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  • 1
    Electronic Resource
    Electronic Resource
    Diatom-salinity relationships in 111 lakes from the Interior Plateau of British Columbia, Canada: the development of diatom-based models for paleosalinity reconstructions (1994)
    Springer
    Journal of paleolimnology 12 (1994), S. 197-221 
    Details
    ISSN: 1573-0417
    Keywords: diatoms ; paleolimnology ; paleoclimatology ; salinity ; athalassic ; British Columbia ; CCA ; transfer function
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Geosciences
    Notes: Abstract Diatoms were identified and enumerated from the surface sediments of 111 lakes, 45 from the Kamloops region and 66 from the Cariboo/Chilcotin region, located on the southern Interior Plateau of British Columbia, Canada. This paper is an extension of another study which investigated the relationship of diatoms to salinity and ionic composition in 65 lakes from the Cariboo/Chilcotin region. The 111 lakes spanned a large gradient in salinity, ranging from fresh through hypersaline (late-summer salinity values ranged from 0.04 to 369 g l−1), and included both carbonate- and sulphate-dominated lakes with sodium and magnesium as the dominant cations. The Kamloops region had more sulphate-dominated, hypersaline lakes and fewer carbonate-rich lakes than the Cariboo/Chilcotin region. Most lakes had higher salinities in the late-summer compared to the spring. Both salinity and brine-type were important variables that could explain the different diatom assemblages present in the lakes. The majority of diatom taxa had salinity optima in the freshwater to subsaline range (〈3 g l−1), and the taxa displayed a range of both narrow and broad tolerances along the salinity gradient. Weighted-averaging regression and calibration, and maximum likelihood techniques were used to develop salinity inference models from the diatom assemblages based on their relationship to the spring, late-summer and average lakewater salinity measurements. Simple weighted-averaging (WA) models generally produced the same or lower bootstrapped RMSEs of prediction than weighted-averaging with tolerance downweighting (WA(tol)) in the two regional and the combined datasets. Weighted averaging partial least squares (WA-PLS) showed little or no improvement in the predictive abilities of the datasets, as judged by the jackknifed RMSE of prediction. In all cases, the combined dataset of 102 lakes performed better than either of the smaller regional datasets, with relatively little difference between spring, average and late-summer salinity models. The maximum likelihood models gave lower apparent RMSEs of prediction in comparison to other methods; however, independent validation of this technique using methods such as bootstrapping were not undertaken because of the computer intensive nature of such analyses. These diatom-based salinity models are now available for reconstructing salinity and climatic trends from appropriately chosen closed-basin lakes in the Interior region of British Columbia.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00678021
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  • 2
    Electronic Resource
    Electronic Resource
    A Holocene paleosalinity diatom record from southwestern Saskatchewan, Canada: Harris Lake revisited (1997)
    Springer
    Journal of paleolimnology 17 (1997), S. 23-31 
    Details
    ISSN: 1573-0417
    Keywords: diatoms ; salinity ; climatic change ; Holocene ; CypressHills ; Saskatchewan
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Geosciences
    Notes: Abstract Fossil diatoms were analysed from a 10.3 m core from Harris Lake, Cypress Hills, Saskatchewan, and a diatom-salinity transfer function was used to construct a history of Holocene salinity changes for the lake. The diatom paleosalinity record indicates that Harris Lake remained fresh 〈0.5 g l-1 throughout the Holocene, with only slight increases in salinity between approximately 6500 and 5200 years BP. This interval corresponds to the only period in the lake's history when planktonic diatoms were abundant; benthic Fragilaria taxa, mainly F. pinnata, F. construens and F. brevistriata were dominant throughout most of the Holocene. The shift from a benthic to a planktonic diatom flora between 6500 and 5200 years BP may be an indirect response to a warmer climate that reduced forest cover in the watershed and allowed greater rates of inorganic sedimentation. The small salinity increase that accompanies the floristic change is probably not the result of lower lake levels; in fact the lake was probably deeper at this point than in the later Holocene. This paleosalinity record indicates that Harris Lake did not experience episodes of hypersalinity during the mid-Holocene, as suggested by a previous study, and that the lake may have been fresh during the early Holocene as well.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1023/A:1007956808240
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  • 3
    Electronic Resource
    Electronic Resource
    Midge-and diatom-based palaeosalinity reconstructions for Mahoney Lake, Okanagan Valley, British Columbia, Canada (1997)
    Springer
    International journal of salt lake research 6 (1997), S. 249-267 
    Details
    ISSN: 1573-8590
    Keywords: Chironanidae ; diatoms ; palaeoclimate ; palaeolimnology ; palaeoecology ; palaeosalinity ; salinity ; postglacial ; climate change
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Geography
    Notes: Abstract Salinity fluctuations in lakes of semi-arid regions have long been recognised as indicators of palaeoclimatic change, and have provided a valuable line of evidence in palaeo-climatic reconstruction. In the present study, fossil remains of diatoms and midges were used to reconstruct salinity changes at Mahoney Lake from the early postglacial, through the early, mid and late Holocene. A transition from midges typical of a freshwater community (Protanypus, Sergentia, Heterotrissocladius, Cladopelma, Dicrotendipes) during the early postglacial, to those indicative of saline environments (Cricotopus/Orthocladius, Tanypus) occurred in the early Holocene. The midge-inferred salinity values reflected the shift from freshwater (0.031 g/L) immediately after deglaciation, to saline water (2.4 to 55.2 g/L) in subsequent periods. A less saline period was found to have occurred after 1000 yr BP, suggesting a cooler or wetter period. The diatom record indicates similar trends, with freshwater taxa (e.g.,Cyclotella bodanica var. aff.lemanica) dominating near the bottom of the core. Diatom-inferred salinities indicate that saline conditions (about 30 g/L) prevailed throughout subsequent Holocene time, although relatively fresh conditions are indicated following deposition of the Mazama Ash, and from about 1500 yr BP until the present day. Midge and diatom-inferred salinity reconstructions for Mahoney Lake compare favorably with each other, and with climate trends inferred from earlier palynological evidence. The palaeosalinity record thus contributes new data relevant to past climatic conditions, in a region where little data have previously been collected.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF02449928
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  • 4
    Electronic Resource
    Electronic Resource
    Midge- and diatom-based palaeosalinity reconstructions for Mahoney Lake, Okanagan Valley, British Columbia, Canada (1997)
    Springer
    International journal of salt lake research 6 (1997), S. 249-267 
    Details
    ISSN: 1573-8590
    Keywords: Chironanidae ; diatoms ; palaeoclimate ; palaeolimnology ; palaeoecology ; palaeosalinity ; salinity ; postglacial ; climate change
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Geography
    Notes: Abstract Salinity fluctuations in lakes of semi-arid regions have long beenrecognised as indicators of palaeoclimatic change, and have provided avaluable line of evidence in palaeoclimatic reconstruction. In the presentstudy, fossil remains of diatoms and midges were used to reconstructsalinity changes at Mahoney Lake from the early postglacial, through theearly, mid and late Holocene. A transition from midges typical of afreshwater community (Protanypus, Sergentia, Heterotrissocladius,Cladopelma, Dicrotendipes) during the early postglacial, to those indicativeof saline environments (Cricotopus/Orthocladius, Tanypus) occurred in theearly Holocene. The midge-inferred salinity values reflected the shift fromfreshwater (0.031 g/L) immediately after deglaciation, to saline water (2.4to 55.2 g/L) in subsequent periods. A less saline period was found to haveoccurred after 1000 yr BP, suggesting a cooler or wetter period. The diatomrecord indicates similar trends, with freshwater taxa (e.g., Cyclotellabodanica var. aff. lemanica) dominating near the bottom of the core.Diatom-inferred salinities indicate that saline conditions (about 30 g/L)prevailed throughout subsequent Holocene time, although relatively freshconditions are indicated following deposition of the Mazama Ash, and fromabout 1500 yr BP until the present day. Midge and diatom-inferred salinityreconstructions for Mahoney Lake compare favorably with each other, and withclimate trends inferred from earlier palynological evidence. Thepalaeosalinity record thus contributes new data relevant to past climaticconditions, in a region where little data have previously been collected.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1023/A:1009056003978
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  • 5
    Electronic Resource
    Electronic Resource
    Development of diatom-based salinity models for paleoclimatic research from lakes in British Columbia (Canada) (1993)
    Springer
    Hydrobiologia 269-270 (1993), S. 179-196 
    Details
    ISSN: 1573-5117
    Keywords: diatoms ; salinity ; saline lakes ; canonical correspondence analysis ; weighted-averaging ; paleoclimate ; British Columbia ; Canada
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract Diatoms were identified and enumerated from the surface sediments of 65 lakes located on the Cariboo and Chilcotin Plateaux (British Columbia, Canada). These lakes span a large gradient in lakewater ionic concentration (fresh through hypersaline) and composition, as well as other physical/chemical variables. Almost all of the study lakes had higher salinities in the late-summer than in the spring. The lakes with spring salinities 〉8 g l−1 showed the largest seasonal increases in salinity. Ionic composition was similar in the spring and late-summer for most lakes. Both ionic concentration (i.e. salinity) and composition were important environmental variables that could account for the different diatom floras in the lakes. Diatom assemblages characteristic of carbonate-dominated and sulfate-dominated waters were identified. Other variables such as water depth and phosphorus concentration were also important. The majority (87%) of diatom taxa had estimated salinity optima 〈 3 g l−1 Halophilic diatom taxa had broader tolerances to salinity when compared to the fresh water taxa, however taxa with narrow and broad tolerances could be identified across the salinity gradient. Species diversity was weakly but significantly correlated to lakewater salinity (r 2 = 0.18 to 0.3, P 〈 0.05). Salinity inference models were developed based on the relationship between the diatom assemblages and the spring, late-summer and average salinity. The correlations between the measured and diatominferred salinity, based on the spring (r = 0.95), late-summer (r = 0.94) and average (r = 0.95) salinity data, are high because there was an extremely strong correlation (r = 0.98) between the log transformed spring and late-summer measured salinities. These salinity reconstruction models provide a tool that can be used to infer past climatic changes as part of paleolimnological studies from appropriate closed-basin lakes in British Columbia.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00028017
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