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  • 1
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 361 (1993), S. 623-626 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] The study area comprises two of the three Canadian Maritime provinces (43°-48°N, 60°-68°W), New Brunswick and Nova Scotia. Deglaciation of the region may have begun as early as 14,500 yr BP and was completed by 11,000 yr BP, although some evidence ...
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 385 (1997), S. 423-426 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Although the hypothesized link between midge assemblages and climate was at one time a controversial issue3"6, recent statistical analysis of midge and environmental data of eastern Canadian lakes has shown that the abundance and distribution of midge larvae (Chironomidae and Ceratopogonidae) are ...
    Type of Medium: Electronic Resource
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  • 3
    ISSN: 1573-0417
    Keywords: Ceratopogonidae ; Chironomidae ; Chaoborus ; weighted averaging ; weighted averaging partial least squares ; temperature optima ; error estimates ; palaeoclimate ; late-glacial ; Younger Dryas
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Geosciences
    Notes: Abstract Using an expanded surface sample data set, representing lakes distributed across a transect from southernmost Canada to the Canadian High Arctic, a revised midge-palaeotemperature inference model was developed for eastern Canada. Modelling trials with weighted averaging (with classical and inverse deshrinking; with and without tolerance downweighting) and weighted averaging partial least squares (WA-PLS) regression, with and without square-root transformation of the species data, were used to identify the best model. Comparison of measured and predicted temperatures revealed that a 2 component WA-PLS model for square-root transformed percentage species data provided the model with the highest explained variance (r $$_{jack}^2 $$ = 0.88) and the lowest error estimate (RMSEP jack  = 2.26 °C). Comparison of temperature inferences based on the new and old models indicates that the original model may have seriously under-estimated the magnitude of late-glacial temperature oscillations in Atlantic Canada. The new inferences suggest that summer surface water temperatures in Splan Pond, New Brunswick were approximately 10 to 12 °C immediately following deglaciation and during the Younger Dryas. During the Allerod and early Holocene, surface water temperatures of 20 to 24 °C were attained. The new model thus provides the basis for more accurate palaeotemperature reconstructions throughout easternmost Canada.
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Springer
    Journal of paleolimnology 16 (1996), S. 257-274 
    ISSN: 1573-0417
    Keywords: late-glacial ; transect ; chironomid ; New Brunswick
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Geosciences
    Notes: Abstract Chironomid analysis was performed on late-glacial sediment from four New Brunswick lakes in order to gain basic ecological information regarding the richness and diversity of late-glacial chironomid assemblages, and to compare the pattern of succession at each site. At all sites, the richness and diversity of the larval assemblages were lowest immediately following deglaciation and during the Younger Dryas, corresponding to the coldest times of the late-glacial period. Although cold-stenothermous taxa are characteristic of sediments deposited immediately following deglaciation, as well as during the Killarney Oscillation and Younger Dryas cooling events, the constituent taxa are different at each site. During the intervening warm periods, the larval assemblages at each site are also dissimilar, with the more southern sites containing a greater variety of temperate littoral taxa. This raises the possibility that a north-south temperature gradient existed during the warm intervals of the late-glacial period in New Brunswick.
    Type of Medium: Electronic Resource
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  • 5
    facet.materialart.
    Unknown
    PANGAEA
    In:  European Pollen Database (EPD)
    Publication Date: 2023-02-23
    Keywords: Age, dated; Age, dated, error to older; Age, dated, error to younger; Age, dated material; Age, radiocarbon; BALLYBET; Ballybetagh, Ireland; Comment; DEPTH, sediment/rock; Sample, optional label/labor no
    Type: Dataset
    Format: text/tab-separated-values, 28 data points
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  • 6
    facet.materialart.
    Unknown
    PANGAEA
    In:  European Pollen Database (EPD)
    Publication Date: 2023-11-01
    Keywords: Achillea-type; Armeria; Artemisia; Asteroideae; Astragalus alpinus-type; BALLYBET; Ballybetagh, Ireland; Betula; Botrychium; Campanula; Caryophyllaceae; Ceratophyllum hair; cf. Lotus; Chenopodiaceae; Cichorioideae; Cirsium-type; Corylus; Cruciferae; Cyperaceae; Cystopteris; DEPTH, sediment/rock; Diphasium alpinum; Dryopteris; Elatine; Empetrum; Epilobium; Equisetum; Filipendula; Galium; Gramineae; Helianthemum; Hippophae; Huperzia selago; Indeterminable: undifferentiated; Indeterminable: unknown; Jasione; Juniperus; Koenigia islandica; Linum; Littorella uniflora; Mentha-type; Myriophyllum alterniflorum; Myriophyllum spicatum; Ononis-type; Ophioglossum; Pinus; Plantago major; Plantago maritima; Polygonum amphibium; Polygonum persicaria; Polygonum viviparum; Polypodium; Populus; Potamogeton; Potentilla; Quercus; Ranunculus; Rosaceae; Rumex; Salix; Sanguisorba; Saxifraga aizoides; Saxifragaceae; Saxifraga oppositifolia; Scrophulariaceae; Sparganium; Thalictrum; Trifolium; Typha latifolia; Umbelliferae; Urtica; Vicia-type
    Type: Dataset
    Format: text/tab-separated-values, 2484 data points
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  • 7
    Publication Date: 2024-04-20
    Keywords: Abrupt Climate Changes and Environmental Responses; Accumulation model; ACER; Aconitum; Alnus incana; Alnus viridis; Amaranthaceae/Chenopodiaceae; Ambrosia; Andromeda; Androsace; Apiaceae; Arctostaphylos uva-ursi; Artemisia; Asteraceae; Astragalus; Betula; Botrychium; Brassicaceae; Bupleurum; Calendar age; Calendar age, maximum/old; Calendar age, minimum/young; Caryophyllaceae; Cassiope; Classical age-modeling approach, CLAM (Blaauw, 2010); Cnidium; Counting, palynology; Cyperaceae; Cystopteris; DEPTH, sediment/rock; Dodecatheon; Douglasia; Dryas; Empetrum; Epilobium; Equisetum; Ericaceae; Ericales; Fabaceae; Galium; Gentiana; Geum; Hanging_Lake; Hedysarum; Hippuris vulgaris; Huperzia selago; Lagotis glauca; Ledum; Lesquerella; Liliaceae; Linnaea borealis; Lupinus; Lycopodiaceae; Lycopodium annotinum; Lycopodium clavatum; Lycopodium complanatum; Lycopodium obscurum; Mertensia-type; Myrica; Oxyria digyna; Oxytropis; Pedicularis lanceolata; Phlox; Picea; Pinus; Plantago canescens; Plantago major; Poaceae; Polemonium; Pollen indeterminata; Polygonum viviparum; Polypodiaceae; Populus; Potamogeton; Potentilla; Pyrola; Ranunculaceae; Rosaceae; Rubus chamaemorus; Rumex; Salix; Sample ID; Saussurea; Saxifragaceae; Saxifraga cernua; Saxifraga hieracifolia; Saxifraga tricuspidata; Selaginella sibirica; Shepherdia canadensis; Sparganium; Sphagnum; Spiraea; Thalictrum; Tofieldia; Triglochin; Type of age model; Typha latifolia; Unknown; Vaccinium; Valeriana
    Type: Dataset
    Format: text/tab-separated-values, 12350 data points
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  • 8
    Publication Date: 2024-04-17
    Description: This dataset provides chironomid counts for the Holocene sediment sequence retrieved from Crooked Pond (United States). Sediment cores were retrieved from the lake using a 1-m long handheld piston corer deployed from a floating coring platform during field work in May 2009. Volumetric samples were obtained from splits of the core and processed in the laboratory (University of New Brunswick, Canada) using standard protocols. Chironomid counts are presented against both depth (cm) and age (cal yr. BP). A total of 58 downcore 1-cm-thick samples were analysed, ranging between 477.5cm depth (9056 cal yr BP) and 0.5cm depth (the present). The chironomid record provides information about changes in the chironomid fauna as well as in within-lake conditions. The dataset was produced to inform on the exact age and duration of a major lake-level lowstand during the mid-Holocene. This lowstand was compared to palynological transitions determined on pollen samples from an older core sequence derived from the same coring location.
    Keywords: Ablabesmyia; AGE; Ceratopogonidae; Chaoborus; Chironomids; Chironomini indeterminata; Chironomus anthracinus-type; Chironomus plumosus-type; Cladopelma lateralis-type; Cladotanytarsus mancus-type; Cladotanytarsus-type A; Corynoneura edwardsi-type; Counting; Counting, microscope; Cricotopus bicinctus-type; Cricotopus cylindraceus-type; Cricotopus laricomalis-type; Cricotopus obnixus-type; CrookedPond_CP1a; Cryptochironomus; Demicryptochironomus; DEPTH, sediment/rock; Dicrotendipes nervosus-type; drought; Einfeldia; Endochironomus albipennis-type; Endochironomus impar-type; Georthocladius; Glyptotendipes barbipes-type; Glyptotendipes severini-type; Guttipelopia; Hand-held piston corer; Heterotrissocladius grimshawi-type; Heterotrissocladius marcidus-type; Heterotrissocladius subpilosus-type; HH_PC; Labrundinia; Lake core; Lauterborniella/Zavreliella; Limnophyes; Micropsectra insignilobus-type; Microtendipes pedellus-type; Nanocladius; Nilothauma; Oliveridia; ORDINAL NUMBER; Orthocladiinae indeterminata; Pagastiella; Parachironomus varus-type; Parakiefferiella bathophila-type; Parakiefferiella-type A; Parametriocnemus/Paraphaenocladius; Paratanytarsus penicillatus-type; Paratendipes albimanus-type; Paratendipes nudisquama-type; Polypedilum nubeculosum-type; Procladius; Psectrocladius calcaratus-type; Psectrocladius flavus-type; Psectrocladius sordidellus-type; Pseudochironomus; Pseudosmittia; Stempellina; Stempellinella/Zavrelia; Stenochironomus; Stictochironomus rosenschoeldi-type; Synorthocladius; Tanypodinae indeterminata; Tanytarsini indeterminata; Tanytarsus glabrescens-type; Tanytarsus indeterminata; Tanytarsus lugens-type; Tanytarsus mendax-type; Tanytarsus pallidicornis-type; Thienemanniella; Thienemannimyia; Tribelos; United States; Unniella; Xenochironomus; Zalutschia-type B; Zalutschia zalutschicola
    Type: Dataset
    Format: text/tab-separated-values, 4060 data points
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  • 9
    Publication Date: 2024-04-17
    Description: This dataset provides the percentage-abundances of chironomid taxa identified in a set of surface sediment samples taken in the Plymouth area (Massachusetts, United States) in 2009. For each sample, a short sediment core was retrieved from a rubber dinghy using a gravity corer (both the Glew and the mini-Glew models were used) during field work in June and September 2009. Volumetric samples taken from the 0-1cm sediment depth sample were subsequently processed in the laboratory (University of New Brunswick, Canada) using standard protocols. The procedure involved placing the sample aliquot in a glass beaker and submerging it in warm 10% KOH for ca. 20 mins. Subsequently the material was rinsed over a 100µm mesh and individual head capsules were hand-sorted from the residue and mounted on microscope slides. Chironomid head capsules were identified using Brooks et al. 2007 and encountered taxa that were not present in that handbook are illustrated and described in Engels & Cwynar (2011). This dataset provides chironomid abundances (expressed as percentage of the total chironomid sum) as well as measurements of water depth for each of the samples; Engels & Cwynar (2011) provide additional environmental observations for each of the 8 lakes sampled. A total of 132 surface sediment samples were originally counted, but as 3 samples only reached total chironomid count sums of less-than-50 these were removed from the original dataset, resulting in a final dataset consisting of 129 samples. The chironomid data provides information on within-lake distribution patterns of chironomid taxa for each of the 8 lakes sampled. The dataset was used to determine depth-preferences of each of the taxa encountered, and to determine common threshold depths (i.e. those water depths where abrupt changes in the composition of the chironomid fauna take place). These data were subsequently used to produce site-specific (i.e. one lake) and regional (i.e. 7- or 8-lake) chironomid-water depth inference models.
    Keywords: Ablabesmyia; BloodyPond_BP-001; BloodyPond_BP-002; BloodyPond_BP-003; BloodyPond_BP-004; BloodyPond_BP-005; BloodyPond_BP-006; BloodyPond_BP-101; BloodyPond_BP-102; BloodyPond_BP-103; BloodyPond_BP-105; BloodyPond_BP-106; BloodyPond_BP-107; BloodyPond_BP-108; BloodyPond_BP-201; BloodyPond_BP-202; BloodyPond_BP-203; BloodyPond_BP-204; BloodyPond_BP-205; BloodyPond_BP-206; BP-001; BP-002; BP-003; BP-004; BP-005; BP-006; BP-101; BP-102; BP-103; BP-105; BP-106; BP-107; BP-108; BP-201; BP-202; BP-203; BP-204; BP-205; BP-206; Ceratopogonidae; Chaoborus; Chironomidae indeterminata; Chironomids; Chironomini indeterminata; Chironomus anthracinus-type; Chironomus plumosus-type; Cladopelma lateralis-type; Cladotanytarsus mancus-type; Cladotanytarsus-type A; Corynoneura edwardsi-type; Counting, microscope; CP-001; CP-002; CP-003; CP-004; CP-005; CP-006; CP-007; CP-008; CP-009; CP-010; CP-011; CP-012; CP-013; CP-014; CP-015; CP-016; CP-017; CP-018; CP-019; CP-020; CP-021; CP-022; CP-023; CP-024; CP-025; CP-026; Cricotopus bicinctus-type; Cricotopus cylindraceus-type; Cricotopus laricomalis-type; Cricotopus obnixus-type; Cricotopus trifasciatus-type; CrookedPond_CP-001; CrookedPond_CP-002; CrookedPond_CP-003; CrookedPond_CP-004; CrookedPond_CP-005; CrookedPond_CP-006; CrookedPond_CP-007; CrookedPond_CP-008; CrookedPond_CP-009; CrookedPond_CP-010; CrookedPond_CP-011; CrookedPond_CP-012; CrookedPond_CP-013; CrookedPond_CP-014; CrookedPond_CP-015; CrookedPond_CP-016; CrookedPond_CP-017; CrookedPond_CP-018; CrookedPond_CP-019; CrookedPond_CP-020; CrookedPond_CP-021; CrookedPond_CP-022; CrookedPond_CP-023; CrookedPond_CP-024; CrookedPond_CP-025; CrookedPond_CP-026; Cryptochironomus; Date/Time of event; DeepPond_DP-1; DeepPond_DP-2; DeepPond_DP-3; DeepPond_DP-4; DeepPond_DP-5; Demicryptochironomus; Depth, bathymetric; DEPTH, sediment/rock; DIC-001; DIC-002; DIC-101; DIC-102; DIC-103; DIC-104; DicksPond_DIC-001; DicksPond_DIC-002; DicksPond_DIC-101; DicksPond_DIC-102; DicksPond_DIC-103; DicksPond_DIC-104; Dicrotendipes nervosus-type; DP-1; DP-2; DP-3; DP-4; DP-5; Einfeldia; Endochironomus albipennis-type; Endochironomus impar-type; Event label; GC; Georthocladius; Glyptotendipes barbipes-type; Glyptotendipes severini-type; Gravity corer; Guttipelopia; Gymnometriocnemus/Bryophaenocladius; Heterotanytarsus; Heterotrissocladius grimshawi-type; Heterotrissocladius marcidus-type; Heterotrissocladius subpilosus-type; Labrundinia; Lake, depth, maximum; lake depth; Latitude of event; Lauterborniella/Zavreliella; Limnophyes; LittleWestPond_LWP-101; LittleWestPond_LWP-102; LittleWestPond_LWP-103; LittleWestPond_LWP-104; LittleWestPond_LWP-105; LittleWestPond_LWP-106; LittleWestPond_LWP-107; LittleWestPond_LWP-108; LittleWestPond_LWP-109; Longitude of event; LongPond_LOP-001; LongPond_LOP-002; LongPond_LOP-003; LongPond_LOP-004; LongPond_LOP-005; LongPond_LOP-006; LongPond_LOP-007; LongPond_LOP-008; LongPond_LOP-009; LongPond_LOP-010; LongPond_LOP-011; LongPond_LOP-012; LongPond_LOP-013; LongPond_LOP-014; LongPond_LOP-201; LongPond_LOP-203; LongPond_LOP-204; LongPond_LOP-205; LongPond_LOP-206; LongPond_LOP-207; LongPond_LOP-209; LongPond_LOP-210; LongPond_LOP-211; LongPond_LOP-212; LongPond_LOP-213; LOP-001; LOP-002; LOP-003; LOP-004; LOP-005; LOP-006; LOP-007; LOP-008; LOP-009; LOP-010; LOP-011; LOP-012; LOP-013; LOP-014; LOP-201; LOP-203; LOP-204; LOP-205; LOP-206; LOP-207; LOP-209; LOP-210; LOP-211; LOP-212; LOP-213; LWP-101; LWP-102; LWP-103; LWP-104; LWP-105; LWP-106; LWP-107; LWP-108; LWP-109; MIC-001; MIC-002; MIC-003; MIC-004; MIC-005; MIC-006; MIC-007; MIC-008; MIC-009; MIC-010; MIC-011; MIC-012; MIC-013; MIC-014; MIC-101; MIC-102; MIC-103; MIC-104; MIC-105; MIC-106; MIC-107; MIC-108; MIC-109; MIC-110; MIC-111; MicajahPond_MIC-001; MicajahPond_MIC-002; MicajahPond_MIC-003; MicajahPond_MIC-004; MicajahPond_MIC-005; MicajahPond_MIC-006; MicajahPond_MIC-007; MicajahPond_MIC-008; MicajahPond_MIC-009; MicajahPond_MIC-010; MicajahPond_MIC-011; MicajahPond_MIC-012; MicajahPond_MIC-013; MicajahPond_MIC-014; MicajahPond_MIC-101; MicajahPond_MIC-102; MicajahPond_MIC-103; MicajahPond_MIC-104; MicajahPond_MIC-105; MicajahPond_MIC-106; MicajahPond_MIC-107; MicajahPond_MIC-108; MicajahPond_MIC-109; MicajahPond_MIC-110; MicajahPond_MIC-111; Micropsectra insignilobus-type; Microtendipes pedellus-type; Nanocladius; Neostempellina; Nilothauma; Oliveridia; ORDINAL NUMBER; Orthocladiinae indeterminata; Pagastiella; Parachironomus potamogeti-type; Parachironomus varus-type; Parachironomus vitiosus-type; Paracladopelma; Parakiefferiella bathophila-type; Parakiefferiella triquetra-type; Parakiefferiella-type A; Paralauterborniella; Parametriocnemus/Paraphaenocladius; Paratanytarsus austriacus-type; Paratanytarsus penicillatus-type; Paratendipes albimanus-type; Paratendipes nudisquama-type; Phaenopsectra; Polypedilum; Polypedilum nubeculosum-type; Polypedilum sordens-type; Procladius; Psectrocladius calcaratus-type; Psectrocladius flavus-type; Psectrocladius sordidellus-type; Pseudochironomus; Pseudorthocladius; Pseudosmittia; Sample code/label; Smittia; Stempellina; Stempellinella/Zavrelia; Stenochironomus; Stictochironomus rosenschoeldi-type; Surface samples; Synorthocladius; Tanypodinae indeterminata; Tanytarsini indeterminata; Tanytarsus chinyensis-type; Tanytarsus glabrescens-type; Tanytarsus lugens-type; Tanytarsus mendax-type; Tanytarsus pallidicornis-type; Thienemanniella; Thienemannimyia; Tribelos; UnionPond_UP-001; UnionPond_UP-002; UnionPond_UP-003; UnionPond_UP-004; UnionPond_UP-005; UnionPond_UP-006; UnionPond_UP-007; UnionPond_UP-101; UnionPond_UP-102; UnionPond_UP-103; UnionPond_UP-104; UnionPond_UP-105; UnionPond_UP-106; UnionPond_UP-107; United States; Unniella; UP-001; UP-002; UP-003; UP-004; UP-005; UP-006; UP-007; UP-101; UP-102; UP-103; UP-104; UP-105; UP-106; UP-107; Xenochironomus; Zalutschia-type B; Zalutschia zalutschicola
    Type: Dataset
    Format: text/tab-separated-values, 11585 data points
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  • 10
    Publication Date: 1985-12-01
    Description: Previous reconstructions of the late Quaternary biogeographical history of lodgepole pine (Pinuscontorta Dougl.) have been based upon inferences from the modern geographical distribution of morphological and genetic variation. These studies have led to the widely accepted conclusion that relict populations of the Rocky Mountain subspecies of lodgepole pine (ssp. latifolia Engelm.) persisted in glacial refugia located in northwestern Canada. New fossil pollen evidence of the late Pleistocene and Holocene distribution of lodgepole pine in the western interior of Canada contradicts this view. Pinuscontorta ssp. latifolia migrated northward into Canada from refugia located south of the continental glacial limits and did not reach its northern range limits in the southern Yukon until the late Holocene.
    Print ISSN: 0045-5067
    Electronic ISSN: 1208-6037
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
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