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The loss on ignition (LOI) method is cheap and simple, but is time-consuming and provides information only for specific, pre-determined temperatures. It also requires relatively large sample sizes and is destructive. Thermogravimetric analysis (TGA) is an alternative method for determination of organic and carbonate content in sediment samples, and provides accurate and precise data in a time-efficient manner. We compared results from these two thermal analysis techniques, which were applied to sediment samples from a submerged landscape (Doggerland). An organic-rich peat sample and a silty fine-sand sample were used. An unpaired t-test was used to test agreement and repeatability of the two analytical techniques. One advantage of being able to monitor mass loss throughout the analytical operation is that free and bound moisture losses can be distinguished. TGA is less time-consuming, involves automated sample handling (minimising operator error), and can yield reliable data from sample masses (typically 30–50 mg), which are much smaller than those needed for LOI (typically 3–5 g). The unpaired t-test, along with precision and repeatability analyses led us to conclude that TGA can be used instead of LOI to provide reliable measures of organic matter and carbonate content in sediments, and has several advantages over LOI.\u003C\u002Fjats:p>",{"EN":135},"Loss on ignition vs. thermogravimetric analysis: a comparative study to determine organic matter and carbonate content in sediments",{"VOID":137},"10.1007\u002Fs10933-021-00209-6","PUBLICATION","VERIFIED","Auto 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M (2005) Loss on Ignition (LOI) procedures. Standard Operating Procedures.  University of Pittsburgh, Pittsburgh",{},{"id":18,"text":269,"url":18,"identifiers":270},"Ben-Dor E, Banin A (1989) Determination of organic matter content in arid-zone soils using a simple “loss-on-ignition” method. Commun Soil Sci Plan 20:1675–1695",{"doi":271},"10.1080\u002F00103628909368175",{"id":18,"text":273,"url":18,"identifiers":274},"Bengtsson L, Enell M (1986) Chemical analysis. In: Berglund BE (ed) Handbook of holocene paleoecology and paleohydrology. Wiley, Chichester",{},{"id":18,"text":276,"url":18,"identifiers":277},"Çaylı G, Küsefoğlu S (2008) Increased yields in biodiesel production from used cooking oils by a two step process: comparison with one step process by using TGA. 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Springer, Cambridge",{},{"id":18,"text":289,"url":18,"identifiers":290},"Gaffney V, Fitch S, Bates M, Ware RL, Kinnaird T, Gearey B, Hill T, Telford R, Batt C, Stern B, Whittaker J, Davies S, Sharada MB, Everett R, Cribdon R, Kistler L, Harris S, Kearney K, Walker J, Muru M, Hamilton D, Law M, Finlay A, Bates R (2020) Allaby RG (2020) Multi-proxy characterisation of the Storegga Tsunami and its impact on the Early Holocene landscapes of the southern North Sea. Geosciences 10:270",{"doi":291},"10.3390\u002Fgeosciences10070270",{"id":18,"text":293,"url":18,"identifiers":294},"Heiri O, Lotter AF, Lemcke G (2001) Loss on ignition as a method for estimating organic and carbonate content in sediments: reproducibility and comparability of results. J Paleolimnol 25:101–110",{"doi":295},"10.1023\u002FA:1008119611481",{"id":18,"text":297,"url":18,"identifiers":298},"Hoogsteen MJJ, Lantinga EA, Bakker EJ, Groot JCJ, Tittonell PA (2015) Estimating soil organic carbon through loss on ignition: effects of ignition conditions and structural water loss. Eur J Soil Sci 66:320–328",{"doi":299},"10.1111\u002Fejss.12224",{"id":18,"text":301,"url":18,"identifiers":302},"Konare H, Yost R, Doumbia M, Mccarty G, Jarju A, Kablan R (2010) Loss on ignition: measuring soil organic carbon in soils of the Sahel. Afr J Agr Res 5:3088–3095",{},{"id":18,"text":304,"url":18,"identifiers":305},"Lopes H, Trindade T, Gulyurtlu I, Cabrita I (2001) Characterisation of FBC ashes from co-combustion of coal with oily residues. Fuel 80:785–793",{"doi":306},"10.1016\u002FS0016-2361(00)00152-6",{"id":18,"text":308,"url":18,"identifiers":309},"Miller J, Miller JC (2010) Statistics and chemometrics for analytical chemistry. Prentice Hall, New Jersey",{},{"id":18,"text":311,"url":18,"identifiers":312},"Santisteban JI, Mediavilla R, Lopez-Pamo E, Dabrio CJ, Zapata MBR, García MJG, Martínez-Alfaro CS, PE, (2004) Loss on ignition: a qualitative or quantitative method for organic matter and carbonate mineral content in sediments? J Paleolimnol 32:287–299",{"doi":313},"10.1023\u002FB:JOPL.0000042999.30131.5b",{"id":18,"text":315,"url":18,"identifiers":316},"Virkanen J, Korhola A, Tikkanen M, Blom T (1997) Recent environmental changes in a naturally acidic rocky lake in southern Finland, as reflected in its sediment geochemistry and biostratigraphy. J Paleolimnol 17:191–213",{"doi":317},"10.1023\u002FA:1007919922330",{"id":18,"text":319,"url":18,"identifiers":320},"Whitley E, Ball J (2002) Statistics review 2: Samples and populations. 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A simple, but useful, application of image analysis. J. Paleolim. 15: 111–113.",{"EN":333,"VI":334},"Public domain software has been developed for remote exposure control of a consumer digital camera for use in photomicroscopy. A computer-controlled shutter release and remote control of various camera functions are essential to avoid mechanical disturbance of the microscope and slide during the imaging procedure. These features have previously been available only with expensive professional models. The digital images of diatom specimens obtained with this system captured the same detail as conventional photographs. The setup can therefore be used as a cost-effective tool for documenting taxonomic information of microscopically small organisms. In combination with the fast data transfer rates available via the Internet, microscopical studies can now be performed faster, more reliably, and more consistently.","Phần mềm mã nguồn mở đã được phát triển để điều khiển từ xa việc phơi sáng của máy ảnh kỹ thuật số tiêu dùng sử dụng trong nhiếp ảnh vi mô. Một thiết bị điều khiển màn trập được điều khiển bằng máy tính và điều khiển từ xa các chức năng khác nhau của máy ảnh là rất cần thiết để tránh làm nhiễu loạn cơ học của kính hiển vi và phiến mẫu trong quá trình chụp hình. Những tính năng này trước đây chỉ có sẵn trên các mẫu máy ảnh chuyên nghiệp đắt đỏ. Các hình ảnh kỹ thuật số của các mẫu diatom thu được bằng hệ thống này đã nắm bắt được cùng một chi tiết như các bức ảnh truyền thống. Do đó, thiết lập này có thể được sử dụng như một công cụ tiết kiệm chi phí để tài liệu hóa thông tin phân loại của các sinh vật rất nhỏ ở mức độ vi mô. Kết hợp với tốc độ truyền dữ liệu nhanh có sẵn qua Internet, các nghiên cứu vi mô giờ đây có thể được thực hiện nhanh hơn, đáng tin cậy hơn và đồng nhất hơn.",{"EN":336,"VI":337},"Economical digital photomicroscopy","Ứng dụng kinh tế của nhiếp ảnh vi mô kỹ thuật số",{"VOID":339},"10.1023\u002FA:1011198227381",{"VI":341},"phần mềm mã nguồn mở, máy ảnh kỹ thuật số, nhiếp ảnh vi mô, điều khiển từ xa, tài liệu hóa thông tin phân loại","2025-02-06T01:34:43.524+00:00",[344],"VI","https:\u002F\u002Flink.springer.com\u002Farticle\u002F10.1023\u002FA:1011198227381",[347,364],{"id":348,"sortIndex":167,"researcher":18,"roles":349,"affiliations":351,"properties":361},"1fab4310-fc10-400d-846b-9737dfd197e2",[350],"AUTHOR",[352],{"id":18,"sortIndex":19,"affiliation":353,"properties":18},{"id":354,"createTime":355,"updateTime":355,"relativeEntities":356,"slug":357,"properties":358,"entityType":46,"verifyStatus":17,"verifyTime":18,"verifyNote":18,"syncStatus":17,"languages":18,"translateLanguages":18,"viewCount":19},"b209809b-4360-4ca4-8012-4f623da9353b","2024-04-16T02:03:38.652+00:00",[],"Department-of-Mathematical-Sciences-University-of-Alberta-Edmonton-Canada",{"title":359},{"EN":360},"Department of Mathematical Sciences University of Alberta Edmonton Canada",{"title":362},{"VI":363},"John C. 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Geochim Cosmochim Acta 61:5233–5253\nAdelson JM, Helx GR, Miller CV (2001) Reconstructing the rise of recent coastal anoxia; molybdenum in Chesapeake Bay sediments. Geochim Cosmochim Acta 65:237–252\nAlgeo TJ, Maynard JB (2004) Trace-element behavior and redox facies in core shales of Upper Pennsylvanian Kansas-type cyclotherms. Chem Geol 206:289–318\nAnderson L, Abbott MB, Finney BP, Burns SJ (2005) Regional atmospheric circulation change in the North Pacific during the Holocene inferred from lacustrine carbonate oxygen isotopes, Yukon Territory, Canada. Quaternary Res 64:21–35\nBerrang PG, Grill EV (1974) The effect of manganese oxide scavenging on molybdenum in Saanich Inlet, British Columbia. Mar Chem 2:125–148\nBorns HW Jr, Goldthwait RP (1966) Late-Pleistocene fluctuations of Kaskawulsh Glacier, southwestern Yukon Territory, Canada. Am J Sci 264:600–619\nBostock HS (1969) Kluane Lake, Yukon Territory; its drainage and allied problems. Geological Survey of Canada, Paper 69-28\nBoyle JF (2001) Inorganic geochemical methods in palaeolimnology. In: Last WM, Smol JP (eds) Tracking environmental change using lake sediments, physical and geochemical techniques, vol 2. Kluwer Academic Publishers, Dordrecht, pp 83–141\nBrahney J (2007) Paleolimnology of Kluane Lake. MSc thesis, Simon Fraser University, Burnaby, BC\nBryan ML (1972) Variations in quality and quantity of Slims River water, Yukon Territory. Can J Earth Sci 9:1469–1478\nBryan WB, Finger LW, Chayes F (1969) Estimating proportions in petrographic mixing equations by least-squares approximation. Science 163:926–927\nCalvert SE, Pedersen TF (1993) Geochemistry of recent oxic and anoxic marine sediments: implications for the geologic record. Mar Geol 113:67–88\nCampbell RB, Dodds CJ (1982) Geology, Kluane Lake map area (115F and G). Geol Surv Can Open File 829\nClague JJ (1981) Landslides at the south end of Kluane Lake, Yukon Territory. Can J Earth Sci 18:959–971\nClague JJ, Evans SG, Rampton VN, Woodsworth GJ (1995) Improved age estimates for the White River and Bridge River tephras, western Canada. Can J Earth Sci 32:1172–1179\nClague JJ, Luckman BH, Van Dorp RD, Gilbert R, Froese D, Jensen BJL, Reyes AV (2006) Rapid changes in the level of Kluane Lake in Yukon Territory over the last millennium. Quaternary Res 66:342–355\nCollins AL, Walling DE, Leeks GJL (1997) Source type ascription for fluvial suspended sediment based on a quantitative composite fingerprinting technique. Catena 29:1–27\nCollins AL, Walling DE, Leeks GJL (1998) Use of composite fingerprints to determine the provenance of the contemporary suspended sediment load transported by rivers. Earth Surf Process Landforms 23:31–52\nCrusius J, Calvert S, Pedersen T, Sage D (1996) Rhenium and molybdenum enrichments in sediments as indicators of oxic, suboxic and sulfidic conditions of deposition. Earth Planet Sci Lett 145:65–78\nDenton GH, Karlén W (1977) Holocene glacial and tree-line variations in the White River valley and Skolai Pass, Alaska and Yukon Territory. Quaternary Res 7:63–111\nDenton GH, Stuiver M (1966) Neoglacial chronology, northeastern St. Elias Mountains, Canada. Am J Sci 264:577–599\nEmerson SR, Huested SS (1991) Ocean anoxia and the concentration of molybdenum and vanadium in seawater. Mar Chem 34:177–196\nEngstrom DR, Wright HE Jr (1984) Chemical stratigraphy of lake sediments as a record of environmental change. In: Haworth EY, Lund JWG (eds) Lake sediments and environmental history, studies in paleolimnology and paleoecology, vol 11. Leicester University Press, pp 11–67\nFilippelli GM, Souch C, Menounos B, Slater-Atwater S, Jull T, Slaymaker O (2006) Alpine lake records reveal the impact of climate and rapid climate change on the biogeochemical cycling of soil nutrients. Quaternary Res 66:158–166\nGardner JS, Jones NK (1985) Evidence for a Neoglacial advance of the Boundary Glacier, Banff National Park, Alberta. Can J Earth Sci 22:1753–1755\nHelz GR, Miller CV, Charnock JM, Mosselmans JFW, Pattrick RAD, Garner CD, Vaughan DJ (1996) Mechanism of molybdenum removal from the sea and its concentration in black shales: EXAFS evidence. Geochim Cosmochim Acta 60:3631–3642\nHuerta-Diaz MG, Morse JW (1992) Pyritization of trace metals in anoxic marine sediments. Geochim Cosmochim Acta 56:2681–2702\nKelly CA, Rudd JWM, Cook RB, Schindler DW (1982) The potential importance of bacterial processes in regulating rate of lake acidification. Limnol Oceanogr 27:868–882\nKlinkhammer GP, Palmer MR (1991) Uranium in the ocean where it goes and why. Geochim Cosmochim Acta 55:1799–1806\nLewan MD, Maynard JB (1982) Factors controlling the enrichment of vanadium and nickel in the bitumen of organic sedimentary rocks. Geochim Cosmochim Acta 46:2547–2560\nMorse JW, Luther GW III (1999) Chemical influence on trace metal-sulfide interaction in anoxic sediments. Geochim Cosmochim Acta 63:3373–3378\nMosser C (1991) Relationship between sediments and their igneous source rocks using clay mineral multi-element chemistry the Cenozoic lacustrine Anloua Basin (Adamaoua, Cameroon). Chem Geol 90:319–342\nNatural Resources Canada (2003) The atlas of Canada: facts about Canada: lakes. http:\u002F\u002Fwww.atlas.gc.ca\u002Fsite\u002Fenglish\u002Flearningresources\u002Ffacts\u002Flakes.html#yukon. Accessed January 2005\nOsborn GD, Karlstrom ET (1989) Holocene moraine and paleosol stratigraphy, Bugaboo Glacier, British Columbia. Boreas 18:311–322\nOsborn G, Menounos B, Koch J, Clague J, Vallis V (2007) Multi-proxy record of Holocene glacier history of the Spearhead and Fitzsimmons ranges, southern Coast Mountains, British Columbia. Quaternary Sci Rev 26:479–493\nPienitz R, Smol JP, Last WM, Leavitt PR, Cumming BF (2000) Multi-proxy Holocene paleoclimatic record from a saline lake in the Canadian Subarctic. Holocene 10:673–686\nRampton VN, Shearer JM (1978a) Bottom and sub-bottom conditions at Kluane Lake, Teslin River, and Nisutlin Bay pipe line crossings. Terrain Analysis Mapping Serv, Stittsville\nRampton VN, Shearer JM (1978b) The geology and limnology of Kluane Lake, Yukon Territory, I preliminary assessment. Terrain Analysis Mapping Serv, Stittsville\nRoss GJ, Wang C (1993) Extractable Al, Fe, Mn and Si. In: Carter MR (ed) Soil sampling and methods of analysis for Canadian society of soil science. Lewis Publ, Boca Raton, pp 239–246\nSchlesinger WH (1997) Biogeochemistry: an analysis of global change. Academic Press, London\nTempleton GD III, Chasteen ND (1980) Vanadium fulvic acid chemistry: conformational and binding studies by electron spin probe techniques. Geochim Cosmochim Acta 44:741–752\nTribovillard N, Riboulleau A, Lyons T, Baudin F (2004) Enhanced trapping of molybdenum by sulfurized marine organic matter of marine origin in Mesozoic limestones and shales. Chem Geol 213:385–401\nWanty RB, Goldhaber MB (1992) Thermodynamics and kinetics of reactions involving vanadium in natural systems: accumulation of vanadium in sedimentary rocks. Geochim Cosmochim Acta 56:1471–1483\nWehrli B, Stumm W (1989) Vanadyl in natural waters: adsorption and hydrolysis promote oxygenation. Geochim Cosmochim Acta 53:69–77\nWood C, Smith DJ (2004) Dendroglaciological evidence for a Neoglacial advance of the Saskatchewan Glacier, Banff National Park, Canadian Rocky Mountains. Tree-Ring Res 60:59–65",{"EN":502},"The level of Kluane Lake in southwest Yukon Territory, Canada, has fluctuated tens of metres during the late Holocene. Contributions of sediment from different watersheds in the basin over the past 5,000 years were inferred from the elemental geochemistry of Kluane Lake sediment cores. Elements associated with organic material and oxyhydroxides were used to reconstruct redox fluctuations in the hypolimnion of the lake. The data reveal complex relationships between climate and river discharge during the late Holocene. A period of influx of Duke River sediment coincides with a relatively warm climate around 1,300 years BP. Discharge of Slims River into Kluane Lake occurred when Kaskawulsh Glacier advanced to the present drainage divide separating flow to the Pacific Ocean via Kaskawulsh and Alsek rivers from flow to Bering Sea via tributaries of Yukon River. During periods when neither Duke nor Slims river discharged into Kluane Lake, the level of the lake was low and stable thermal stratification developed, with anoxic and eventually euxinic conditions in the hypolimnion.",{"EN":504},"Geochemical reconstruction of late Holocene drainage and mixing in Kluane Lake, Yukon Territory",{"VOID":506},"10.1007\u002Fs10933-007-9177-z","http:\u002F\u002Flink.springer.com\u002F10.1007\u002Fs10933-007-9177-z",[509,525,541,556],{"id":510,"sortIndex":167,"researcher":18,"roles":511,"affiliations":512,"properties":522},"120a90ad-f756-41bd-a7e4-53390bb463a1",[350],[513],{"id":18,"sortIndex":19,"affiliation":514,"properties":18},{"id":515,"createTime":516,"updateTime":516,"relativeEntities":517,"slug":518,"properties":519,"entityType":46,"verifyStatus":17,"verifyTime":18,"verifyNote":18,"syncStatus":17,"languages":18,"translateLanguages":18,"viewCount":19},"4bb9c3ed-6af4-4e53-a61e-5adb1d4a6c1a","2023-11-25T11:29:24.228+00:00",[],"Department-of-Earth-Science-Simon-Fraser-University-Burnaby-Canada",{"title":520},{"VI":521},"Department of Earth Science, Simon Fraser University, Burnaby, Canada",{"title":523},{"VI":524},"John J. 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Academy of Sciences of the USSR Publishers, Moscow. (English translation 1988: Freshwater Ostracoda—Fauna of the USSR: Crustaceans, vol. II, No.1. AA Balkema, Rotterdam)\nBroodbaker NW (1983) The subfamily Candoninae (Crustacea, Ostracoda) in the West Indies. Bijdr Dierk 53:287–326\nBuday T (1962) Neogén Turčianské kotliny [Neogeneof the TuriecDepression]. Sbornik Ústředního Ústavu geologického 28:475–498 (in Czech with English abstract)\nCarbonnel G (1969) Les Ostracodes du Miocène rhodanien; Systématique, biostratigraphie, écologie, paléobiologie. Docum Lab Géol Fac Sci Lyon 32:1–469\nCarbonnel G, Weidmann M, Berger JP (1985) Les ostracodes lacustres et saumâtres de la molasse de Suisse occidentale. Rev Paléobiol 4(2):215–251\nDanielopol DL (1980) On the carapace shape of some European freshwater interstitial Candoninae (Ostracoda). Proc Biol Soc Washington 93:743–756\nFreels D (1980) Limnische Ostrakoden aus Jungtertiär und Quartär der Türkei. Geol Jb B 39:3–169\nFuhrmann R (1991) Ostrakoden aus den Holstein-Intergalzialbecken Wildschütz und Dahlen (Sachsen). Z Geol Wiss 19:269–288\nGašparík J, Brestenská E, Forgáč J, Franko O, Hajošová M, Hanáček J, Marková M, Matkulčík E, Planderová E, Sitár V (1974) Štruktúrny vrt GHŠ-1 (Horná Štubňa) [Structural core GHŠ-1 (Horná Štubňa)]. Region Geol Západ Karpát 3:1–97 (in Slovak)\nGašparík J, Halouzka R, Miko O, Gorek J, Rakús M, Bujnovský A, Lexa J, Panáček A, Samuel O, Gašparíková V, Planderová E, Snopková P, Fendek M, Hanáček J, Modlitba I, Klukanová A, Žáková E, Horniš J, Ondrejičková A (1995) Vysvetlivky ku geologickej mape Turčianskej kotliny 1:50000 [Explanations to geological map 1:50000 of the Turiec Depression]. Geologický ústav Dionýza Štúra, Bratislava (in Slovak)\nGierlowski-Kordesch EH, Jacobson AD, Blum JD, Valero Garces BL (2008) Watershed reconstruction of a Paleocene-Eocene lake basin using Sr isotopes in carbonate rocks. Geol Soc Am Bull 120:85–95\nGorthner A (1994) What is an ancient lake? In: Martens K, Goddeeris B, Coulter G (eds) Speciation in ancient lakes. Arch Hydrobiol Beih Ergebn Limnol 44:97–100\nHók J, Kováč M, Rakús M, Kováč P, Nagy A, Kováčová-Slamková M, Sitár V, Šujan M (1998) Geologic and tectonic evolution of the Turiec depression in the Neogene. Slovak Geol Mag 4:165–176\nJanz H (1997) Die Ostrakoden der kleini-Schichten des miozänen Kratersees von Steinheim am Albuch (Süddeutschland). Stuttgarter Beitr Naturk B (Geologie und Paläontologie) 251:1–101\nJanz H, Vennemann TW (2005) Isotopic composition (O, C, Sr, and Nd) and trace element ratios (Sr\u002FCa, Mg\u002FCa) of Miocene marine and brackish ostracods from North Alpine Foreland deposits (Germany and Austria) as indicators for palaeoclimate. Palaeogeogr Palaeoclimatol Palaeoecol 225:216–247\nJiříček R (1985) Die Ostracoden des Pannonien. In: Papp A (ed) Chronostratigraphie und Neostratotypen, Miozän der Zentral Paratethys, Bd. VII, M6 Pannonien (Slavonien und Serbien). Akadémiai Kiado Budapest, pp 378\nKheil J (1968) Význam rodu Mediocypris (Ostracoda) pro stratigrafii miocénu Evropy a Asie [Significance of the genus Mediocypris for Miocene stratigraphy of the Europe and Asia]. Věstník Ústředního ústavu geologického 43:23–36 (in Czech)\nKonečný V, Lexa J, Planderová E (1983) Stratigrafické členenie neovulkanitov stredného Slovenska [Stratigraphy of the Central Slovakia Volcanic Field]. Západ Karpaty, Geol 9:1–203 (in Slovak with English abstract)\nKováč M (2000) Geodynamický, paleogeografický a štruktúrny vývoj karpatsko-panónskeho regiónu v miocéne: Nový pohľad na neogénne panvy Slovenska [Miocene geodynamic, paleogeographic and tectonic evolution of the Carpatho-Pannonian region: new inside to Neogene basins of Slovakia]. VEDA, Bratislava (in Slovak)\nKováč P, Hók J (1993) The central Slovakia fault system—field evidence of a strike slipe. Geol Carpath 44:155–159\nKrál’ J, Zielinski G, Fordinál K (1995) 87 Sr\u002F86Sr in three mollusc shells from the tertiary rocks of the Western Carpathians. Mineralia Slov 27:365–374 (in Slovak with English abstract)\nKrstić N (1972) Rod Candona (Ostracoda) iz kongerijskikh slojeva juzhnog dela Panonskog basena [Genus Candona (Ostracoda) from Congeria beds of Southern Pannonian Basin]. Serbian Acad Sci Arts Monogr 450:1–145 (in Serbian with English abstract)\nKrstić N (1995a) Ostracodes of lower and middle Paludinian beds of Fruska Gora s.l. In: Marinescu Fl, Papaianopol I (eds) Chronostratigraphie und Neostratotypen—Neogene der Zentrale Paratethys, Bd. IX, Dacien Pl1. Rumänische Akademie, Bucarest, pp 387–427\nKrstić N (1995b) A new Cyclocypris subgenus—Laevicypris. In: Říha J (ed) Ostracoda and Biostatigraphy. Proceedings of the 12 international symposium on Ostracoda. AA Balkema, Rotterdam Brookfield, pp 37–42\nMalz H, Moayedpour E (1973) Miozäne Süßwasser-Ostracoden aus der Rhön. Senck leth 54:281–309\nMandelstam MI, Schneider GF (1963) Iskopaemye ostrakody SSSR, semejstvo Cyprididae [Fossil ostracods of the USSR, family Cyprididae]. Trudy VNIGRI 203:1–242 (in Russian)\nMarmonier P, Meisch C, Danielopol DL (1989) A review of the genus Cavernocypris Hartmann (Ostracoda, Cypridopsinae): systematics, ecology and biogeography. Bull Soc Nat Luxembourg 89:221–278\nMartens K (1994) Ostracod speciation in ancient lakes: a review. In: Martens K, Goddeeris B, Coulter G (eds) Speciation in ancient lakes. Arch Hydrobiol Beih Ergebn Limnol 44:203–222\nMartens K (1997) Speciation in ancient lakes. Trends Ecol Evol 12:177–182\nMartens K, Coulter G, Goddeeris B (1994) Speciation in Ancient lakes—40 years after Brooks. In: Martens K, Goddeeris B, Coulter G (eds) Speciation in ancient lakes. Arch Hydrobiol Beih Ergebn Limnol 44:75–96\nMartens K, Rossetti G, Fuhrmann R (1997) Pleistocene and Recent species of the family Darwinulidae Brady & Norman, 1889 (Crustacea, Ostracoda) in Europe. Hydrobiol 357:99–116\nMcArthur JM (1994) Recent trends in strontium isotope stratigraphy. Terra Nova 6:331–358\nMcArthur JM, Howarth RJ, Bailey TR (2001) Strontium isotope stratigraphy: LOWESS Version 3: best fit to the marine Sr-isotope curve for 0–509 Ma and accompanying look-up table for deriving numerical age. J Geol 109:155–169\nMeisch C (2000) Freshwater Ostracoda of Western and Central Europe. Spektrum Akademischer Verlag, Heidelberg, Berlin\nMikulić F (1961) Neue Arten Candona aus dem Ohridsee. Bull Mus Hist Nat B 17:87–108 (in Serbian with German abstract)\nMostafawi N (1994) Süßwasser-Ostracoden aus dem Ober-Pliozän von N-Euböa (Griechland). Neues Jahrb Geol P-M 5:309–319\nMostafawi N (1996) Neogene Ostracodenfaunen im Gebiet südlich von Thessaloniki (Nordgriechenland). Senck Leth 76:159–173\nNemčok M, Lexa J (1990) Evolution of the basin and range Structure around the Žiar Mountain range. Geol Zbor Geol Carpath 41:229–258\nNemčok M, Hók J, Kováč P, Marko F, Coward MP, Madarás J, Houghton JJ, Bezák V (1998) Tertiary development and extension\u002Fcompression interplay in the West Carpathians mountain belt. Tectonophysics 290:137–167\nPin C, Bassin C (1992) Evaluation of a strontium-specific extraction chromatographic method for isotopic analysis in geological materials. Anal Chim Acta 269:249–255\nPipík R (2001) Les Ostracodes d’un lac ancien et ses paléobiotopes au Miocène supérieur: le Bassin de Turiec (Slovaquie). Thesis, Université Claude-Bernard, Lyon I\nPipík R (2004) Sladkovodné lastúrničky (Ostracoda) a vrchnomiocénne paleobiotopy severnej časti Tučianskej kotliny [Freshwater ostracods (Ostracoda) and Upper Miocene paleobiotopes of the northern part of the Turiec Depression (Slovakia)]. Mineralia Slov 36:87–100 (in Slovak with English abstract)\nPipík R (2005) Vrchnomiocénne sladkovodné lastúrničky (Ostracoda) okrajových sedimentov turčianskeho súvrstvia [Upper Miocene freshwater ostracods (Ostracoda) of the littoral deposits of the Turiec Formation]. Mineralia Slov 37:27–40 (in Slovak with English abstract)\nPipík R, Bodergat AM (2003a) Ostracodes du Miocène supérieur du Bassin de Turiec (Slovaquie): familles Darwinulidae et Ilyocyprididae. Rev Esp Micropaleont 35:345–355\nPipík R, Bodergat AM (2003b) Upper Miocene Ostracods of the Turiec Basin (Slovakia)—sub-family Cyclocypridinae. Ann Limnol-Int J Lim 39:347–361\nPipík R, Bodergat AM (2004a) Cyprididae (Ostracoda) du Miocène supérieur du Bassin de Turiec (Slovaquie): Taxonomie et Paléoécologie. Rev Micropaléont 47:225–242\nPipík R, Bodergat AM (2004b) Euxinocythere (Ostracoda, Cytheridae, Leptocytherinae) du Miocène supérieur du Bassin de Turiec (Slovaquie): taxonomie et paléoécologie. Rev Micropaléont 47:36–52\nPipík R, Bodergat AM (2006) Groupe de Candona clivosa, nouveau groupe de Candoninae (Crustacea, Ostracoda) et sa diversification dans le Bassin de Turiec (Slovaquie) au Miocène supérieur. Géobios 39:394–414\nPipík R, Bodergat AM (2007) Candoninae trapézoïdales (Crustacea, Ostracoda) du Bassin de Turiec (Slovaquie) du Miocène supérieur—systématique, écologie et évolution. Géobios 40:645–676\nPipík R, Bodergat AM (2008) Nouvelle faune d’ostracodes d’eau douce du Miocène supérieur de la Paratéthys Centrale et description d’espèces appartenant aux genres Pseudocandona, Fabaeformiscandona et Candonopsis. Palaeontogr Abt A 286:89–121\nPipík R, Fordinál K, Slamková M, Starek D, Chalupová B (2004) Annotated checklist of the Pannonian microflora, evertebrate and vertebrate community from Studienka, Vienna Basin. Scripta Fac Sci Nat Univ Masaryk Brun Geol 31–32:47–54\nPokorný V (1954) Paleontologický výzkum neogenních vrstev v oblasti Sučany—Kl'ačany (Paleontological investigation of the Neogene deposits in vicinity of Sučany—Kl'ačany). Věstnik Ústředního ústavu geologického 29:81–84 (in Czech)\nRakús M, Hók J, Král’ J, Kotulová J (2005) The Turčianska kotlina depression an example of the strike-slipe basin. Geolines 19:97–98\nSemhi K, Clauer N, Probst JL (2000) Strontium isotope compositions of river waters as records of lithology-dependent mass transfers: the Garonne river and its tributaries (SW France). Chem Geol 168:173–193\nShapkarev JA (1980) Composition and variation of the bottom fauna in the sublittoral of the eutrophic lake Doiran (Macedonia, Yugoslavia). In: Dokulil M, Metz H, Jewson D (eds) Developments in Hydrobiology 3—Shallow lakes, Contribution to their Limnology. Dr. W. Junk Bv Publishers, The Hague Boston London, pp 195–201\nSitár V (1969) Die Paläoflora des Turiec-Beckens und ihre Beziehung zu den Mitteleuropäischen Floren. Acta Geol Geogr Univ Comenianae Geol 17:191–206\nStanković S (1960) The Balkan Lake Ohrid and its living world. Uitgeverij Dr. W. Junk, Den Haag\nStraub EW (1952) Mikropaläontologische Untersuchungen im Tertiär zwischen Ehingen und Ulm a.d. Donau. Geol Jb 66:433–524\nWitt W (2000) Süßwasserostracoden der miozänen Vorlandmolasse Süddeutschland. Mitt Bayer Staatsslg Paläont hist Geol 40:109–151\nZbořil L, Šefara J, Halmešová S, Král’ M, Puchnerová M, Stránska M, Szalaiová V (1985) Geofyzikálny výskum Turčianskej kotliny [Geophysical research of the Turiec Depression]. Manuscript, Geofond Bratislava (in Slovak)",{"EN":613},"The Turiec Basin (TB) of Slovakia formed in the Miocene when the West Carpathians escaped from the Alpine region. The 1,250-m-thick sedimentary Neogene fill of the basin preserved fossil leaves as well as endemic bivalves, gastropods, and ostracodes. The paleolimnologic changes recorded in the TB infill were derived from the most abundant fossils, the ostracodes. Five contemporaneous ostracode assemblages within the Late Miocene lacustrine system were distinguished through statistical analysis. These assemblages have low species similarity, between 2.1 and 24.1%, and are recognized by shape differences among the Candoninae. The ostracode assemblages, mollusca fossils, and Sr-isotope ratios suggest a low-salinity environment at the beginning of the Late Miocene, during a brief connection with the Central Paratethys. When the connection ceased, the basin became an isolated freshwater lake, with five zones differentiated ecologically and bathymetrically using the ostracode assemblages. Taxonomic comparison of the faunas of the TB and the freshwater to brackish Neogene basins of Europe demonstrates the endemic character of the TB ostracode fauna. The biologic characteristics of the ostracode families, along with the geology of the lake basin, suggest that the longevity of the Late Miocene lake probably exceeded 1 Ma.",{"EN":615},"Physical and biological properties of the late Miocene, long-lived Turiec Basin, Western Carpathians (Slovakia) and its 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Pipík",{"id":636,"sortIndex":147,"researcher":18,"roles":637,"affiliations":638,"properties":647},"b3f92cd1-7c8a-4c64-a901-a49452401825",[350],[639],{"id":18,"sortIndex":19,"affiliation":640,"properties":18},{"id":641,"createTime":642,"updateTime":642,"relativeEntities":643,"slug":18,"properties":644,"entityType":46,"verifyStatus":17,"verifyTime":18,"verifyNote":18,"syncStatus":17,"languages":18,"translateLanguages":18,"viewCount":19},"55a0ba81-6359-4785-a1bf-e050d9bb2880","2024-02-11T17:53:04.858+00:00",[],{"title":645},{"VI":646},"Université Blaise Pascal Clermont-Ferrand II, UMR 6524 “Laboratoire Magmas et Volcans”, Clermont-Ferrand Cedex, France",{"title":648},{"VI":649},"Danielle Briot",{"id":651,"sortIndex":167,"researcher":18,"roles":652,"affiliations":653,"properties":672},"f3d5135a-9736-42c0-8f47-e8522c2190b7",[350],[654,662],{"id":18,"sortIndex":19,"affiliation":655,"properties":18},{"id":656,"createTime":657,"updateTime":657,"relativeEntities":658,"slug":18,"properties":659,"entityType":46,"verifyStatus":17,"verifyTime":18,"verifyNote":18,"syncStatus":17,"languages":18,"translateLanguages":18,"viewCount":19},"54271c20-486d-4ccf-8c78-4f3c573851a1","2024-02-11T17:53:04.835+00:00",[],{"title":660},{"VI":661},"UMR 5125 PEPS CNRS, Villeurbanne Cedex, France",{"id":663,"sortIndex":167,"affiliation":664,"properties":671},"ca62c9ab-8e55-4721-b309-d6834edda17a",{"id":665,"createTime":666,"updateTime":666,"relativeEntities":667,"slug":18,"properties":668,"entityType":46,"verifyStatus":17,"verifyTime":18,"verifyNote":18,"syncStatus":17,"languages":18,"translateLanguages":18,"viewCount":19},"aeb8dac9-fc2c-471f-b841-671dd1a40419","2024-02-11T17:53:04.841+00:00",[],{"title":669},{"VI":670},"Université Lyon 1, Laboratoire de Géologie de Lyon Terre, Planètes, Environnement, Villeurbanne, France",{},{"title":673},{"VI":674},"Anne-Marie Bodergat",{"id":676,"sortIndex":107,"researcher":18,"roles":677,"affiliations":678,"properties":687},"e87b5984-7860-451e-9876-71a4f33fb6b3",[350],[679],{"id":18,"sortIndex":19,"affiliation":680,"properties":18},{"id":681,"createTime":682,"updateTime":682,"relativeEntities":683,"slug":18,"properties":684,"entityType":46,"verifyStatus":17,"verifyTime":18,"verifyNote":18,"syncStatus":17,"languages":18,"translateLanguages":18,"viewCount":19},"fea58685-6fc9-4b27-b81d-9843a8aeb81a","2024-02-11T17:53:04.875+00:00",[],{"title":685},{"VI":686},"Department of Geology and Paleontology, Comenius University, Bratislava, Slovak Republic",{"title":688},{"VI":689},"Michal 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Zielinski",{"id":708,"sortIndex":709,"researcher":18,"roles":710,"affiliations":711,"properties":720},"0b23a5ea-389e-4c97-b73d-426d458961bb",4,[350],[712],{"id":18,"sortIndex":19,"affiliation":713,"properties":18},{"id":714,"createTime":715,"updateTime":715,"relativeEntities":716,"slug":18,"properties":717,"entityType":46,"verifyStatus":17,"verifyTime":18,"verifyNote":18,"syncStatus":17,"languages":18,"translateLanguages":18,"viewCount":19},"acd3330e-1884-4840-b773-c8e2f2eef1cc","2023-12-13T23:41:44.124+00:00",[],{"title":718},{"VI":719},"State Geological Institute of Dionýz Štúr, Bratislava, Slovak Republic",{"title":721},{"VI":722},"Ján Král’",{"url":618,"publisher":724,"properties":751},{"id":6,"createTime":7,"updateTime":8,"relativeEntities":725,"slug":10,"properties":726,"entityType":16,"verifyStatus":17,"verifyTime":18,"verifyNote":18,"syncStatus":17,"languages":18,"translateLanguages":18,"viewCount":19,"subjectFields":729,"manageAffiliations":730,"indexDatabases":731,"url":18,"thumbnailPath":18,"statistic":746,"gsStatistic":18,"type":18,"analyzePriority":18},[],{"issn":727,"title":728},{"VOID":13},{"EN":15},[],[],[732,739],{"id":62,"indexDatabase":733,"url":77,"indexYears":18,"academicFieldIds":738,"indexDatabaseRanking":18},{"id":64,"createTime":65,"updateTime":66,"relativeEntities":734,"label":735,"description":736,"key":73,"publicationTags":737,"standard":18},[],{"EN":69,"VI":69},{"VI":71,"EN":72},[75,76],[79,80,81],{"id":83,"indexDatabase":740,"url":96,"indexYears":97,"academicFieldIds":745,"indexDatabaseRanking":101},{"id":85,"createTime":86,"updateTime":87,"relativeEntities":741,"label":742,"description":743,"key":93,"publicationTags":744,"standard":18},[],{"EN":90,"VI":90},{"EN":90,"VI":92},[95],[99,100],{"impactFactor":19,"impactFactorByYear":747,"i10Index":104,"i10IndexLast5Year":19,"totalPublication":105,"totalPublicationByYear":748,"totalCitation":108,"totalCitationByYear":749,"totalCitationPerPublication":112,"totalCitationPerPublicationByYear":750,"hindexLast5Year":104,"hindex":104},{},{"2003":107,"2004":104},{"2003":110,"2004":111},{"2003":114,"2004":115},{"volume":752,"pages":754},{"VOID":753},"47",{"VOID":755},"233-249","2011-12-27",2011,{"id":759,"createTime":760,"updateTime":761,"relativeEntities":762,"slug":763,"properties":764,"entityType":138,"verifyStatus":139,"verifyTime":761,"verifyNote":140,"syncStatus":17,"languages":18,"translateLanguages":18,"viewCount":19,"primaryUrl":769,"fullTextUrl":18,"authors":770,"publicationType":221,"publisherRelationship":786,"citationCount":18,"citationInfo":18,"publishDate":819,"publishYear":820,"citationAnalyzeStatus":17,"lastCitationAnalyze":18,"indexDatabases":18,"openAccess":18,"references":18,"isForceReanalyzing":322},"754a119c-2cf9-468f-82cd-1ed8e5e5c6f8","2023-12-27T14:35:18.959+00:00","2024-10-22T23:57:04.100+00:00",[],"Paleoclimatology-Reconstructing-Cimates-of-the-Quaternary-R-S-Bradley",{"title":765,"doi":767},{"EN":766},"Paleoclimatology - Reconstructing Cimates of the Quaternary. R.S. Bradley",{"VOID":768},"10.1023\u002FA:1008107127646","https:\u002F\u002Flink.springer.com\u002Farticle\u002F10.1023\u002FA:1008107127646",[771],{"id":772,"sortIndex":19,"researcher":18,"roles":773,"affiliations":774,"properties":783},"b5c241a1-3fff-455e-b2ec-aa51b77f2afd",[350],[775],{"id":18,"sortIndex":19,"affiliation":776,"properties":18},{"id":777,"createTime":778,"updateTime":778,"relativeEntities":779,"slug":18,"properties":780,"entityType":46,"verifyStatus":17,"verifyTime":18,"verifyNote":18,"syncStatus":17,"languages":18,"translateLanguages":18,"viewCount":19},"6c872cd9-d8b5-4415-9335-f38c249bde5d","2023-12-27T14:35:19.081+00:00",[],{"title":781},{"VI":782},"Quaternary Environments Research Group, Department of Geographical Sciences, University of Plymouth, Drake Circus, Plymouth, Devon",{"title":784},{"VI":785},"Neil Roberts",{"url":769,"publisher":787,"properties":814},{"id":6,"createTime":7,"updateTime":8,"relativeEntities":788,"slug":10,"properties":789,"entityType":16,"verifyStatus":17,"verifyTime":18,"verifyNote":18,"syncStatus":17,"languages":18,"translateLanguages":18,"viewCount":19,"subjectFields":792,"manageAffiliations":793,"indexDatabases":794,"url":18,"thumbnailPath":18,"statistic":809,"gsStatistic":18,"type":18,"analyzePriority":18},[],{"issn":790,"title":791},{"VOID":13},{"EN":15},[],[],[795,802],{"id":62,"indexDatabase":796,"url":77,"indexYears":18,"academicFieldIds":801,"indexDatabaseRanking":18},{"id":64,"createTime":65,"updateTime":66,"relativeEntities":797,"label":798,"description":799,"key":73,"publicationTags":800,"standard":18},[],{"EN":69,"VI":69},{"VI":71,"EN":72},[75,76],[79,80,81],{"id":83,"indexDatabase":803,"url":96,"indexYears":97,"academicFieldIds":808,"indexDatabaseRanking":101},{"id":85,"createTime":86,"updateTime":87,"relativeEntities":804,"label":805,"description":806,"key":93,"publicationTags":807,"standard":18},[],{"EN":90,"VI":90},{"EN":90,"VI":92},[95],[99,100],{"impactFactor":19,"impactFactorByYear":810,"i10Index":104,"i10IndexLast5Year":19,"totalPublication":105,"totalPublicationByYear":811,"totalCitation":108,"totalCitationByYear":812,"totalCitationPerPublication":112,"totalCitationPerPublicationByYear":813,"hindexLast5Year":104,"hindex":104},{},{"2003":107,"2004":104},{"2003":110,"2004":111},{"2003":114,"2004":115},{"volume":815,"pages":817},{"VOID":816},"23",{"VOID":818},"455-456","2000-04-01",2000,{"id":822,"createTime":823,"updateTime":824,"relativeEntities":825,"slug":826,"properties":827,"entityType":138,"verifyStatus":139,"verifyTime":838,"verifyNote":140,"syncStatus":17,"languages":18,"translateLanguages":18,"viewCount":19,"primaryUrl":839,"fullTextUrl":18,"authors":840,"publicationType":221,"publisherRelationship":856,"citationCount":18,"citationInfo":18,"publishDate":889,"publishYear":890,"citationAnalyzeStatus":891,"lastCitationAnalyze":892,"indexDatabases":18,"openAccess":18,"references":18,"isForceReanalyzing":322},"d5978f68-2c52-41d8-810f-97acb30dd514","2024-01-12T10:13:08.835+00:00","2026-05-05T23:56:59.788+00:00",[],"The-misrepresentation-of-the-planktonic-diatom-assemblage-in-traps-and-sediments-southern-Lake-Mala%C5%B5i-Africa",{"references":828,"abstract":830,"title":832,"doi":834,"gsPaper":836},{"VOID":829},"BattarbeeR. W., 1981. Changes in the diatom microflora of a eutrophic lake since 1900 from a comparison of old algal samples and the sedimentary record. Holarc. Ecol. 4: 73–81.\nBeadleL. C., 1981. The inland waters of tropical Africa. 2ed. Longman, New York. 475 pp.\nBeauchampR. S. A., 1953. Hydrological data from Lake Nyasa. J. Ecol. 41: 226–239.\nBeauchampR. S. A., 1964. The rift valley lakes of Africa. Verh. int. Ver. Limnol. 15: 91–99.\nBloeschJ. & N. M.Burns, 1980. A critical review of sediment trap technique. Schweiz. Z. Hydrobiol. 42: 15–55.\nBlomqvistS. & L.Hakanson, 1981. A review on sediment traps in aquatic environments. Arch. Hydrobiol. 91: 101–132.\nBonnyA. P., 1976. Recruitment of pollen to the seston and sediment of some English Lake District lakes. J. Ecol. 64: 859–887.\nDavisM. B., 1963. On the theory of pollen analysis. Amer. J. Sci. 261: 897–912.\nDavisM. B. & L. B.Brubaker, 1973. Differential sedimentation of pollen grains in lakes. Limnol. Oceanogr. 18: 635–646.\nEcclesD. H., 1974. An outline of the physical limnology of Lake Malaŵi (Lake Nyasa). Limnol. Oceanogr. 19: 730–742.\nEppleyR. W., 1977. The growth and culture of diatoms. In WernerD. (ed), The Biology of Diatoms. University of California Press, Berkeley. 498 pp.\nFaegriK. & J.Iverson 1975. Textbook of pollen analysis. 3ed. Monksgaard, Copenhagen, 295 pp.\nFerranteJ. G. & J. I.Parker, 1978. The influence of planktonic and benthic crustaceans on silicon cycling in Lake Michigan, USA. Verh. int. Ver. Limnol. 20: 324–328.\nGardnerW. D., 1980. Field assessment of sediment traps. J. Mar. Res. 38: 41–52.\nHaberyanK. A., 1985 The role of copepod fecal pellets in the deposition of diatoms in Lake Tanganyika. Limnol. Oceanogr. 30: 1010–1023.\nHaberyan, K. A., 1988. Phycology, sedimentology, and paleolimnology near Cape Maclear, Lake Malaŵi, Africa. Ph. D dissertation, Duke University, Durham, N. C. 246 pp.\nHaberyan, K. A. & O. K. Mhone, submitted. Observations on the algae near Cape Maclear, southern Lake Malaŵi, Africa. 21 ms pp., 6 tab., 6 fig. Submitted to Limnol. Oceanogr., December 1988.\nHaworthE. Y., 1976. The changes in the composition of the diatom assemblages found in the surface sediments of Blelham Tarn in the English Lake District during 1973. Ann. Bot. 40: 1195–1205.\nHaworthE. Y., 1980. Comparison of continuous phytoplankton records with the diatom stratigraphy in the recent sediments of Blelham Tarn. Limnol. oceanogr. 25: 1093–1103.\nHeckyR. E. & H. J.Kling, 1987. Phytoplankton ecology of the great lakes in the rift valleys of central Africa. Arch. Hydrobiol. Beih. Ergebn. Limnol. 25: 197–228.\nHonjoS., 1976. Coccoliths: production, transportation, and sedimentation. Mar. Micropaleontol. 1: 65–79.\nHustedtF., 1949. Susswässer diatomeen. In Exploration du Parc National Albert, Mission 2, fasc. 8. Institute des Parcs Nationaux du Congo Belge, Brussels, 199 pp.\nHutschinsonG. E., 1957. A treatise on limnology, v. 1(1). The geography and physics of lakes. Wiley, New York. 540 pp.\nJohnsonT. C. & R. E.Hecky, 1988. A silica budget for Lake Malaŵi: net fluvial input, biogenic opal preservation and burial. Eos 69: 1144 (abstract).\nOwen, R. B., R. Crossley, T. C. Johnson, S. Davidson-Hirschmann, D. Tweddle, D. Eccles & D. E. Engstrom, in prep. Major low levels of Lake Malawi and implications for evolution rates in cichlid fishes. 24 ms pp.\nPorterK. G., 1973. Selective grazing and differential digestion of algae by zooplankton. Nature 244: 179–180.\nSchraderH. J., 1971. Fecal pellets: role in sedimentation of pelagic diatoms. Science 174: 55–57.\nSimolaH., 1977. Diatom succession in the formation of annually laminated sediment in Lovojärvi, a small eutrophicated lake. Ann. Bot. Fennici 14: 143–148.\nVanMeelL., 1954. Le phytoplancton. In Exploration Hydrobiologique du Lac Tanganyika, vol. 4(1). Institute Royal des Sciences Naturelles de Belgique, Brussels. 680 pp.",{"EN":831},"Sediment trap collections near Cape Maclear, Lake Malaŵi, were compared to phytoplankton and surface sediment diatoms to assess taphonomic variations. The sedimenting diatom community became progressively different from the diatom plankton with increasing depth: long Nitzschia species were strongly under-represented in the traps (annually, 53% among planktonic diatoms vs. 14% in the offshore 29 m trap; p≪0.005 by Kruskal-Wallis test), while Melosira was greatly over-represented in traps (32% vs. 57%; p\u003C0.005). The abundances of the minor taxa (Rhopalodia, Fragilaria, Cymbella, and Surirella) were greatly enhanced in traps relative to the plankton, but they were still relatively uncommon (\u003C3% of all diatoms each). Differences in grazing, dissolution, and sinking rates alone are insufficient to account for these distortions; a combination of these, plus perhaps unknown factors, strongly influence the deposited assemblage. These misrepresentations were also present at the sediment surface. The greatest discrepancy was noted for Melosira (32% of plankton vs. 53% of sediment surface diatoms; p\u003C0.005) and for elongate Nitzschia species (53% of plankton vs. 0.8% in sediments; p\u003C0.005). In Lake Malaŵi, at least, paleolimnologists must not assume a straightforward correlation of modern and fossil assemblages.",{"EN":833},"The misrepresentation of the planktonic diatom assemblage in traps and sediments: southern Lake Malaŵi, Africa",{"VOID":835},"10.1007\u002FBF00209298",{"VOID":837},"[]","2024-06-24T13:36:36.720+00:00","https:\u002F\u002Flink.springer.com\u002Farticle\u002F10.1007\u002FBF00209298",[841],{"id":842,"sortIndex":19,"researcher":18,"roles":843,"affiliations":844,"properties":853},"b4a28d92-0535-4237-9d18-9f494a869003",[350],[845],{"id":18,"sortIndex":19,"affiliation":846,"properties":18},{"id":847,"createTime":848,"updateTime":848,"relativeEntities":849,"slug":18,"properties":850,"entityType":46,"verifyStatus":17,"verifyTime":18,"verifyNote":18,"syncStatus":17,"languages":18,"translateLanguages":18,"viewCount":19},"fbc80bd3-dd80-406d-8d6a-f90df44958cb","2024-02-15T06:06:36.872+00:00",[],{"title":851},{"VI":852},"Department of Zoology, Duke University, Durham, USA",{"title":854},{"VI":855},"Kurt A. 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Limnol Oceanogr 18:647–653",{"doi":1031},"10.4319\u002Flo.1973.18.4.0647",{"id":18,"text":1033,"url":18,"identifiers":1034},"Birks HJB (2010) Numerical methods for the analysis of diatom assemblage data. In: Smol JP, Stoermer EF (eds) The diatoms: applications for environmental and earth sciences. Cambridge University press, Cambridge, pp 23–54",{"doi":1035},"10.1017\u002FCBO9780511763175.004",{"id":18,"text":1037,"url":18,"identifiers":1038},"Blaauw M (2010) Methods and code for ‘classical’ age-modelling of radiocarbon sequences. Quat Geochronol 5:512–518",{"doi":1039},"10.1016\u002Fj.quageo.2010.01.002",{"id":18,"text":1041,"url":18,"identifiers":1042},"Bradbury JP (2000) Limnologic history of Lago de Pátzcuaro, Michoacán, Mexico for the past 48, 000 years: impacts of climate and man. Palaeogeogr Palaeoclimatol Palaeoecol 163:69–95",{"doi":1043},"10.1016\u002FS0031-0182(00)00146-2",{"id":18,"text":1045,"url":18,"identifiers":1046},"Camburn KE, Charles DF (2000) Diatoms of low-alkalinity lakes in the Northeastern United States. Academy of Natural Sciences of Philadelphia, Philadelphia",{},{"id":18,"text":1048,"url":18,"identifiers":1049},"Cremer H, Wagner B, Melles M, Hubberten HW (2001) The postglacial environmental development of Raffles Sø, East Greenland: inferences from a 10, 000 year diatom record. J Paleolimnol 26:67–87",{"doi":1050},"10.1023\u002FA:1011179321529",{"id":18,"text":1052,"url":18,"identifiers":1053},"Cremer H, Sangiorgi F, Wagner-Cremer F, McGee V, Lotter AF, Visscher H (2007) Diatoms (Bacillariophyceae) and Dinoflagellate Cysts (Dinophyceae) from Rookery Bay, Florida, USA. 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Kluwer Academic Publishers, Dordrecht, pp 203–223",{},{"id":1226,"createTime":1227,"updateTime":1227,"relativeEntities":1228,"slug":1229,"properties":1230,"entityType":138,"verifyStatus":17,"verifyTime":18,"verifyNote":18,"syncStatus":17,"languages":1239,"translateLanguages":18,"viewCount":19,"primaryUrl":1240,"fullTextUrl":18,"authors":1241,"publicationType":221,"publisherRelationship":1300,"citationCount":18,"citationInfo":18,"publishDate":1328,"publishYear":1329,"citationAnalyzeStatus":17,"lastCitationAnalyze":18,"indexDatabases":18,"openAccess":18,"references":1330,"isForceReanalyzing":322},"544c13e4-44ac-434c-bcee-28c459bc6ac0","2024-04-11T23:56:34.559+00:00",[],"Palaeoclimatic-implications-of-isotopic-data-from-modern-and-early-Holocene-shells-of-the-freshwater-snail-Melanoides-tuberculata-from-lakes-in-the-Ethiopian-Rift-Valley",{"keywords":1231,"abstract":1233,"title":1235,"doi":1237},{"EN":1232},"",{"EN":1234},"Carbon and oxygen isotope ratios in the shells of the freshwater snail Melanoides tuberculata yield information on the isotopic composition of the water in which the shell was formed, which in turn relates to climatic conditions prevailing during the snails' life span. Melanoides is particularly important because it is widespread in Quaternary deposits throughout Africa and Asia and is ubiquitous in both fresh and highly evaporated lakes. Whole-shell and incremental growth data were collected from modern and fossil shells from two lakes in the Ethiopian Rift Valley. δ18O values in the modern shells from Lake Awassa are in equilibrium with modern waters, while δ18O values in subfossil shells from the margins of Lake Tilo indicate high rainfall during the early Holocene. Sequential analysis along the growth spiral of the shell provides information on seasonal or shorter-term variability of lake water during the lifetime of the organism.",{"EN":1236},"Palaeoclimatic implications of isotopic data from modern and early Holocene shells of the freshwater snail Melanoides tuberculata, from lakes in the Ethiopian Rift Valley",{"VOID":1238},"10.1023\u002FA:1008079219280",[142],"https:\u002F\u002Flink.springer.com\u002Farticle\u002F10.1023\u002FA:1008079219280",[1242,1259,1276,1288],{"id":1243,"sortIndex":19,"researcher":18,"roles":1244,"affiliations":1245,"properties":1256},"65a18167-38bf-41c1-af20-7e67e3b64e30",[],[1246],{"id":18,"sortIndex":19,"affiliation":1247,"properties":18},{"id":1248,"createTime":1249,"updateTime":1250,"relativeEntities":1251,"slug":1252,"properties":1253,"entityType":46,"verifyStatus":17,"verifyTime":18,"verifyNote":18,"syncStatus":17,"languages":18,"translateLanguages":18,"viewCount":19},"bfea0ccf-ea4f-4c7a-bb3b-38e12398abcf","2024-01-04T11:09:04.554+00:00","2025-02-05T01:19:47.066+00:00",[],"NERC-Isotope-Geosciences-Laboratory-British-Geological-Survey-Keyworth-Nottingham-UK",{"title":1254},{"VI":1255},"NERC Isotope Geosciences Laboratory, British Geological Survey, Keyworth, Nottingham, UK",{"title":1257},{"EN":1258},"Melanie J. Leng",{"id":1260,"sortIndex":167,"researcher":18,"roles":1261,"affiliations":1262,"properties":1273},"cdd34cd3-5f97-4084-8db1-9b4ab82a4343",[],[1263],{"id":18,"sortIndex":19,"affiliation":1264,"properties":18},{"id":1265,"createTime":1266,"updateTime":1267,"relativeEntities":1268,"slug":1269,"properties":1270,"entityType":46,"verifyStatus":17,"verifyTime":18,"verifyNote":18,"syncStatus":17,"languages":18,"translateLanguages":18,"viewCount":19},"87f3e7fc-2640-4b38-8742-4568313e706e","2024-01-16T06:10:47.345+00:00","2024-09-28T07:21:50.073+00:00",[],"Institute-of-Geography-and-Earth-Sciences-University-of-Wales-Aberystwyth-UK",{"title":1271},{"VI":1272},"Institute of Geography and Earth Sciences, University of Wales, Aberystwyth, UK",{"title":1274},{"EN":1275},"Angela L. Lamb",{"id":1277,"sortIndex":147,"researcher":18,"roles":1278,"affiliations":1279,"properties":1285},"f6a201e1-a041-45c2-9752-1968e721bb7e",[],[1280],{"id":18,"sortIndex":19,"affiliation":1281,"properties":18},{"id":1265,"createTime":1266,"updateTime":1267,"relativeEntities":1282,"slug":1269,"properties":1283,"entityType":46,"verifyStatus":17,"verifyTime":18,"verifyNote":18,"syncStatus":17,"languages":18,"translateLanguages":18,"viewCount":19},[],{"title":1284},{"VI":1272},{"title":1286},{"EN":1287},"Henry F. 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Telford",{"url":18,"publisher":1301,"properties":18},{"id":6,"createTime":7,"updateTime":8,"relativeEntities":1302,"slug":10,"properties":1303,"entityType":16,"verifyStatus":17,"verifyTime":18,"verifyNote":18,"syncStatus":17,"languages":18,"translateLanguages":18,"viewCount":19,"subjectFields":1306,"manageAffiliations":1307,"indexDatabases":1308,"url":18,"thumbnailPath":18,"statistic":1323,"gsStatistic":18,"type":18,"analyzePriority":18},[],{"issn":1304,"title":1305},{"VOID":13},{"EN":15},[],[],[1309,1316],{"id":62,"indexDatabase":1310,"url":77,"indexYears":18,"academicFieldIds":1315,"indexDatabaseRanking":18},{"id":64,"createTime":65,"updateTime":66,"relativeEntities":1311,"label":1312,"description":1313,"key":73,"publicationTags":1314,"standard":18},[],{"EN":69,"VI":69},{"VI":71,"EN":72},[75,76],[79,80,81],{"id":83,"indexDatabase":1317,"url":96,"indexYears":97,"academicFieldIds":1322,"indexDatabaseRanking":101},{"id":85,"createTime":86,"updateTime":87,"relativeEntities":1318,"label":1319,"description":1320,"key":93,"publicationTags":1321,"standard":18},[],{"EN":90,"VI":90},{"EN":90,"VI":92},[95],[99,100],{"impactFactor":19,"impactFactorByYear":1324,"i10Index":104,"i10IndexLast5Year":19,"totalPublication":105,"totalPublicationByYear":1325,"totalCitation":108,"totalCitationByYear":1326,"totalCitationPerPublication":112,"totalCitationPerPublicationByYear":1327,"hindexLast5Year":104,"hindex":104},{},{"2003":107,"2004":104},{"2003":110,"2004":111},{"2003":114,"2004":115},"1999-01-01",1999,[1331,1333,1335,1337,1339,1341,1343,1345,1347,1349,1351,1353,1355,1357,1359,1361,1363,1365,1367,1369,1371,1373,1375,1377,1379,1381,1383,1385,1387,1389,1391,1393,1395],{"id":18,"text":1332,"url":18,"identifiers":18},"Abell, P. 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Hydrol., 53 pp.",{"id":1398,"createTime":1399,"updateTime":1400,"relativeEntities":1401,"slug":1402,"properties":1403,"entityType":138,"verifyStatus":139,"verifyTime":1412,"verifyNote":140,"syncStatus":17,"languages":18,"translateLanguages":18,"viewCount":19,"primaryUrl":1413,"fullTextUrl":18,"authors":1414,"publicationType":221,"publisherRelationship":1523,"citationCount":18,"citationInfo":18,"publishDate":1556,"publishYear":1557,"citationAnalyzeStatus":17,"lastCitationAnalyze":18,"indexDatabases":18,"openAccess":18,"references":18,"isForceReanalyzing":322},"f5c1f8ff-5ffc-4e5a-9cc5-1865b0ea255f","2024-02-14T01:02:05.148+00:00","2025-01-16T23:56:27.839+00:00",[],"Influence-of-vegetation-change-on-watershed-hydrology-implications-for-paleoclimatic-interpretation-of-lacustrine-%CE%B418O-records",{"references":1404,"abstract":1406,"title":1408,"doi":1410},{"VOID":1405},"Binford, M. W., E. S. Deevey & T. L. Crisman, 1983. Paleolimnology: An historical perspective on lacustrine ecosystems. 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Ecology 65: 657–659.",{"EN":1407},"Stratigraphic shifts in the oxygen isotopic (δ18O) and trace element (Mg and Sr) composition of biogenic carbonate from tropical lake sediment cores are often interpreted as a proxy record of the changing relation between evaporation and precipitation (E\u002FP). Holocene δ18O and Mg and Sr records from Lakes Salpetén and Petén Itzá, Guatemala were apparently affected by drainage basin vegetation changes that influenced watershed hydrology, thereby confounding paleoclimatic interpretations. Oxygen isotope values and trace element concentrations in the two lowland lakes were greatest between ~ 9000 and 6800 14C-yr BP, suggesting relatively high E\u002FP, but pollen data indicate moist conditions and extensive forest cover in the early Holocene. The discrepancy between pollen- and geochemically-inferred climate conditions may be reconciled if the high early Holocene δ18O and trace element values were controlled principally by low surface runoff and groundwater flow to the lake, rather than high E\u002FP. Dense forest cover in the early Holocene would have increased evapotranspiration and soil moisture storage, thereby reducing delivery of meteoric water to the lakes. Carbonate δ18O and Mg and Sr decreased between 7200 and 3500 14C-yr BP in Lake Salpetén and between 6800 and 5000 14C-yr BP in Lake Petén Itzá. This decline coincided with palynologically documented forest loss that may have led to increased surface and groundwater flow to the lakes. In Lake Salpetén, minimum δ18O values (i.e., high lake levels) occurred between 3500 and 1800 14C-yr BP. Relatively high lake levels were confirmed by 14C-dated aquatic gastropods from subaerial soil profiles ~ 1.0–7.5 m above present lake stage. High lake levels were a consequence of lower E\u002FP and\u002For greater surface runoff and groundwater inflow caused by human-induced deforestation.",{"EN":1409},"Influence of vegetation change on watershed hydrology: implications for paleoclimatic interpretation of lacustrine δ18O records",{"VOID":1411},"10.1023\u002FA:1013535930777","2025-01-16T23:56:27.838+00:00","https:\u002F\u002Flink.springer.com\u002Farticle\u002F10.1023\u002FA:1013535930777",[1415,1432,1448,1460,1475,1487,1499,1511],{"id":1416,"sortIndex":709,"researcher":18,"roles":1417,"affiliations":1418,"properties":1429},"ebede9e0-9ed1-45ac-a260-2b6cf1703a9e",[350],[1419],{"id":18,"sortIndex":19,"affiliation":1420,"properties":18},{"id":1421,"createTime":1422,"updateTime":1423,"relativeEntities":1424,"slug":1425,"properties":1426,"entityType":46,"verifyStatus":17,"verifyTime":18,"verifyNote":18,"syncStatus":17,"languages":18,"translateLanguages":18,"viewCount":19},"a174c331-ca9e-4d13-bd86-8628035bf75a","2024-01-05T12:32:51.572+00:00","2024-09-18T17:43:08.987+00:00",[],"Department-of-Geological-Sciences-University-of-Florida-Gainesville-USA",{"title":1427},{"VI":1428},"Department of Geological Sciences, University of Florida, Gainesville, USA",{"title":1430},{"VI":1431},"Jonathan B. Martin",{"id":1433,"sortIndex":1434,"researcher":18,"roles":1435,"affiliations":1436,"properties":1445},"1822f2e0-8861-4887-bfc2-d9c5ecc2dedd",7,[350],[1437],{"id":18,"sortIndex":19,"affiliation":1438,"properties":18},{"id":1439,"createTime":1440,"updateTime":1440,"relativeEntities":1441,"slug":18,"properties":1442,"entityType":46,"verifyStatus":17,"verifyTime":18,"verifyNote":18,"syncStatus":17,"languages":18,"translateLanguages":18,"viewCount":19},"d2dd8e1b-c453-493c-b7dc-057ccab6a7fe","2024-02-14T01:02:05.301+00:00",[],{"title":1443},{"VI":1444},"Lawrence Livermore National Laboratory, Center for Accelerator Mass Spectrometry, Livermore, USA",{"title":1446},{"VI":1447},"Thomas P. Guilderson",{"id":1449,"sortIndex":167,"researcher":18,"roles":1450,"affiliations":1451,"properties":1457},"edc39b79-c5c4-4918-beb6-c61c52252a55",[350],[1452],{"id":18,"sortIndex":19,"affiliation":1453,"properties":18},{"id":1421,"createTime":1422,"updateTime":1423,"relativeEntities":1454,"slug":1425,"properties":1455,"entityType":46,"verifyStatus":17,"verifyTime":18,"verifyNote":18,"syncStatus":17,"languages":18,"translateLanguages":18,"viewCount":19},[],{"title":1456},{"VI":1428},{"title":1458},{"VI":1459},"David A. Hodell",{"id":1461,"sortIndex":260,"researcher":18,"roles":1462,"affiliations":1463,"properties":1472},"ccb68022-a80b-4994-9a75-e059a8d92106",[350],[1464],{"id":18,"sortIndex":19,"affiliation":1465,"properties":18},{"id":1466,"createTime":1467,"updateTime":1467,"relativeEntities":1468,"slug":18,"properties":1469,"entityType":46,"verifyStatus":17,"verifyTime":18,"verifyNote":18,"syncStatus":17,"languages":18,"translateLanguages":18,"viewCount":19},"c31fdd06-e526-44a0-958d-198a78b72630","2024-02-14T01:02:05.277+00:00",[],{"title":1470},{"VI":1471},"Geological Institute, ETH-Zentrum, Zürich, Switzerland",{"title":1473},{"VI":1474},"Flavio S. 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