplankton; Trophic levels; Seasonal

variations; Eutrophic lakes; Algal blooms; Aulacoseira islandica;

Aulacoseira granulata; Stephanodiscus binderanus; Gloeotrichia

echinulata; Aphanizomenon flos-aquae; Anabaena flos-aquae;

Estonia, Peipsi L.

Freshwater

Q1 01461 Plankton

Abstract: In different seasons and years main species of phytoplankton (dominants and subdominants) form 68-96% of biomass in L. Pihkva (southern, more eutrophic part) and 60-97% in L. Peipsi (northern, less eutrophic part) (Estonia). L. Lammijarv, connecting the two parts is similar to L. Pihkva in respect to phytoplankton and the trophic state. Diatoms and blue-green algae prevail in biomass, diatoms and green algae, in the species number. The complex of main species show the moderate eutrophy in northern part and high eutrophic state of southern part of L. Peipsi. Besides the different trophic level, the dominant complex and dynamics is connected with different water capacity of lake parts: water level and temperature in shallow L. Pihkva, the wind actions and streams in larger and deeper L. Peipsi "s.s." are the important factors effecting on occurrence and distribution of algae. The dominant complex has not changed considerably since 1909; however, the distribution of dominant species in lake parts has become more even in the last decades. Periods of high biomass occurred in the first half of the 1960s and 1970s and in 1988-1994, of low biomass in 1981-1987. The first coincided, in general, with periods of low water level and high water temperature.

Notes: Estonian Naturalists' Soc., Tallinn (Estonia)

Year-book of the Estonian Naturalists' Society. Eesti Looduseuurijate Seltsi aastaraamat. Vol. 79

Estonian

Book Monograph



Author Address: Institute of Zoology and Botany, Estonian Agricultural University Riia Str. 181, 51014 Tartu Estonia, [mailto:reet@zbi.ee]
Reference Type: Journal Article

Record Number: 144

Author: Hyenstrand, P.; Rydin, E.; Gunnerhed, M.

Year: 2000

Title: Response of pelagic cyanobacteria to iron additions - enclosure experiments from Lake Erken

Journal: Journal of Plankton Research

Volume: 22

Issue: 6

Pages: 1113-1126

Date: Jun

Alternate Journal: J. Plankton Res.

Accession Number: 4767820

Keywords: Iron; Lakes; Growth rate; Colony-inhibiting factors; Nutrient

availability; Sweden; Pelagic environment; Aquatic bacteria;

Nutrient deficiency; Limiting factors; Sweden, L. Erken; Bacteria;

Phosphates; Nitrates; Ammonium; Phytoplankton; Algal blooms;

Nutritional requirements; Gloeotrichia echinulata; Sweden, Erken

L.

phosphates; nitrates; ammonium; iron



Freshwater

K 03073 Algae; D 04627 Algae/lichens; SW 0850 Lakes; Q1 01425

Nutrition and feeding habits

Abstract: In this study, low epilimnetic iron availability during the summer stagnation period was concluded to be a limiting factor for cyanobacterial development in Lake Erken. In three enclosure experiments, different combinations of phosphate, nitrate and ammonium additions were tested both with and without additions of dissolved iron. The addition of iron increased the growth of diazotrophic cyanobacteria significantly compared with enclosures not receiving iron. This was especially evident for the colony-forming cyanobacterium Gloeotrichia echinulata. In one experiment, colonies of G.echinulata disappeared in enclosures not receiving iron, while the abundance of this species increased in those enclosures to which iron was added.

Notes: 0142-7873

English


Journal Article

Author Address: Department of Limnology, Evolutionary Biology Centre, Uppsala University, Norbyvaegen 20, S-752 36 Uppsala, Sweden
Reference Type: Journal Article

Record Number: 145

Author: Huszar, V. L. M.; Silva, L. H. S.; Marinho, M.; Domingos, P.; Sant'Anna, C. L.

Year: 2000

Title: Cyanoprokaryote assemblages in eight productive tropical Brazilian waters

Journal: Hydrobiologia

Volume: 424

Issue: 1-3

Pages: 67-77

Accession Number: AN 2000:587689

Keywords: Cylindrospermopsis; Lake waters; Microcystis; Water pollution (cyanoprokaryote assemblages in productive tropical Brazilian waters); Nitrates Role: GOC (Geological or astronomical occurrence), POL (Pollutant), OCCU (Occurrence) (cyanoprokaryote assemblages in productive tropical Brazilian waters); Lake waters (eutrophic; cyanoprokaryote assemblages in productive tropical Brazilian waters); Plankton (nanno-; cyanoprokaryote assemblages in productive tropical Brazilian waters); Lake waters (oligotrophic; cyanoprokaryote assemblages in productive tropical Brazilian waters); Plankton (pico-; cyanoprokaryote assemblages in productive tropical Brazilian waters)

cyanoprokaryote tropical Brazilian water



Abstract: Cyanoprokaryote assemblages of 8 very productive Brazilian lakes are described and the main driving forces of their dominance are considered. Relative abundance of blue-greens is shown to have been pos. related to temp., but not to pH or total P and to have been neg. assocd. with light, mixing, NO3-, but not with NH4+, total N or total N/total P ratio. Both heterocytic and non-heterocytic groups were neg. related to NO3-. However, if Cylindrospermopsis species are considered as non-N-fixing organisms (only 10% of the filaments carried heterocytes), the lakes could be considered as dominated by non-N-fixing populations during most of the years. In this new scenario, non-N-fixing were dominant in NO3- (but not NH4+) deficient lakes, and in both NO3- and NH4+ deficient conditions. Assemblages S, Sn, H, M, X1, as groups of descriptor species of systems having similar features as proposed by Reynolds, were representative of warm, shallow, turbid, enriched and frequently mixed lakes. We propose to move some species from Z (picoplankton of oligotrophic lakes) to X1 assemblage (nanoplankton of eutrophic lakes) and we comment on Microcystis species of M assemblage from mixed shallow lakes in relation to Lm assemblage of end-summer in temperate lakes. S and Sn assemblages, which comprise species which are good-light antennae, were the best represented group in these generally turbid and shallow lakes. [on SciFinder (R)]

Notes: CAN 133:271129

61-2


Water

Departamento de Botanica,Laboratorio de Ficologia, Museu Nacional, Universidade Federal do Rio de Janeiro, Quinta da Boa Vista,Rio de Janeiro,Brazil.

Journal

0018-8158



written in English.

7723-14-0 (Phosphorus); 14798-03-9 (Ammonium) Role: GOC (Geological or astronomical occurrence), POL (Pollutant), OCCU (Occurrence) (cyanoprokaryote assemblages in productive tropical Brazilian waters)



Reference Type: Journal Article

Record Number: 146

Author: Dokulil, Martin T.; Teubner, Katrin

Year: 2000

Title: Cyanobacterial dominance in lakes

Journal: Hydrobiologia

Volume: 438

Pages: 1-12

Accession Number: AN 2001:129132

Keywords: Cyanobacteria; Lake waters (causes and consequences of cyanobacteria dominance in lakes)

review cyanobacteria dominance lake water



Abstract: A review with 75 refs. concerning causes and consequences of cyanobacterial dominance in 4 ecotype lakes, including solns. to reduce eutrophication and bloom-forming cyanobacterial species, is given. Topics discussed include: causes of cyanobacterial dominance; factors affecting cyanobacterial dominance; and corrective actions. [on SciFinder (R)]

Notes: CAN 134:242074

61-0


Water

Institute of Limnology,Austrian Academy of Sciences,Mondsee,Austria.

Journal; General Review

0018-8158

written in English.

Reference Type: Book

Record Number: 147

Author: Watanabe, Y.; Drucker, V. V.

Year: 1999

Title: Phytoplankton blooms in Lake Baikal, with reference to the lake's present state of eutrophication

Series Editor: Kawanabe, H.; Coulter, G. W.; Roosevelt, A. C.

City: Ghent (Belgium)

Publisher: Kenobi Productions

ISBN: 9080434124

Accession Number: 5151374

Keywords: Freshwater lakes; Phytoplankton; Algal blooms; Eutrophic lakes;

Resource conservation; Environmental protection; Russia, Siberia,

Baykal L.

Freshwater

Q1 01481 Productivity; Q5 01523 Conservation, wildlife management

and recreation



Abstract: Lake Baikal (Russia) is the largest ancient lake in volume, containing about 20% of the Earth's surface fresh water. The water of Lake Baikal has long been considered clear, but recent observations have shown decreases in the transparency of the lake, in particular owing to phytoplankton blooms over broad areas in early spring and summer, when the lake's water is thermally stratified. Especially in summer, blooms of very small phytoplankton develop in the pelagic zone of most the lake. Additionally, massive growths of large colony-forming, nitrogen-fixing cyanobacteria such as Anabaena and Gloeotrichia, similar to those observed in highly eutrophic temperate lakes, are observed in bays into which large rivers flow. These facts suggest that the water of lake Baikal is potentially eutrophic. Because of the large amount of cold water in the hypolimnion and long retention time of the lake's water, eutrophication of Lake Baikal does not appear to be advancing rapidly. However, it is urgent to monitor the water quality of the lake and the nutrient loads from the watershed, where great social and economic changes are now taking place. The influence of eutrophication on the biological community, made up of many valuable endemic species, also has to be investigated for the protection and conservation of Lake Baikal, an invaluable natural heritage of the world .

Notes: Int. Conf. on Ancient Lakes: Their Biological and Cultural Diversities (ICAL '97), (Japan), 22-28 Jun 1997

Ancient lakes. Their cultural and biological diversity. pp. 217-225. 1999.

English

Book Monograph; Numerical data



Author Address: Department of Biology, Tokyo Metropolitan University, Minamiosawa 1-1, Hachioji, Tokyo 192-0397, Japan
Reference Type: Journal Article

Record Number: 110

Author: Vrede, Katarina; Vrede, Tobias; Isaksson, Anneli; Karlsson, Anna

Year: 1999

Title: Effects of Nutrients (Phosphorous, Nitrogen, and Carbon) and Zooplankton on Bacterioplankton and Phytoplankton-A Seasonal Study

Journal: Limnology and Oceanography

Volume: 44

Issue: 7

Pages: 1616-1624

Date: Nov.

Abstract: The effects of inorganic nutrients (P and N), organic C, and metazoan zooplankton on bacterioplankton production and abundance and on phytoplankton biomass were studied in five experiments (from May to September) in Lake Erken. In addition, the seasonal dynamics of bacterioplankton and phytoplankton were followed in the lake from April to November. Bacterioplankton production was P limited from May to August. N alone never stimulated bacterioplankton production, but bacterioplankton growth was close to colimited by P and N in July and August. Organic C stimulated bacterial production in June and September. Zooplankton enhanced bacterioplankton production in June, when bacterioplankton production was limited by P and C and the phytoplankton biomass in the lake was low. N alone stimulated phytoplankton growth in all experiments. In addition, P alone stimulated phytoplankton growth in May and July, and the combination of P and N stimulated phytoplankton growth in July and August. Zooplankton additions resulted in a decrease in phytoplankton biomass in May and September, mainly owing to grazing on Cryptophyceae. The experimental results indicate that bacterioplankton and phytoplankton growth were uncoupled during most of the open-water period because P primarily limited bacterioplankton growth and N limited phytoplankton growth. The response of the bacterioplankton community was most likely a direct effect of nutrient additions. Primary production and bacterioplankton production were correlated during the season, but partial correlations analysis indicates that this relationship can be attributed to the fact that both primary production and bacterioplankton production showed strong positive correlations with temperature. We suggest that uncoupling of bacterioplankton production and phytoplankton production may be a common phenomenon in lakes.

Notes: FLA

00243590


American Society of Limnology and Oceanography

Copyright 1999 American Society of Limnology and Oceanography



URL: http://links.jstor.org/sici?sici=0024-3590%28199911%2944%3A7%3C1616%3AEON%28NA%3E2.0.CO%3B2-K

Reference Type: Journal Article

Record Number: 19

Author: Keeley, J. E.

Year: 1999

Title: Photosynthetic Pathway Diversity in a Seasonal Pool Community

Journal: Functional Ecology

Volume: 13

Issue: 1

Pages: 106-118

Date: Feb.

Keywords: C$_3$, C$_4$, CAM, Community Assembly, Diversity, Photosynthetic Pathways

Abstract: 1. Photosynthetic pathway diversity was evaluated for the dominant species in a seasonally aquatic community in the south-western USA using $^{14}$C pulse-chase techniques. 2. Under submerged conditions, only about half of the species were clearly C$_3$, three of the 15 dominants were CAM, one species was C$_4$ and three were potentially assimilating carbon with both C$_3$ and C$_4$ fixation. 3. During the brief terrestrial stage in the life history of these amphibious plants, both the CAM and the C$_3$ + C$_4$ species switched to C$_3$, whereas the C$_4$ species did not switch. 4. Numerous variations were apparent; for example, the C$_4$ species, while exhibiting a biochemical pathway indistinguishable from terrestrial C$_4$ plants, lacked Kranz anatomy in the aquatic foliage. Also, despite well-developed CAM in several species, others exhibited low-level diel changes in acidity, apparently not indicative of CAM. 5. Species with C$_4$ or CAM CO$_2$ concentrating mechanisms lacked the capacity for bicarbonate uptake, an alternative CO$_2$ concentrating mechanism found in certain C$_3$ species in this community. 6. Rubisco/PEPC in aquatic foliage was higher in C$_3$ species than in C$_4$, CAM or putative C$_3$ + C$_4$ species. In the terrestrial phase, as expected, the switch from CAM or C$_3$ + C$_4$ to strictly C$_3$ assimilation was associated with a substantial increase in Rubisco/PEPC. Quite unexpected, however, was the substantial increase in this ratio in terrestrial C$_3$ foliage. It is hypothesized that submerged C$_3$ plants utilize PEPC for recycling of respiratory CO$_2$ and/or C$_4$ phototrophism under field conditions of limited CO$_2$ and O$_2$ saturation, and this is lost in the terrestrial foliage.

Notes: FLA

02698463


British Ecological Association

latex


Copyright 1999 British Ecological Society

URL: http://links.jstor.org/sici?sici=0269-8463%28199902%2913%3A1%3C106%3APPDIAS%3E2.0.CO%3B2-3

Reference Type: Book

Record Number: 148

Author: Karlsson, I.

Year: 1999

Title: On the germination of the akinete-forming cyanobacterium Gloeotrichia echinulata, in Lake Erken, Sweden

Series Editor: Komarek, J.; Eloranta, P.; Lhotsky, O.

City: Stuttgart (FRG)

Publisher: Schweizerbart'sche Verlagsbuchhandlung

Number of Pages: 175-180. [Arch. Hydrobiol. (Suppl.) (Algol. Stud.)]. 1999.

ISBN: 0342-1120

3510660153



Accession Number: 4728514

Keywords: Germination; Colonies; Gloeotrichia echinulata; Sweden, Erken L.

Freshwater

Q1 01204 Reproduction and development

Abstract: The potential germination of akinetes of Gloeotrichia echinulata was studied in in vitro germination experiments with akinete colonies from sediment samples collected during the spring and summer of 1998 at three different depths: 0.5, 1.5, and 4 metres. Germination in vitro occurred between April and August, with the highest germination frequency in colonies collected from the sediment of the shallowest station. The germination period in the lake occurred between the middle of June and the end of July.

Notes: 14. Symposium of the International Association for Cyanophyte Research (IAC), Lammi (Finland), 17-21 Aug 1998

Cyanobacteria/Cyanophyta, morphology, taxonomy, ecology. Proceedings of the 14th Symposium of the International Association for Cyanophyte Research (IAC). Vol. 129

Referred to also as Algological Studies 94.

English


Book Monograph; Conference

Author Address: Uppsala University, Dep. of Limnology Norbyvaegen 20, S-75236 Uppsala Sweden, [mailto:irene.karlsson@limno.uu.se]
Reference Type: Journal Article

Record Number: 149

Author: Head, R. M.; Jones, R. I.; Bailey-Watts, A. E.

Year: 1999

Title: An assessment of the influence of recruitment from the sediment on the development of planktonic populations of cyanobacteria in a temperate mesotrophic lake

Journal: Freshwater Biology

Volume: 41

Issue: 4

Pages: 759-769

Date: Jun

Accession Number: ISI:000081929600009

Keywords: akinetes; blue-green algae; cyanobacteria; migration; recruitment;

resting stages; vertical movement; trapping

microcystis-aeruginosa kutz; blue-green-algae; gloeotrichia-echinulata;

gloetrichia-echinulata; eutrophic lake; emend-elenkin; shallow lake;

phosphorus; water; aphanizomenon

Abstract: 1. A number of planktonic cyanobacteria species form resting stages that survive in the sediments of lakes. The significance of this life history strategy to the ecology of new planktonic populations was investigated in Esthwaite Water, a mesotrophic lake in the English Lake District. 2. A simple trapping technique was used to quantify vertical movements of five species of buoyant gas-vacuolate cyanobacteria from close to the sediments, along a depth transect. 3. 'Recruitment' from the sediments was found to be widespread amongst the cyanobacteria species associated with the summer phytoplankton community. 4. Estimates of the vertical upward fluxes of cyanobacteria based upon trap catches could not account for observed increases in the planktonic populations suggesting that 'recruitment' was not a significant source of biomass. 5. Vertical upward movements of Anabaena solitaria were recorded prior to this species becoming established in the plankton suggesting that benthic populations might be a source of cells for initial pelagic growth of populations of this species. 6. Low numbers of vegetative filaments of Anabaena flos-aquae, Aphanizomenon flos-aquae and Oscillatoria agardhii were observed in the plankton through the winter. These small overwintering populations appeared to be the primary source of inocula for the large summer populations of these species.

Notes: Cited References:

BARBIERO RP, 1992, FRESHWATER BIOL, V27, P249

BARBIERO RP, 1993, ARCH HYDROBIOL, V127, P87

BARBIERO RP, 1994, J PLANKTON RES, V16, P1581

FALLON RD, 1981, FRESHWATER BIOL, V11, P217

FORSELL L, 1995, MAR FRESHWATER RES, V46, P287

FOY RH, 1980, BR PHYCOL J, V15, P279

GANF GG, 1983, AUST J MAR FRESH RES, V34, P755

HANSSON LA, 1993, OECOLOGIA, V94, P286

HANSSON LA, 1994, CAN J FISH AQUAT SCI, V51, P2825

HANSSON LA, 1996, LIMNOL OCEANOGR, V41, P1312

HEAD RM, 1996, THESIS LANCASTER U L

HEAD RM, 1998, VERHANDLUNGEN INT VE, V26, P1711

HEANEY SI, 1983, BRIT PHYCOL J, V18, P47

HEANEY SI, 1986, INT REV GES HYDROBIO, V71, P441

HEANEY SI, 1992, EUROPHICATION RES AP, P199

ISTVANOVICS V, 1990, VERH INT VER LIMNOL, V24, P231

ISTVANOVICS V, 1993, J PLANKTON RES, V15, P531

JONES RI, 1979, HYDROBIOLOGIA, V62, P55

KAPPERS FI, 1976, HYDROBIOL B, V10, P164

KIRK JTO, 1994, LIGHT PHOTOSYNTHESIS

LUND JWG, 1958, HYDROBIOLOGIA, V11, P143

LUND JWG, 1959, LIMNOL OCEANOGR, V4, P57

LUND JWG, 1961, VERH INT VEREIN THEO, V14, P147

LUND JWG, 1972, TAXONOMY BIOL BLUE G, P305

LYNCH M, 1980, AM SOC LIMNOL OCEANO, V3, P299

OSGOOD RA, 1988, HYDROBIOLOGIA, V169, P69

PAERL HW, 1988, GROWTH REPROD STRATE, P261

PETTERSSON K, 1990, VERH INT VER LIMNOL, V24, P236

PETTERSSON K, 1993, HYDROBIOLOGIA, V253, P123

PRESTON T, 1980, NATURE, V288, P365

RAMSBOTTOM AE, 1976, DEPTH CHARTS CUMBRIA

REYNOLDS CS, 1972, FRESHWATER BIOL, V2, P87

REYNOLDS CS, 1973, P ROY SOC LOND B BIO, V184, P29

REYNOLDS CS, 1981, PHILOS T ROY SOC B, V293, P419

REYNOLDS CS, 1984, ECOLOGY FRESHWATER P

REYNOLDS CS, 1987, ADV BOT RES, V13, P67

ROELOFS TD, 1970, LIMNOL OCEANOGR, V15, P224

ROTHER JA, 1977, P ROY SOC LOND B BIO, V196, P317

ROTT E, 1981, SCHWEIZ Z HYDROL, V43, P34

TAKAMURA N, 1984, J PLANKTON RES, V6, P1019

TALLING JF, 1963, C PRIM PROD MEAS MAR, P142

TALLING JF, 1983, EVALUATION HIST DATA

TIKKANEN T, 1986, KASVIPLANKTONOPAS

TRIMBEE AM, 1984, J PLANKTON RES, V6, P897

TRIMBEE AM, 1988, VERH INT VER THEOR A, V23, P220

WETZEL RG, 1991, LIMNOLOGICAL ANAL

English


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