The Experts below are selected from a list of 270 Experts worldwide ranked by ideXlab platform
Ian R. Walker - One of the best experts on this subject based on the ideXlab platform.
-
Midge-inferred Holocene climate history of two subalpine lakes in southern British Columbia, Canada
The Holocene, 2004Co-Authors: Sandra M. Rosenberg, Ian R. Walker, Rolf W. Mathewes, Douglas J. HallettAbstract:To investigate postglacial environmental changes in both the coastal and interior wet belts of British Columbia, fossil midges were analysed from two subalpine lakes, one adjacent to the lower Fraser canyon (Frozen Lake), and the other in Mount Revelstoke National Park (Eagle Lake). The midge stratigraphy for Frozen Lake revealed an abundance of rheophilous chironomid taxa and Simuliidae larvae, refecting the presence of an inflowing stream. An abundance of Chaoborus mandibles and Microtendipes during the early Holocene (c. 10100–7700 14C years BP, c. 11500–8500 cal. years BP) suggests warmer temperatures. A subsequent decline in the warm indicators and relative increases in cold stenotherms (Heterotrissocladius and Diamesa) indicate cooling until present day. This climate reconstruction is consistent with other quantitative and qualitative evidence for past climatic change in southern British Columbia. At Eagle Lake the warm indicators, Dicrotendipes and Polypedilum, are seen in the early Holocene (c. 85...
-
Postglacial changes in chironomid communities and inferred climate near treeline at Mount Stoyoma, Cascade Mountains, southwestern British Columbia, Canada
Journal of Paleolimnology, 1998Co-Authors: Michael J. Smith, Ian R. Walker, Marlow G. Pellatt, Rolf W. MathewesAbstract:Analysis of the distributions of chironomid (midge) and other dipteran subfossils from two high elevation lake sediment cores in the Cascade Mountains reveals changes in midge communities and inferred climate since the late-glacial. Cabin Lake and 3M Pond are located near treeline in the subalpine Engelmann Spruce/Subalpine Fir biogeoclimatic zone of British Columbia. In Cabin Lake, chironomid head capsule assemblages depict a typical late-glacial community, and three distinct Holocene communities. In Cabin Lake, the late-glacial community is composed of cold-stenothermous taxa dominated by Stictochironomus, Mesocricotopus, Heterotrissocladius, Parakiefferiella nigra, Protanypus and Paracladius, whereas warm water midges are absent or rare, indicating cold conditions. A late-glacial chironomid community was not found in 3M Pond. In both lakes the early Holocene is dominated by a diverse warm-adapted assemblage, corresponding to the warm climatic conditions of the xerothermic period. Cabin Lake's mid-Holocene zone records a decrease in relative abundance of the warm water types and is accompanied by an increase in cold-stenotherms. At 3M Pond this period shows a dramatic loss in diversity of warm-adapted taxa, as the temperate genus Dicrotendipes dominates. This zone corresponds to Hebda's (1995) mesothermic period. Further cooling in the late Holocene (to modern conditions) is inferred from continued reduction of warm water midges and persistence (at Cabin Lake) or appearance (at 3M Pond) of a cold-stenothermal community. This late Holocene cooling is similar in timing to Neoglacial advances in the Coast, Cascade, and Rocky Mountains of southern British Columbia. Similarities in the timing of chironomid and vegetation community changes at these high elevation sites, along with the more rapid response time of the Chironomidae, support the sensitivity of midges to postglacial climatic change at high elevation sites.
-
A palaeolimnological study of Tugulnuit Lake, British Columbia, Canada, with special emphasis on river influence as recorded by chironomids in the lake's sediment
Journal of Paleolimnology, 1998Co-Authors: Andrea Rück, Ian R. Walker, Richard HebdaAbstract:Sediments from Tugulnuit Lake in the Okanagan Valley of British Columbia, Canada, were examined for chironomid assemblages. The chironomid stratigraphy obtained encompasses the last 4000 to 5000 years and suggests a warm and fairly stable climate typical for a temperate lake at low- to mid-elevation. This is indicated by the even distribution of warm-water taxa, such as Cladopelma, Dicrotendipes, Polypedilum, Pentaneurini, Stempellina, Stempellinella/Zavrelia and Pseudochironomus throughout the core. Very few cold-water taxa occurred in the sediments. However, stream inputs have had a major impact on Tugulnuit Lake. Sandy sediments and the appearance of Simuliidae and stream-inhabiting chironomid taxa (e.g., Brillia/Euryhapsis, Eukiefferiella/Tvetenia, Rheocricotopus) indicate that a stream intruded into the current lake's basin ca. 3800 yr Before Present (BP). Sediments deposited prior to, and after, the stream's intrusion show a distinctly different chironomid assemblage exhibiting chironomid taxa more typical for lentic habitats. This result indicates that chironomids can serve to detect past stream influences on lake environments. Thus, rheophilic chironomids preserved in lake cores provide a new alternative for reconstructing stream palaeoenvironmental records.
-
Midge- and diatom-based palaeosalinity reconstructions for Mahoney Lake, Okanagan Valley, British Columbia, Canada
International Journal of Salt Lake Research, 1997Co-Authors: Mark L. Heinrichs, Ian R. Walker, Rolf W. Mathewes, Susan E. Wilson, John P. Smol, Kenneth J. HallAbstract: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.
-
Chironomidae (Diptera): quantitative palaeosalinity indicators for lakes of western Canada
Canadian Journal of Fisheries and Aquatic Sciences, 1995Co-Authors: Ian R. Walker, Susan E. Wilson, John P. SmolAbstract:A survey of chironomid remains preserved in the surficial sediments of 86 British Columbia lakes was conducted to assess the feasibility of reconstructing palaeosalinities from assemblages of fossil chironomid head capsules. Many taxa common in freshwater lakes were either rare or absent at higher salinities. Lakes having salinities greater than about 10.0 g∙L−1 were distinguished by the overwhelming relative abundance of Cricotopus/Orthocladius. In less saline waters, common taxa included Chironomus, Procladius, Psectrocladius, and the subtribe Tanytarsina. Heterotrissocladius, Lauterborniella/Zavreliella, Pagastiella, and Sergentia were only collected in freshwater habitats. Canonical correspondence analysis revealed that three environmental variables (late summer lakewater salinity and concentrations of Sr and total P) explained significant variation in the weighted averages of taxa. Tanytarsina and Dicrotendipes were common at low Sr concentrations in carbonate lakes. A weighted-averaging calibration ...
Rolf W. Mathewes - One of the best experts on this subject based on the ideXlab platform.
-
Midge-inferred Holocene climate history of two subalpine lakes in southern British Columbia, Canada
The Holocene, 2004Co-Authors: Sandra M. Rosenberg, Ian R. Walker, Rolf W. Mathewes, Douglas J. HallettAbstract:To investigate postglacial environmental changes in both the coastal and interior wet belts of British Columbia, fossil midges were analysed from two subalpine lakes, one adjacent to the lower Fraser canyon (Frozen Lake), and the other in Mount Revelstoke National Park (Eagle Lake). The midge stratigraphy for Frozen Lake revealed an abundance of rheophilous chironomid taxa and Simuliidae larvae, refecting the presence of an inflowing stream. An abundance of Chaoborus mandibles and Microtendipes during the early Holocene (c. 10100–7700 14C years BP, c. 11500–8500 cal. years BP) suggests warmer temperatures. A subsequent decline in the warm indicators and relative increases in cold stenotherms (Heterotrissocladius and Diamesa) indicate cooling until present day. This climate reconstruction is consistent with other quantitative and qualitative evidence for past climatic change in southern British Columbia. At Eagle Lake the warm indicators, Dicrotendipes and Polypedilum, are seen in the early Holocene (c. 85...
-
Postglacial changes in chironomid communities and inferred climate near treeline at Mount Stoyoma, Cascade Mountains, southwestern British Columbia, Canada
Journal of Paleolimnology, 1998Co-Authors: Michael J. Smith, Ian R. Walker, Marlow G. Pellatt, Rolf W. MathewesAbstract:Analysis of the distributions of chironomid (midge) and other dipteran subfossils from two high elevation lake sediment cores in the Cascade Mountains reveals changes in midge communities and inferred climate since the late-glacial. Cabin Lake and 3M Pond are located near treeline in the subalpine Engelmann Spruce/Subalpine Fir biogeoclimatic zone of British Columbia. In Cabin Lake, chironomid head capsule assemblages depict a typical late-glacial community, and three distinct Holocene communities. In Cabin Lake, the late-glacial community is composed of cold-stenothermous taxa dominated by Stictochironomus, Mesocricotopus, Heterotrissocladius, Parakiefferiella nigra, Protanypus and Paracladius, whereas warm water midges are absent or rare, indicating cold conditions. A late-glacial chironomid community was not found in 3M Pond. In both lakes the early Holocene is dominated by a diverse warm-adapted assemblage, corresponding to the warm climatic conditions of the xerothermic period. Cabin Lake's mid-Holocene zone records a decrease in relative abundance of the warm water types and is accompanied by an increase in cold-stenotherms. At 3M Pond this period shows a dramatic loss in diversity of warm-adapted taxa, as the temperate genus Dicrotendipes dominates. This zone corresponds to Hebda's (1995) mesothermic period. Further cooling in the late Holocene (to modern conditions) is inferred from continued reduction of warm water midges and persistence (at Cabin Lake) or appearance (at 3M Pond) of a cold-stenothermal community. This late Holocene cooling is similar in timing to Neoglacial advances in the Coast, Cascade, and Rocky Mountains of southern British Columbia. Similarities in the timing of chironomid and vegetation community changes at these high elevation sites, along with the more rapid response time of the Chironomidae, support the sensitivity of midges to postglacial climatic change at high elevation sites.
-
Midge- and diatom-based palaeosalinity reconstructions for Mahoney Lake, Okanagan Valley, British Columbia, Canada
International Journal of Salt Lake Research, 1997Co-Authors: Mark L. Heinrichs, Ian R. Walker, Rolf W. Mathewes, Susan E. Wilson, John P. Smol, Kenneth J. HallAbstract: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.
Geoffrey Scudder - One of the best experts on this subject based on the ideXlab platform.
-
Postglacial midge community change and Holocene palaeotemperaturereconstructions near treeline, southern British Columbia (Canada)
Journal of Paleolimnology, 2002Co-Authors: Samantha Palmer, Ian Walker, Markus Heinrichs, Geoffrey ScudderAbstract:Stratigraphic analysis of fossil chironomid head capsules wasperformed at North Crater Lake and Lake of the Woods, located at treeline (2250m) in the Ashnola region of southernmost British Columbia. Priorto 10,000 yr BP, cold conditions were indicated by the lack oftemperate taxa and the presence of cold-stenotherms. The abundance anddiversity of warm-adapted taxa (e.g., Dicrotendipes,Microtendipes, Polypedilum and Cladopelma )increased rapidly after 9500 yr BP, whereas taxa indicative ofcold conditions disappeared. Beginning prior to deposition of the Mazama ash(6730 ± 40 yr BP), several warm-adapted taxa decreasedin abundance. Mid- to late-Holocene assemblages (ca. 4500yr BP to present) indicated continued cooling as revealed by afurther reduction in diversity and abundance of warm-adapted taxa atboth lakes, and the reappearance of cold-stenotherms in Lake of theWoods. Diversity changes in the cores paralleled the inferred climatic changes.Diversity was low during the late-glacial, increased in theearly-Holocene, and declined after 5400 yr BP.To quantitatively infer past climatic changes, a newweighted yphen;averaging partial-least-squares (WA-PLS)model was developed and applied to the fossil midge data. The quantitativereconstructions revealed late-glacial mean July air temperatures rangingfrom about 8 to 10°C. Summer air temperatures were highest inthe early Holocene (13 to 17°C), gradually decreasing by about3°C through the mid- to late-Holocene.
Richard Hebda - One of the best experts on this subject based on the ideXlab platform.
-
A palaeolimnological study of Tugulnuit Lake, British Columbia, Canada, with special emphasis on river influence as recorded by chironomids in the lake's sediment
Journal of Paleolimnology, 1998Co-Authors: Andrea Rück, Ian R. Walker, Richard HebdaAbstract:Sediments from Tugulnuit Lake in the Okanagan Valley of British Columbia, Canada, were examined for chironomid assemblages. The chironomid stratigraphy obtained encompasses the last 4000 to 5000 years and suggests a warm and fairly stable climate typical for a temperate lake at low- to mid-elevation. This is indicated by the even distribution of warm-water taxa, such as Cladopelma, Dicrotendipes, Polypedilum, Pentaneurini, Stempellina, Stempellinella/Zavrelia and Pseudochironomus throughout the core. Very few cold-water taxa occurred in the sediments. However, stream inputs have had a major impact on Tugulnuit Lake. Sandy sediments and the appearance of Simuliidae and stream-inhabiting chironomid taxa (e.g., Brillia/Euryhapsis, Eukiefferiella/Tvetenia, Rheocricotopus) indicate that a stream intruded into the current lake's basin ca. 3800 yr Before Present (BP). Sediments deposited prior to, and after, the stream's intrusion show a distinctly different chironomid assemblage exhibiting chironomid taxa more typical for lentic habitats. This result indicates that chironomids can serve to detect past stream influences on lake environments. Thus, rheophilic chironomids preserved in lake cores provide a new alternative for reconstructing stream palaeoenvironmental records.
Samantha Palmer - One of the best experts on this subject based on the ideXlab platform.
-
Postglacial midge community change and Holocene palaeotemperaturereconstructions near treeline, southern British Columbia (Canada)
Journal of Paleolimnology, 2002Co-Authors: Samantha Palmer, Ian Walker, Markus Heinrichs, Geoffrey ScudderAbstract:Stratigraphic analysis of fossil chironomid head capsules wasperformed at North Crater Lake and Lake of the Woods, located at treeline (2250m) in the Ashnola region of southernmost British Columbia. Priorto 10,000 yr BP, cold conditions were indicated by the lack oftemperate taxa and the presence of cold-stenotherms. The abundance anddiversity of warm-adapted taxa (e.g., Dicrotendipes,Microtendipes, Polypedilum and Cladopelma )increased rapidly after 9500 yr BP, whereas taxa indicative ofcold conditions disappeared. Beginning prior to deposition of the Mazama ash(6730 ± 40 yr BP), several warm-adapted taxa decreasedin abundance. Mid- to late-Holocene assemblages (ca. 4500yr BP to present) indicated continued cooling as revealed by afurther reduction in diversity and abundance of warm-adapted taxa atboth lakes, and the reappearance of cold-stenotherms in Lake of theWoods. Diversity changes in the cores paralleled the inferred climatic changes.Diversity was low during the late-glacial, increased in theearly-Holocene, and declined after 5400 yr BP.To quantitatively infer past climatic changes, a newweighted yphen;averaging partial-least-squares (WA-PLS)model was developed and applied to the fossil midge data. The quantitativereconstructions revealed late-glacial mean July air temperatures rangingfrom about 8 to 10°C. Summer air temperatures were highest inthe early Holocene (13 to 17°C), gradually decreasing by about3°C through the mid- to late-Holocene.