Postglacial development of a marl and peat complex on the Precambrian Shield of northwestern Ontario
Identifieur interne : 000D03 ( Istex/Corpus ); précédent : 000D02; suivant : 000D04Postglacial development of a marl and peat complex on the Precambrian Shield of northwestern Ontario
Auteurs : S. H. Mcintyre ; H. C. Duthie ; B. C. WarnerSource :
- Journal of Paleolimnology [ 0921-2728 ] ; 1991-01-01.
Abstract
Abstract: This paper presents the first paleolimnological study of the postglacial development of a marl and peat complex on the Canadian Precambrian Shield. Ring Lake (48° 46′ N, 85° 51′ W), situated within the carbonate glacial drift area of northwestern Ontario, originated about 9000 BP in a basin exposed by the retreating waters of proglacial Lake Superior. The development of Ring Lake was interpreted from pollen and diatom analysis of one sediment core from the littoral zone and another core from near the lake centre. The sequence of postglacial vegetation development parallels published accounts of forest history in northern Ontario. The predominant diatom throughout the littoral core was the alkaliphilous Cymbella diluviana. The central core was dominated by circumneutral and alkaliphilous species of Achnanthes Navicula, Fragilaria, and Cymbella, except in recent samples where acidophilous species of Anomoeoneis were common. Diatom-inferred (DI) pH shows that the early lake was alkaline because of drainage from base-rich tills. The presence of marl in the littoral core indicates deposition of calcareous materials until the site dried out during the Hypsithermal period. There is evidence that beaver activity around 5000 BP caused a temporary change in lake hydrology. A decline in DI pH over much of the postglacial reflects gradual exhaustion of carbonates in the drainage area. An increase in acidophilous diatoms in samples representing the past 3500 y is consistent with gradual acidification of the system and development of a littoral peatland in a cooler neoglacial climate.
Url:
DOI: 10.1007/BF00153738
Links to Exploration step
ISTEX:5C63EF66C375E5AD172ED5B9B093F9DF1D0A92A9Le document en format XML
<record><TEI wicri:istexFullTextTei="biblStruct"><teiHeader><fileDesc><titleStmt><title xml:lang="en">Postglacial development of a marl and peat complex on the Precambrian Shield of northwestern Ontario</title><author><name sortKey="Mcintyre, S H" sort="Mcintyre, S H" uniqKey="Mcintyre S" first="S. H." last="Mcintyre">S. H. Mcintyre</name><affiliation><mods:affiliation>Department of Biology, University of Waterloo, N2L 3G1, Waterloo, Ontario, Canada</mods:affiliation></affiliation><affiliation><mods:affiliation>Quaternary Sciences Institute, University of Waterloo, N2L 3G1, Waterloo, Ontario, Canada</mods:affiliation></affiliation></author><author><name sortKey="Duthie, H C" sort="Duthie, H C" uniqKey="Duthie H" first="H. C." last="Duthie">H. C. Duthie</name><affiliation><mods:affiliation>Department of Biology, University of Waterloo, N2L 3G1, Waterloo, Ontario, Canada</mods:affiliation></affiliation><affiliation><mods:affiliation>Quaternary Sciences Institute, University of Waterloo, N2L 3G1, Waterloo, Ontario, Canada</mods:affiliation></affiliation></author><author><name sortKey="Warner, B C" sort="Warner, B C" uniqKey="Warner B" first="B. C." last="Warner">B. C. Warner</name><affiliation><mods:affiliation>Department of Geography, University of Waterloo, N2L 3G1, Waterloo, Ontario, Canada</mods:affiliation></affiliation><affiliation><mods:affiliation>Quaternary Sciences Institute, University of Waterloo, N2L 3G1, Waterloo, Ontario, Canada</mods:affiliation></affiliation></author></titleStmt><publicationStmt><idno type="wicri:source">ISTEX</idno><idno type="RBID">ISTEX:5C63EF66C375E5AD172ED5B9B093F9DF1D0A92A9</idno><date when="1991" year="1991">1991</date><idno type="doi">10.1007/BF00153738</idno><idno type="url">https://api.istex.fr/document/5C63EF66C375E5AD172ED5B9B093F9DF1D0A92A9/fulltext/pdf</idno><idno type="wicri:Area/Istex/Corpus">000D03</idno><idno type="wicri:explorRef" wicri:stream="Istex" wicri:step="Corpus" wicri:corpus="ISTEX">000D03</idno></publicationStmt><sourceDesc><biblStruct><analytic><title level="a" type="main" xml:lang="en">Postglacial development of a marl and peat complex on the Precambrian Shield of northwestern Ontario</title><author><name sortKey="Mcintyre, S H" sort="Mcintyre, S H" uniqKey="Mcintyre S" first="S. H." last="Mcintyre">S. H. Mcintyre</name><affiliation><mods:affiliation>Department of Biology, University of Waterloo, N2L 3G1, Waterloo, Ontario, Canada</mods:affiliation></affiliation><affiliation><mods:affiliation>Quaternary Sciences Institute, University of Waterloo, N2L 3G1, Waterloo, Ontario, Canada</mods:affiliation></affiliation></author><author><name sortKey="Duthie, H C" sort="Duthie, H C" uniqKey="Duthie H" first="H. C." last="Duthie">H. C. Duthie</name><affiliation><mods:affiliation>Department of Biology, University of Waterloo, N2L 3G1, Waterloo, Ontario, Canada</mods:affiliation></affiliation><affiliation><mods:affiliation>Quaternary Sciences Institute, University of Waterloo, N2L 3G1, Waterloo, Ontario, Canada</mods:affiliation></affiliation></author><author><name sortKey="Warner, B C" sort="Warner, B C" uniqKey="Warner B" first="B. C." last="Warner">B. C. Warner</name><affiliation><mods:affiliation>Department of Geography, University of Waterloo, N2L 3G1, Waterloo, Ontario, Canada</mods:affiliation></affiliation><affiliation><mods:affiliation>Quaternary Sciences Institute, University of Waterloo, N2L 3G1, Waterloo, Ontario, Canada</mods:affiliation></affiliation></author></analytic><monogr></monogr><series><title level="j">Journal of Paleolimnology</title><title level="j" type="abbrev">J Paleolimnol</title><idno type="ISSN">0921-2728</idno><idno type="eISSN">1573-0417</idno><imprint><publisher>Kluwer Academic Publishers</publisher><pubPlace>Dordrecht</pubPlace><date type="published" when="1991-01-01">1991-01-01</date><biblScope unit="volume">6</biblScope><biblScope unit="issue">2</biblScope><biblScope unit="page" from="141">141</biblScope><biblScope unit="page" to="155">155</biblScope></imprint><idno type="ISSN">0921-2728</idno></series><idno type="istex">5C63EF66C375E5AD172ED5B9B093F9DF1D0A92A9</idno><idno type="DOI">10.1007/BF00153738</idno><idno type="ArticleID">BF00153738</idno><idno type="ArticleID">Art6</idno></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0921-2728</idno></seriesStmt></fileDesc><profileDesc><textClass></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Abstract: This paper presents the first paleolimnological study of the postglacial development of a marl and peat complex on the Canadian Precambrian Shield. Ring Lake (48° 46′ N, 85° 51′ W), situated within the carbonate glacial drift area of northwestern Ontario, originated about 9000 BP in a basin exposed by the retreating waters of proglacial Lake Superior. The development of Ring Lake was interpreted from pollen and diatom analysis of one sediment core from the littoral zone and another core from near the lake centre. The sequence of postglacial vegetation development parallels published accounts of forest history in northern Ontario. The predominant diatom throughout the littoral core was the alkaliphilous Cymbella diluviana. The central core was dominated by circumneutral and alkaliphilous species of Achnanthes Navicula, Fragilaria, and Cymbella, except in recent samples where acidophilous species of Anomoeoneis were common. Diatom-inferred (DI) pH shows that the early lake was alkaline because of drainage from base-rich tills. The presence of marl in the littoral core indicates deposition of calcareous materials until the site dried out during the Hypsithermal period. There is evidence that beaver activity around 5000 BP caused a temporary change in lake hydrology. A decline in DI pH over much of the postglacial reflects gradual exhaustion of carbonates in the drainage area. An increase in acidophilous diatoms in samples representing the past 3500 y is consistent with gradual acidification of the system and development of a littoral peatland in a cooler neoglacial climate.</div></front></TEI><istex><corpusName>springer</corpusName><author><json:item><name>S. H. McIntyre</name><affiliations><json:string>Department of Biology, University of Waterloo, N2L 3G1, Waterloo, Ontario, Canada</json:string><json:string>Quaternary Sciences Institute, University of Waterloo, N2L 3G1, Waterloo, Ontario, Canada</json:string></affiliations></json:item><json:item><name>H. C. Duthie</name><affiliations><json:string>Department of Biology, University of Waterloo, N2L 3G1, Waterloo, Ontario, Canada</json:string><json:string>Quaternary Sciences Institute, University of Waterloo, N2L 3G1, Waterloo, Ontario, Canada</json:string></affiliations></json:item><json:item><name>B. C. Warner</name><affiliations><json:string>Department of Geography, University of Waterloo, N2L 3G1, Waterloo, Ontario, Canada</json:string><json:string>Quaternary Sciences Institute, University of Waterloo, N2L 3G1, Waterloo, Ontario, Canada</json:string></affiliations></json:item></author><articleId><json:string>BF00153738</json:string><json:string>Art6</json:string></articleId><language><json:string>eng</json:string></language><originalGenre><json:string>OriginalPaper</json:string></originalGenre><abstract>Abstract: This paper presents the first paleolimnological study of the postglacial development of a marl and peat complex on the Canadian Precambrian Shield. Ring Lake (48° 46′ N, 85° 51′ W), situated within the carbonate glacial drift area of northwestern Ontario, originated about 9000 BP in a basin exposed by the retreating waters of proglacial Lake Superior. The development of Ring Lake was interpreted from pollen and diatom analysis of one sediment core from the littoral zone and another core from near the lake centre. The sequence of postglacial vegetation development parallels published accounts of forest history in northern Ontario. The predominant diatom throughout the littoral core was the alkaliphilous Cymbella diluviana. The central core was dominated by circumneutral and alkaliphilous species of Achnanthes Navicula, Fragilaria, and Cymbella, except in recent samples where acidophilous species of Anomoeoneis were common. Diatom-inferred (DI) pH shows that the early lake was alkaline because of drainage from base-rich tills. The presence of marl in the littoral core indicates deposition of calcareous materials until the site dried out during the Hypsithermal period. There is evidence that beaver activity around 5000 BP caused a temporary change in lake hydrology. A decline in DI pH over much of the postglacial reflects gradual exhaustion of carbonates in the drainage area. An increase in acidophilous diatoms in samples representing the past 3500 y is consistent with gradual acidification of the system and development of a littoral peatland in a cooler neoglacial climate.</abstract><qualityIndicators><score>7.916</score><pdfVersion>1.3</pdfVersion><pdfPageSize>547.56 x 737.84 pts</pdfPageSize><refBibsNative>false</refBibsNative><keywordCount>0</keywordCount><abstractCharCount>1607</abstractCharCount><pdfWordCount>5747</pdfWordCount><pdfCharCount>33237</pdfCharCount><pdfPageCount>15</pdfPageCount><abstractWordCount>243</abstractWordCount></qualityIndicators><title>Postglacial development of a marl and peat complex on the Precambrian Shield of northwestern Ontario</title><refBibs><json:item><author><json:item><name>D,S R B Anderson</name></json:item><json:item><name> Davis</name></json:item></author><host><volume>131</volume><pages><last>143</last><first>133</first></pages><author></author><title>Hydrobiologia</title><publicationDate>1985</publicationDate></host><title>Relationships between diatom assemblages in lake surface-sediments and limnological characteristics in southern Norway</title><publicationDate>1985</publicationDate></json:item><json:item><host><author><json:item><name>A Bajc</name></json:item></author><title>Molluscan paleoecology and Superior basin water levels</title><publicationDate>1986</publicationDate></host></json:item><json:item><author><json:item><name>R,W Battarbee</name></json:item></author><host><volume>18</volume><pages><last>653</last><first>647</first></pages><author></author><title>Limnol. Oceanogr</title><publicationDate>1973</publicationDate></host><title>A new method for the estimation of absolute microfossil numbers, with reference especially to diatoms</title><publicationDate>1973</publicationDate></json:item><json:item><author><json:item><name>J Beaver</name></json:item></author><host><author></author><title>Ontario Ministry of the Environment</title><publicationDate>1981</publicationDate></host><title>Apparent ecological characteristics of some freshwater diatoms</title><publicationDate>1981</publicationDate></json:item><json:item><author><json:item><name>C,S Brousseau</name></json:item><json:item><name>D Baccante</name></json:item><json:item><name>&,L W Maki</name></json:item></author><host><volume>11</volume><pages><last>507</last><first>501</first></pages><author></author><title>J. Great Lakes Res</title><publicationDate>1985</publicationDate></host><title>Role of bedrock and surficial geology in determining the sensitivity of Thunder Bay area lakes to acidification</title><publicationDate>1985</publicationDate></json:item><json:item><author><json:item><name>R,W Butcher</name></json:item></author><host><volume>33</volume><pages><last>283</last><first>268</first></pages><author></author><title>J. Ecol</title><publicationDate>1946</publicationDate></host><title>Studies in the ecology of rivers. VI. The algal growth in certain highly calcareous streams</title><publicationDate>1946</publicationDate></json:item><json:item><host><pages><last>1986</last><first>1984</first></pages><author><json:item><name>K,E Camburn</name></json:item><json:item><name>J,C Kingston</name></json:item><json:item><name>&,D F Charles</name></json:item></author></host></json:item><json:item><author><json:item><name>P,T Cleve</name></json:item></author><host><volume>26</volume><pages><last>194</last><first>1</first></pages><issue>27</issue><author></author><title>K. Sv. Vet. Akad. Handl</title><publicationDate>1965</publicationDate></host><title>Synopsis of the naviculoid diatoms</title><publicationDate>1965</publicationDate></json:item><json:item><author><json:item><name>A Cleve-Euler</name></json:item></author><host><volume>2</volume><pages><last>163</last><first>1</first></pages><issue>54</issue><author></author><title>Die Diatomeen yon Schweden und Finland. K. Sv. Vet. Akad. Handl.; IV</title><publicationDate>1951</publicationDate></host><publicationDate>1951</publicationDate></json:item><json:item><author><json:item><name>E,J Cox</name></json:item></author><host><pages><last>172</last><first>163</first></pages><author></author><title>Proc. 8th Internat. Diatom Symposium</title><publicationDate>1984</publicationDate></host><title>Some taxomomic and ecological considerations of morphological variation with natural populations of benthic diatoms</title><publicationDate>1984</publicationDate></json:item><json:item><author><json:item><name>L,C Cwynar</name></json:item><json:item><name>E Burden</name></json:item><json:item><name>&,J H Mcandrews</name></json:item></author><host><volume>16</volume><pages><last>1120</last><first>1115</first></pages><author></author><title>Can. J. Earth Sci</title><publicationDate>1979</publicationDate></host><title>An inexpensive sieving method for concentrating pollen and spores from fine-gained sediments</title><publicationDate>1979</publicationDate></json:item><json:item><author><json:item><name> Dam</name></json:item><json:item><name>H Van</name></json:item><json:item><name>G Suurmond</name></json:item><json:item><name>&,C J F Braak</name></json:item></author><host><volume>83</volume><pages><last>459</last><first>425</first></pages><author></author><title>Hydrobiologia</title><publicationDate>1981</publicationDate></host><title>Impact of acidification on diatoms and chemistry of Dutch moorland pools</title><publicationDate>1981</publicationDate></json:item><json:item><author><json:item><name>W,E Dean</name></json:item><json:item><name> Jr</name></json:item></author><host><volume>44</volume><pages><last>248</last><first>242</first></pages><author></author><title>J. Sed. Petrol</title><publicationDate>1974</publicationDate></host><title>Determination of carbonate and organic matter in calcareous sediments and sedimentary rocks by loss on ignition: comparison with other methods</title><publicationDate>1974</publicationDate></json:item><json:item><author><json:item><name>L,D Delorme</name></json:item><json:item><name>H,C Duthie</name></json:item><json:item><name>S,R Esterby</name></json:item><json:item><name>S,M Smith</name></json:item><json:item><name>& N,S Harper</name></json:item></author><host><volume>108</volume><pages><last>22</last><first>1</first></pages><author></author><title>Arch. Hydrobiol</title><publicationDate>1986</publicationDate></host><title>Prehistoric inferred pH changes in Batchawana Lake, Ontario, from sedimentary diatom assemblages</title><publicationDate>1986</publicationDate></json:item><json:item><author><json:item><name>S,M D Dixit</name></json:item><json:item><name> Dickman</name></json:item></author><host><volume>120</volume><pages><last>80</last><first>69</first></pages><author></author><title>Hydrobiologia</title><publicationDate>1986</publicationDate></host><title>Correlation of surface sediment diatoms with the present lake water pH in 28 Algoma lakes</title><publicationDate>1986</publicationDate></json:item><json:item><author><json:item><name>N,M Dustin</name></json:item><json:item><name>B,H Wilkinson</name></json:item><json:item><name>&,R M Owen</name></json:item></author><host><volume>31</volume><pages><last>1311</last><first>1301</first></pages><author></author><title>Limnol. Oceanogr</title><publicationDate>1986</publicationDate></host><title>Littlefield Lake, Michigan: carbonate budget of Holocene sedimentation in a temperate-region lacustrine system</title><publicationDate>1986</publicationDate></json:item><json:item><author><json:item><name>G,H Evans</name></json:item></author><host><volume>69</volume><pages><last>874</last><first>821</first></pages><author></author><title>New Phytol</title><publicationDate>1970</publicationDate></host><title>Pollen and diatom analyses of late Quaternary deposits in the Belham Basin, North Lancashire</title><publicationDate>1970</publicationDate></json:item><json:item><host><author><json:item><name>K Faegri</name></json:item><json:item><name>P,E Kaland</name></json:item><json:item><name>&,K Krzywinski</name></json:item></author><title>Textbook of pollen analysis. Fourth edition</title><publicationDate>1989</publicationDate></host></json:item><json:item><author><json:item><name>R,S A F Geddes</name></json:item><json:item><name> Bajc</name></json:item></author><host><pages><first>3055</first></pages><author></author><title>Ontario Geological Survey</title><publicationDate>1985</publicationDate></host><title>Quaternary geology of the White Lake (Hemlo) area, District of Thunder Bay</title><publicationDate>1985</publicationDate></json:item><json:item><author><json:item><name>H,H Harvey</name></json:item><json:item><name>P,J Dillon</name></json:item><json:item><name>J,R Kramer</name></json:item><json:item><name>P,C Pierre</name></json:item><json:item><name>&,D M Whelpdale</name></json:item></author><host><pages><first>369</first></pages><author></author><title>National Research Council of Canada. PuN. C-18475</title><publicationDate>1981</publicationDate></host><title>Acidification in the Canadian aquatic environment: scientific criteria for assessing the effects of acidic deposition on aquatic ecosystems</title><publicationDate>1981</publicationDate></json:item><json:item><author><json:item><name>R,E P Hecky</name></json:item><json:item><name> Kilham</name></json:item></author><host><volume>18</volume><pages><last>71</last><first>53</first></pages><author></author><title>Limnol. Oceanogr</title><publicationDate>1973</publicationDate></host><title>Diatoms in alkaline saline lakes: ecology and geochemical implications</title><publicationDate>1973</publicationDate></json:item><json:item><author><json:item><name>H,P R W Hostetter</name></json:item><json:item><name> Hoshaw</name></json:item></author><host><volume>8</volume><pages><last>296</last><first>289</first></pages><author></author><title>J. Phycol</title><publicationDate>1972</publicationDate></host><title>Asexual developmental patterns of the diatom Stauroneis anceps in culture</title><publicationDate>1972</publicationDate></json:item><json:item><author><json:item><name>C Hudon</name></json:item><json:item><name>H,C Duthie</name></json:item><json:item><name>S,M Smith</name></json:item><json:item><name>&,S A Ditner</name></json:item></author><host><volume>140</volume><pages><last>65</last><first>49</first></pages><author></author><title>Hydrobiologia</title><publicationDate>1986</publicationDate></host><title>Relationships between lakewater pH and sedimentary diatoms in the Matamek Watershed</title><publicationDate>1986</publicationDate></json:item><json:item><author><json:item><name>F Hustedt</name></json:item></author><host><pages><last>192</last><first>1</first></pages><author></author><title>Akademische Verlagsgesellschaft</title><publicationDate>1927</publicationDate></host><title>Die Kieselalgen, Deutschlands, ()sterreichs , und der Schweiz</title><publicationDate>1927</publicationDate></json:item><json:item><author><json:item><name>P,F R S Karrow</name></json:item><json:item><name> Geddes</name></json:item></author><host><volume>24</volume><pages><last>369</last><first>365</first></pages><author></author><title>Can. J. Earth. Sci</title><publicationDate>1987</publicationDate></host><title>Drift carbonate on the Canadian Shield</title><publicationDate>1987</publicationDate></json:item><json:item><author><json:item><name>K,B Liu</name></json:item></author><host><volume>60</volume><pages><last>212</last><first>179</first></pages><author></author><title>Ecol. Monogr</title><publicationDate>1990</publicationDate></host><title>Holocene paleoecology of the boreal forest and Great Lakes-St. Lawrence forest in northern Ontario</title><publicationDate>1990</publicationDate></json:item><json:item><author><json:item><name>R,L Lowe</name></json:item></author><host><volume>670</volume><pages><last>74</last><first>4</first></pages><author></author><title>U.S. EPA</title><publicationDate>1974</publicationDate></host><title>Environmental requirements and pollution tolerances of freshwater diatoms</title><publicationDate>1974</publicationDate></json:item><json:item><author><json:item><name>A,M Mannion</name></json:item></author><host><volume>5</volume><pages><last>318</last><first>301</first></pages><author></author><title>J. Biogeogr</title><publicationDate>1978</publicationDate></host><title>Late Quaternary deposits from southest Scotland. II. The diatom assemblage of a marl core</title><publicationDate>1978</publicationDate></json:item><json:item><host><pages><last>333</last><first>319</first></pages><author><json:item><name>J,H Mcandrews</name></json:item></author><title>Late Quaternary climate of Ontario: temperature trends from the fossil pollen record</title><publicationDate>1981</publicationDate></host></json:item><json:item><author><json:item><name>S,H Mcintyre</name></json:item></author><host><pages><first>187</first></pages><author></author><title>Canada. M. Sc. thesis</title><publicationDate>1990</publicationDate></host><title>Postglacial pH history of a naturally acidified lake in northern Ontario</title><publicationDate>1990</publicationDate></json:item><json:item><author><json:item><name>J Meril~iinen</name></json:item></author><host><volume>4</volume><pages><last>58</last><first>51</first></pages><author></author><title>Ann. Bot. fenn</title><publicationDate>1967</publicationDate></host><title>The diatom flora and the hydrogen-ion concentration of the water</title><publicationDate>1967</publicationDate></json:item><json:item><author><json:item><name>A,R G Otsuki</name></json:item><json:item><name> Wetzel</name></json:item></author><host><volume>73</volume><pages><last>30</last><first>14</first></pages><author></author><title>Arch. Hydrobiol</title><publicationDate>1974</publicationDate></host><title>Calcium and total alkalinity budgets and calcium carbonate precipitation of a small hard-water lake</title><publicationDate>1974</publicationDate></json:item><json:item><author><json:item><name>R,C W Patrick</name></json:item><json:item><name> Reirner</name></json:item></author><host><pages><first>688</first></pages><author></author><title>The diatoms of the United States</title><publicationDate>1966</publicationDate></host><publicationDate>1966</publicationDate></json:item><json:item><author><json:item><name>R,C W Patrick</name></json:item><json:item><name> Reimer</name></json:item></author><host><pages><first>213</first></pages><author></author><title>The diatoms of the United States</title><publicationDate>1975</publicationDate></host><publicationDate>1975</publicationDate></json:item><json:item><author><json:item><name>D,J Rawlence</name></json:item></author><host><volume>1</volume><pages><last>60</last><first>51</first></pages><author></author><title>New Brunswick. J. Paleo</title><publicationDate>1988</publicationDate></host><title>The post-glacial diatom history of Splan Lake</title><publicationDate>1988</publicationDate></json:item><json:item><author><json:item><name>I,T Renberg</name></json:item><json:item><name> Hellberg</name></json:item></author><host><volume>11</volume><pages><last>33</last><first>30</first></pages><author></author><title>Ambio</title><publicationDate>1982</publicationDate></host><title>The pH history of lakes in southwestern Sweden, as calculated from the subfossil diatom flora of the sediments</title><publicationDate>1982</publicationDate></json:item><json:item><author><json:item><name>M Saarnisto</name></json:item></author><host><volume>4</volume><pages><last>339</last><first>316</first></pages><author></author><title>Quat. Res</title><publicationDate>1974</publicationDate></host><title>The deglaciation of the Lake Superior region and its climatic implications</title><publicationDate>1974</publicationDate></json:item><json:item><host><pages><first>50</first></pages><author><json:item><name>F,R R E M Schoeman</name></json:item><json:item><name> Archibald</name></json:item></author><title>The diatom flora of southern Africa No. 6. Council for Scientific and Industrial Research. Special Rep</title><publicationDate>1980</publicationDate></host></json:item><json:item><author><json:item><name>M,R H C Sreenivasa</name></json:item><json:item><name> Duthie</name></json:item></author><host><volume>51</volume><pages><last>1605</last><first>159</first></pages><author></author><title>Can. J. Bot</title><publicationDate>1973</publicationDate></host><title>The postglacial diatom history of Sunfish Lake, southwestern Ontario</title><publicationDate>1973</publicationDate></json:item><json:item><author><json:item><name>M,C Taylor</name></json:item><json:item><name>H,C Duthie</name></json:item><json:item><name>&,S M Smith</name></json:item></author><host><pages><last>280</last><first>273</first></pages><author></author><title>Proc. 9th Internat. Diatom. Symp</title><publicationDate>1986</publicationDate></host><title>Errors associated with diatom-inferred pH indices for predicting pH in Canadian Shield lakes</title><publicationDate>1986</publicationDate></json:item><json:item><author><json:item><name>R Tippett</name></json:item></author><host><volume>42</volume><pages><last>1709</last><first>1693</first></pages><author></author><title>Can. J. Bot</title><publicationDate>1964</publicationDate></host><title>An investigation into the nature of the layering of deep water sediment in two eastern Ontario lakes</title><publicationDate>1964</publicationDate></json:item><json:item><author><json:item><name>K,L B H Treese</name></json:item><json:item><name> Wilkinson</name></json:item></author><host><volume>9</volume><pages><last>390</last><first>375</first></pages><author></author><title>Sedimentology</title><publicationDate>1982</publicationDate></host><title>Peat-marl deposition in a Holocene paludaMacustrme basin -Sucker Lake, Michigan</title><publicationDate>1982</publicationDate></json:item><json:item><author><json:item><name>R,G Wetzel</name></json:item></author><host><pages><first>743</first></pages><author></author><title>Limnology. W.B. Saunders</title><publicationDate>1975</publicationDate></host><publicationDate>1975</publicationDate></json:item><json:item><author><json:item><name>R,G B A Wetzel</name></json:item><json:item><name> Manny</name></json:item></author><host><volume>25</volume><pages><last>469</last><first>453</first></pages><author></author><title>Polish Arch. Hydrobiol</title><publicationDate>1978</publicationDate></host><title>Postglacial rates of sedimentation , nutrient and fossil pigment deposition in a hardwater marl lake of Michigan</title><publicationDate>1978</publicationDate></json:item><json:item><author><json:item><name>T,J Whitmore</name></json:item></author><host><volume>34</volume><pages><last>895</last><first>882</first></pages><author></author><title>Limnol. Oceanogr</title><publicationDate>1989</publicationDate></host><title>Florida diatom assemblages as indicators of trophic status and pH</title><publicationDate>1989</publicationDate></json:item><json:item><author><json:item><name>H,E Wright</name></json:item><json:item><name>D,H Mann</name></json:item><json:item><name>&,P H Glaser</name></json:item></author><host><volume>65</volume><pages><last>659</last><first>657</first></pages><author></author><title>Ecology</title><publicationDate>1984</publicationDate></host><title>Piston corers for peat and lake sediments</title><publicationDate>1984</publicationDate></json:item><json:item><author><json:item><name>O,F Yakushko</name></json:item><json:item><name>N,A Makhnach</name></json:item><json:item><name>G,K Khursevich</name></json:item><json:item><name>&,I A Mislivets</name></json:item></author><host><pages><last>206</last><first>203</first></pages><author></author><title>General features of the development of carbonate accumulations in Byelorussian and Mazurian lakelands</title><publicationDate>1978</publicationDate></host><publicationDate>1978</publicationDate></json:item></refBibs><genre><json:string>research-article</json:string></genre><host><volume>6</volume><pages><last>155</last><first>141</first></pages><issn><json:string>0921-2728</json:string></issn><issue>2</issue><subject><json:item><value>Geochemistry</value></json:item><json:item><value>Hydrogeology</value></json:item><json:item><value>Meteorology/Climatology</value></json:item><json:item><value>Sedimentology</value></json:item><json:item><value>Hydrobiology</value></json:item></subject><journalId><json:string>10933</json:string></journalId><genre><json:string>journal</json:string></genre><language><json:string>unknown</json:string></language><eissn><json:string>1573-0417</json:string></eissn><title>Journal of Paleolimnology</title><publicationDate>1991</publicationDate><copyrightDate>1991</copyrightDate></host><publicationDate>1991</publicationDate><copyrightDate>1991</copyrightDate><doi><json:string>10.1007/BF00153738</json:string></doi><id>5C63EF66C375E5AD172ED5B9B093F9DF1D0A92A9</id><score>1</score><fulltext><json:item><extension>pdf</extension><original>true</original><mimetype>application/pdf</mimetype><uri>https://api.istex.fr/document/5C63EF66C375E5AD172ED5B9B093F9DF1D0A92A9/fulltext/pdf</uri></json:item><json:item><extension>zip</extension><original>false</original><mimetype>application/zip</mimetype><uri>https://api.istex.fr/document/5C63EF66C375E5AD172ED5B9B093F9DF1D0A92A9/fulltext/zip</uri></json:item><istex:fulltextTEI uri="https://api.istex.fr/document/5C63EF66C375E5AD172ED5B9B093F9DF1D0A92A9/fulltext/tei"><teiHeader><fileDesc><titleStmt><title level="a" type="main" xml:lang="en">Postglacial development of a marl and peat complex on the Precambrian Shield of northwestern Ontario</title><respStmt><resp>Références bibliographiques récupérées via GROBID</resp><name resp="ISTEX-API">ISTEX-API (INIST-CNRS)</name></respStmt><respStmt><resp>Références bibliographiques récupérées via GROBID</resp><name resp="ISTEX-API">ISTEX-API (INIST-CNRS)</name></respStmt></titleStmt><publicationStmt><authority>ISTEX</authority><publisher>Kluwer Academic Publishers</publisher><pubPlace>Dordrecht</pubPlace><availability><p>Kluwer Academic Publishers, 1991</p></availability><date>1991-05-27</date></publicationStmt><sourceDesc><biblStruct type="inbook"><analytic><title level="a" type="main" xml:lang="en">Postglacial development of a marl and peat complex on the Precambrian Shield of northwestern Ontario</title><author xml:id="author-1"><persName><forename type="first">S.</forename><surname>McIntyre</surname></persName><affiliation>Department of Biology, University of Waterloo, N2L 3G1, Waterloo, Ontario, Canada</affiliation><affiliation>Quaternary Sciences Institute, University of Waterloo, N2L 3G1, Waterloo, Ontario, Canada</affiliation></author><author xml:id="author-2"><persName><forename type="first">H.</forename><surname>Duthie</surname></persName><affiliation>Department of Biology, University of Waterloo, N2L 3G1, Waterloo, Ontario, Canada</affiliation><affiliation>Quaternary Sciences Institute, University of Waterloo, N2L 3G1, Waterloo, Ontario, Canada</affiliation></author><author xml:id="author-3"><persName><forename type="first">B.</forename><surname>Warner</surname></persName><affiliation>Department of Geography, University of Waterloo, N2L 3G1, Waterloo, Ontario, Canada</affiliation><affiliation>Quaternary Sciences Institute, University of Waterloo, N2L 3G1, Waterloo, Ontario, Canada</affiliation></author></analytic><monogr><title level="j">Journal of Paleolimnology</title><title level="j" type="abbrev">J Paleolimnol</title><idno type="journal-ID">10933</idno><idno type="pISSN">0921-2728</idno><idno type="eISSN">1573-0417</idno><idno type="issue-article-count">9</idno><idno type="volume-issue-count">3</idno><imprint><publisher>Kluwer Academic Publishers</publisher><pubPlace>Dordrecht</pubPlace><date type="published" when="1991-01-01"></date><biblScope unit="volume">6</biblScope><biblScope unit="issue">2</biblScope><biblScope unit="page" from="141">141</biblScope><biblScope unit="page" to="155">155</biblScope></imprint></monogr><idno type="istex">5C63EF66C375E5AD172ED5B9B093F9DF1D0A92A9</idno><idno type="DOI">10.1007/BF00153738</idno><idno type="ArticleID">BF00153738</idno><idno type="ArticleID">Art6</idno></biblStruct></sourceDesc></fileDesc><profileDesc><creation><date>1991-05-27</date></creation><langUsage><language ident="en">en</language></langUsage><abstract xml:lang="en"><p>Abstract: This paper presents the first paleolimnological study of the postglacial development of a marl and peat complex on the Canadian Precambrian Shield. Ring Lake (48° 46′ N, 85° 51′ W), situated within the carbonate glacial drift area of northwestern Ontario, originated about 9000 BP in a basin exposed by the retreating waters of proglacial Lake Superior. The development of Ring Lake was interpreted from pollen and diatom analysis of one sediment core from the littoral zone and another core from near the lake centre. The sequence of postglacial vegetation development parallels published accounts of forest history in northern Ontario. The predominant diatom throughout the littoral core was the alkaliphilous Cymbella diluviana. The central core was dominated by circumneutral and alkaliphilous species of Achnanthes Navicula, Fragilaria, and Cymbella, except in recent samples where acidophilous species of Anomoeoneis were common. Diatom-inferred (DI) pH shows that the early lake was alkaline because of drainage from base-rich tills. The presence of marl in the littoral core indicates deposition of calcareous materials until the site dried out during the Hypsithermal period. There is evidence that beaver activity around 5000 BP caused a temporary change in lake hydrology. A decline in DI pH over much of the postglacial reflects gradual exhaustion of carbonates in the drainage area. An increase in acidophilous diatoms in samples representing the past 3500 y is consistent with gradual acidification of the system and development of a littoral peatland in a cooler neoglacial climate.</p></abstract><textClass><keywords scheme="Journal Subject"><list><head>Life Sciences</head><item><term>Geochemistry</term></item><item><term>Hydrogeology</term></item><item><term>Meteorology/Climatology</term></item><item><term>Sedimentology</term></item><item><term>Hydrobiology</term></item></list></keywords></textClass></profileDesc><revisionDesc><change when="1991-05-27">Created</change><change when="1991-01-01">Published</change><change xml:id="refBibs-istex" who="#ISTEX-API" when="2016-11-22">References added</change><change xml:id="refBibs-istex" who="#ISTEX-API" when="2017-01-20">References added</change></revisionDesc></teiHeader></istex:fulltextTEI><json:item><extension>txt</extension><original>false</original><mimetype>text/plain</mimetype><uri>https://api.istex.fr/document/5C63EF66C375E5AD172ED5B9B093F9DF1D0A92A9/fulltext/txt</uri></json:item></fulltext><metadata><istex:metadataXml wicri:clean="Springer, Publisher found" wicri:toSee="no header"><istex:xmlDeclaration>version="1.0" encoding="UTF-8"</istex:xmlDeclaration><istex:docType PUBLIC="-//Springer-Verlag//DTD A++ V2.4//EN" URI="http://devel.springer.de/A++/V2.4/DTD/A++V2.4.dtd" name="istex:docType"></istex:docType><istex:document><Publisher><PublisherInfo><PublisherName>Kluwer Academic Publishers</PublisherName><PublisherLocation>Dordrecht</PublisherLocation></PublisherInfo><Journal><JournalInfo JournalProductType="ArchiveJournal" NumberingStyle="Unnumbered"><JournalID>10933</JournalID><JournalPrintISSN>0921-2728</JournalPrintISSN><JournalElectronicISSN>1573-0417</JournalElectronicISSN><JournalTitle>Journal of Paleolimnology</JournalTitle><JournalAbbreviatedTitle>J Paleolimnol</JournalAbbreviatedTitle><JournalSubjectGroup><JournalSubject Type="Primary">Life Sciences</JournalSubject><JournalSubject Type="Secondary">Geochemistry</JournalSubject><JournalSubject Type="Secondary">Hydrogeology</JournalSubject><JournalSubject Type="Secondary">Meteorology/Climatology</JournalSubject><JournalSubject Type="Secondary">Sedimentology</JournalSubject><JournalSubject Type="Secondary">Hydrobiology</JournalSubject></JournalSubjectGroup></JournalInfo><Volume><VolumeInfo VolumeType="Regular" TocLevels="0"><VolumeIDStart>6</VolumeIDStart><VolumeIDEnd>6</VolumeIDEnd><VolumeIssueCount>3</VolumeIssueCount></VolumeInfo><Issue IssueType="Regular"><IssueInfo TocLevels="0"><IssueIDStart>2</IssueIDStart><IssueIDEnd>2</IssueIDEnd><IssueArticleCount>9</IssueArticleCount><IssueHistory><CoverDate><DateString>1991</DateString><Year>1991</Year><Month>1</Month></CoverDate></IssueHistory><IssueCopyright><CopyrightHolderName>Kluwer Academic Publishers</CopyrightHolderName><CopyrightYear>1991</CopyrightYear></IssueCopyright></IssueInfo><Article ID="Art6"><ArticleInfo Language="En" ArticleType="OriginalPaper" NumberingStyle="Unnumbered" TocLevels="0" ContainsESM="No"><ArticleID>BF00153738</ArticleID><ArticleDOI>10.1007/BF00153738</ArticleDOI><ArticleSequenceNumber>6</ArticleSequenceNumber><ArticleTitle Language="En">Postglacial development of a marl and peat complex on the Precambrian Shield of northwestern Ontario</ArticleTitle><ArticleFirstPage>141</ArticleFirstPage><ArticleLastPage>155</ArticleLastPage><ArticleHistory><RegistrationDate><Year>2004</Year><Month>6</Month><Day>22</Day></RegistrationDate><Received><Year>1991</Year><Month>5</Month><Day>27</Day></Received><Accepted><Year>1991</Year><Month>10</Month><Day>10</Day></Accepted></ArticleHistory><ArticleCopyright><CopyrightHolderName>Kluwer Academic Publishers</CopyrightHolderName><CopyrightYear>1991</CopyrightYear></ArticleCopyright><ArticleGrants Type="Regular"><MetadataGrant Grant="OpenAccess"></MetadataGrant><AbstractGrant Grant="OpenAccess"></AbstractGrant><BodyPDFGrant Grant="Restricted"></BodyPDFGrant><BodyHTMLGrant Grant="Restricted"></BodyHTMLGrant><BibliographyGrant Grant="Restricted"></BibliographyGrant><ESMGrant Grant="Restricted"></ESMGrant></ArticleGrants><ArticleContext><JournalID>10933</JournalID><VolumeIDStart>6</VolumeIDStart><VolumeIDEnd>6</VolumeIDEnd><IssueIDStart>2</IssueIDStart><IssueIDEnd>2</IssueIDEnd></ArticleContext></ArticleInfo><ArticleHeader><AuthorGroup><Author AffiliationIDS="Aff1 Aff2"><AuthorName DisplayOrder="Western"><GivenName>S.</GivenName><GivenName>H.</GivenName><FamilyName>McIntyre</FamilyName></AuthorName></Author><Author AffiliationIDS="Aff1 Aff2"><AuthorName DisplayOrder="Western"><GivenName>H.</GivenName><GivenName>C.</GivenName><FamilyName>Duthie</FamilyName></AuthorName></Author><Author AffiliationIDS="Aff3 Aff4"><AuthorName DisplayOrder="Western"><GivenName>B.</GivenName><GivenName>C.</GivenName><FamilyName>Warner</FamilyName></AuthorName></Author><Affiliation ID="Aff1"><OrgDivision>Department of Biology</OrgDivision><OrgName>University of Waterloo</OrgName><OrgAddress><Postcode>N2L 3G1</Postcode><City>Waterloo</City><State>Ontario</State><Country>Canada</Country></OrgAddress></Affiliation><Affiliation ID="Aff2"><OrgDivision>Quaternary Sciences Institute</OrgDivision><OrgName>University of Waterloo</OrgName><OrgAddress><Postcode>N2L 3G1</Postcode><City>Waterloo</City><State>Ontario</State><Country>Canada</Country></OrgAddress></Affiliation><Affiliation ID="Aff3"><OrgDivision>Department of Geography</OrgDivision><OrgName>University of Waterloo</OrgName><OrgAddress><Postcode>N2L 3G1</Postcode><City>Waterloo</City><State>Ontario</State><Country>Canada</Country></OrgAddress></Affiliation><Affiliation ID="Aff4"><OrgDivision>Quaternary Sciences Institute</OrgDivision><OrgName>University of Waterloo</OrgName><OrgAddress><Postcode>N2L 3G1</Postcode><City>Waterloo</City><State>Ontario</State><Country>Canada</Country></OrgAddress></Affiliation></AuthorGroup><Abstract ID="Abs1" Language="En"><Heading>Abstract</Heading><Para>This paper presents the first paleolimnological study of the postglacial development of a marl and peat complex on the Canadian Precambrian Shield. Ring Lake (48° 46′ N, 85° 51′ W), situated within the carbonate glacial drift area of northwestern Ontario, originated about 9000 BP in a basin exposed by the retreating waters of proglacial Lake Superior. The development of Ring Lake was interpreted from pollen and diatom analysis of one sediment core from the littoral zone and another core from near the lake centre.</Para><Para>The sequence of postglacial vegetation development parallels published accounts of forest history in northern Ontario. The predominant diatom throughout the littoral core was the alkaliphilous <Emphasis Type="Italic">Cymbella diluviana</Emphasis>. The central core was dominated by circumneutral and alkaliphilous species of <Emphasis Type="Italic">Achnanthes Navicula, Fragilaria</Emphasis>, and <Emphasis Type="Italic">Cymbella</Emphasis>, except in recent samples where acidophilous species of <Emphasis Type="Italic">Anomoeoneis</Emphasis> were common.</Para><Para>Diatom-inferred (DI) pH shows that the early lake was alkaline because of drainage from base-rich tills. The presence of marl in the littoral core indicates deposition of calcareous materials until the site dried out during the Hypsithermal period. There is evidence that beaver activity around 5000 BP caused a temporary change in lake hydrology. A decline in DI pH over much of the postglacial reflects gradual exhaustion of carbonates in the drainage area. An increase in acidophilous diatoms in samples representing the past 3500 y is consistent with gradual acidification of the system and development of a littoral peatland in a cooler neoglacial climate.</Para></Abstract><KeywordGroup Language="En"><Heading>Key words</Heading><Keyword>marl lakes</Keyword><Keyword>paleolimnology</Keyword><Keyword>diatom-inferred pH</Keyword><Keyword>palynology</Keyword><Keyword>Hypsithermal</Keyword><Keyword>wetlands</Keyword></KeywordGroup></ArticleHeader><NoBody></NoBody></Article></Issue></Volume></Journal></Publisher></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>Postglacial development of a marl and peat complex on the Precambrian Shield of northwestern Ontario</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>Postglacial development of a marl and peat complex on the Precambrian Shield of northwestern Ontario</title></titleInfo><name type="personal"><namePart type="given">S.</namePart><namePart type="given">H.</namePart><namePart type="family">McIntyre</namePart><affiliation>Department of Biology, University of Waterloo, N2L 3G1, Waterloo, Ontario, Canada</affiliation><affiliation>Quaternary Sciences Institute, University of Waterloo, N2L 3G1, Waterloo, Ontario, Canada</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">H.</namePart><namePart type="given">C.</namePart><namePart type="family">Duthie</namePart><affiliation>Department of Biology, University of Waterloo, N2L 3G1, Waterloo, Ontario, Canada</affiliation><affiliation>Quaternary Sciences Institute, University of Waterloo, N2L 3G1, Waterloo, Ontario, Canada</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">B.</namePart><namePart type="given">C.</namePart><namePart type="family">Warner</namePart><affiliation>Department of Geography, University of Waterloo, N2L 3G1, Waterloo, Ontario, Canada</affiliation><affiliation>Quaternary Sciences Institute, University of Waterloo, N2L 3G1, Waterloo, Ontario, Canada</affiliation><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><genre type="research-article" displayLabel="OriginalPaper"></genre><originInfo><publisher>Kluwer Academic Publishers</publisher><place><placeTerm type="text">Dordrecht</placeTerm></place><dateCreated encoding="w3cdtf">1991-05-27</dateCreated><dateIssued encoding="w3cdtf">1991-01-01</dateIssued><copyrightDate encoding="w3cdtf">1991</copyrightDate></originInfo><language><languageTerm type="code" authority="rfc3066">en</languageTerm><languageTerm type="code" authority="iso639-2b">eng</languageTerm></language><physicalDescription><internetMediaType>text/html</internetMediaType></physicalDescription><abstract lang="en">Abstract: This paper presents the first paleolimnological study of the postglacial development of a marl and peat complex on the Canadian Precambrian Shield. Ring Lake (48° 46′ N, 85° 51′ W), situated within the carbonate glacial drift area of northwestern Ontario, originated about 9000 BP in a basin exposed by the retreating waters of proglacial Lake Superior. The development of Ring Lake was interpreted from pollen and diatom analysis of one sediment core from the littoral zone and another core from near the lake centre. The sequence of postglacial vegetation development parallels published accounts of forest history in northern Ontario. The predominant diatom throughout the littoral core was the alkaliphilous Cymbella diluviana. The central core was dominated by circumneutral and alkaliphilous species of Achnanthes Navicula, Fragilaria, and Cymbella, except in recent samples where acidophilous species of Anomoeoneis were common. Diatom-inferred (DI) pH shows that the early lake was alkaline because of drainage from base-rich tills. The presence of marl in the littoral core indicates deposition of calcareous materials until the site dried out during the Hypsithermal period. There is evidence that beaver activity around 5000 BP caused a temporary change in lake hydrology. A decline in DI pH over much of the postglacial reflects gradual exhaustion of carbonates in the drainage area. An increase in acidophilous diatoms in samples representing the past 3500 y is consistent with gradual acidification of the system and development of a littoral peatland in a cooler neoglacial climate.</abstract><relatedItem type="host"><titleInfo><title>Journal of Paleolimnology</title></titleInfo><titleInfo type="abbreviated"><title>J Paleolimnol</title></titleInfo><genre type="journal" displayLabel="Archive Journal"></genre><originInfo><dateIssued encoding="w3cdtf">1991-01-01</dateIssued><copyrightDate encoding="w3cdtf">1991</copyrightDate></originInfo><subject><genre>Life Sciences</genre><topic>Geochemistry</topic><topic>Hydrogeology</topic><topic>Meteorology/Climatology</topic><topic>Sedimentology</topic><topic>Hydrobiology</topic></subject><identifier type="ISSN">0921-2728</identifier><identifier type="eISSN">1573-0417</identifier><identifier type="JournalID">10933</identifier><identifier type="IssueArticleCount">9</identifier><identifier type="VolumeIssueCount">3</identifier><part><date>1991</date><detail type="volume"><number>6</number><caption>vol.</caption></detail><detail type="issue"><number>2</number><caption>no.</caption></detail><extent unit="pages"><start>141</start><end>155</end></extent></part><recordInfo><recordOrigin>Kluwer Academic Publishers, 1991</recordOrigin></recordInfo></relatedItem><identifier type="istex">5C63EF66C375E5AD172ED5B9B093F9DF1D0A92A9</identifier><identifier type="DOI">10.1007/BF00153738</identifier><identifier type="ArticleID">BF00153738</identifier><identifier type="ArticleID">Art6</identifier><accessCondition type="use and reproduction" contentType="copyright">Kluwer Academic Publishers, 1991</accessCondition><recordInfo><recordContentSource>SPRINGER</recordContentSource><recordOrigin>Kluwer Academic Publishers, 1991</recordOrigin></recordInfo></mods></metadata><serie></serie></istex></record>Pour manipuler ce document sous Unix (Dilib)
EXPLOR_STEP=$WICRI_ROOT/Wicri/Bois/explor/CheneBelgiqueV1/Data/Istex/Corpus
HfdSelect -h $EXPLOR_STEP/biblio.hfd -nk 000D03 | SxmlIndent | more
Ou
HfdSelect -h $EXPLOR_AREA/Data/Istex/Corpus/biblio.hfd -nk 000D03 | SxmlIndent | more
Pour mettre un lien sur cette page dans le réseau Wicri
{{Explor lien
|wiki= Wicri/Bois
|area= CheneBelgiqueV1
|flux= Istex
|étape= Corpus
|type= RBID
|clé= ISTEX:5C63EF66C375E5AD172ED5B9B093F9DF1D0A92A9
|texte= Postglacial development of a marl and peat complex on the Precambrian Shield of northwestern Ontario
}}
| This area was generated with Dilib version V0.6.27. |  |