The World's Great Lakes
Most of the large lakes lie in glacial scour basins in the northern hemisphere. These lakes are closely similar in physicochemical characteristics and in their biota. Most of the other large lakes are tectonic in origin and they differ greatly among themselves and from other lakes since they occur i...
Gespeichert in:
| Veröffentlicht in: | Journal of Great Lakes research 1984, Vol.10 (2), p.106-113 |
|---|---|
| 1. Verfasser: | |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 113 |
|---|---|
| container_issue | 2 |
| container_start_page | 106 |
| container_title | Journal of Great Lakes research |
| container_volume | 10 |
| creator | Beeton, Alfred M. |
| description | Most of the large lakes lie in glacial scour basins in the northern hemisphere. These lakes are closely similar in physicochemical characteristics and in their biota. Most of the other large lakes are tectonic in origin and they differ greatly among themselves and from other lakes since they occur in a diversity of terrestrial environments under a broad range of climatic conditions. Large lakes have a great diversity of habitats resulting in great species diversity and endemism in ancient lakes. The pronounced horizontal gradients in physicochemical conditions in large lakes contribute to the diversity of habitats. Conditions found in Lakes Michigan and Skadar are examples. |
| doi_str_mv | 10.1016/S0380-1330(84)71817-X |
| format | Article |
| fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_14362306</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><els_id>S038013308471817X</els_id><sourcerecordid>14132073</sourcerecordid><originalsourceid>FETCH-LOGICAL-a416t-9b2d5706800977eb6b594c14dc0d5c06796d64eea511d26eda158359d1c134633</originalsourceid><addsrcrecordid>eNqNkDtLA0EUhadQMD5qKzGVj2L13p3XbiUSNAoBiySYbpjM3OjoJhtnNoL_3iQrtlpdOHznXPgYO0G4QkB1PQReQIacw0UhLjUWqLPJDuv8xntsP6U3AC5KLTvsePRK3ec6Vv48dfuRbNMd2HdKh2x3ZqtERz_3gI3v70a9h2zw1H_s3Q4yK1A1WTnNvdSgCoBSa5qqqSyFQ-EdeOlA6VJ5JYisRPS5Im9RFlyWHh1yoTg_YGft7jLWHytKjZmH5Kiq7ILqVTIouMo5qH-AyHPQm0XZgi7WKUWamWUMcxu_DILZODJbR2YjwxTCbB2Zybp32vZmtjb2JYZkxsMckEMuRal0viZuWoLWQj4DRZNcoIUjHyK5xvg6_PHjG6vPdck</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>14132073</pqid></control><display><type>article</type><title>The World's Great Lakes</title><source>Elsevier ScienceDirect Journals Complete - AutoHoldings</source><creator>Beeton, Alfred M.</creator><creatorcontrib>Beeton, Alfred M.</creatorcontrib><description>Most of the large lakes lie in glacial scour basins in the northern hemisphere. These lakes are closely similar in physicochemical characteristics and in their biota. Most of the other large lakes are tectonic in origin and they differ greatly among themselves and from other lakes since they occur in a diversity of terrestrial environments under a broad range of climatic conditions. Large lakes have a great diversity of habitats resulting in great species diversity and endemism in ancient lakes. The pronounced horizontal gradients in physicochemical conditions in large lakes contribute to the diversity of habitats. Conditions found in Lakes Michigan and Skadar are examples.</description><identifier>ISSN: 0380-1330</identifier><identifier>DOI: 10.1016/S0380-1330(84)71817-X</identifier><language>eng</language><publisher>Elsevier B.V</publisher><subject>Freshwater ; geography ; lakes ; Limnology ; morphometry ; ponds ; water quality</subject><ispartof>Journal of Great Lakes research, 1984, Vol.10 (2), p.106-113</ispartof><rights>1984 International Association for Great Lakes Research</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a416t-9b2d5706800977eb6b594c14dc0d5c06796d64eea511d26eda158359d1c134633</citedby><cites>FETCH-LOGICAL-a416t-9b2d5706800977eb6b594c14dc0d5c06796d64eea511d26eda158359d1c134633</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://dx.doi.org/10.1016/S0380-1330(84)71817-X$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>314,778,782,3539,4012,27906,27907,27908,45978</link.rule.ids></links><search><creatorcontrib>Beeton, Alfred M.</creatorcontrib><title>The World's Great Lakes</title><title>Journal of Great Lakes research</title><description>Most of the large lakes lie in glacial scour basins in the northern hemisphere. These lakes are closely similar in physicochemical characteristics and in their biota. Most of the other large lakes are tectonic in origin and they differ greatly among themselves and from other lakes since they occur in a diversity of terrestrial environments under a broad range of climatic conditions. Large lakes have a great diversity of habitats resulting in great species diversity and endemism in ancient lakes. The pronounced horizontal gradients in physicochemical conditions in large lakes contribute to the diversity of habitats. Conditions found in Lakes Michigan and Skadar are examples.</description><subject>Freshwater</subject><subject>geography</subject><subject>lakes</subject><subject>Limnology</subject><subject>morphometry</subject><subject>ponds</subject><subject>water quality</subject><issn>0380-1330</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1984</creationdate><recordtype>article</recordtype><recordid>eNqNkDtLA0EUhadQMD5qKzGVj2L13p3XbiUSNAoBiySYbpjM3OjoJhtnNoL_3iQrtlpdOHznXPgYO0G4QkB1PQReQIacw0UhLjUWqLPJDuv8xntsP6U3AC5KLTvsePRK3ec6Vv48dfuRbNMd2HdKh2x3ZqtERz_3gI3v70a9h2zw1H_s3Q4yK1A1WTnNvdSgCoBSa5qqqSyFQ-EdeOlA6VJ5JYisRPS5Im9RFlyWHh1yoTg_YGft7jLWHytKjZmH5Kiq7ILqVTIouMo5qH-AyHPQm0XZgi7WKUWamWUMcxu_DILZODJbR2YjwxTCbB2Zybp32vZmtjb2JYZkxsMckEMuRal0viZuWoLWQj4DRZNcoIUjHyK5xvg6_PHjG6vPdck</recordid><startdate>1984</startdate><enddate>1984</enddate><creator>Beeton, Alfred M.</creator><general>Elsevier B.V</general><scope>FBQ</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7SN</scope><scope>7TV</scope><scope>C1K</scope><scope>F1W</scope><scope>H95</scope><scope>H96</scope><scope>L.G</scope></search><sort><creationdate>1984</creationdate><title>The World's Great Lakes</title><author>Beeton, Alfred M.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a416t-9b2d5706800977eb6b594c14dc0d5c06796d64eea511d26eda158359d1c134633</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1984</creationdate><topic>Freshwater</topic><topic>geography</topic><topic>lakes</topic><topic>Limnology</topic><topic>morphometry</topic><topic>ponds</topic><topic>water quality</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Beeton, Alfred M.</creatorcontrib><collection>AGRIS</collection><collection>CrossRef</collection><collection>Ecology Abstracts</collection><collection>Pollution Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 1: Biological Sciences & Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Journal of Great Lakes research</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Beeton, Alfred M.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The World's Great Lakes</atitle><jtitle>Journal of Great Lakes research</jtitle><date>1984</date><risdate>1984</risdate><volume>10</volume><issue>2</issue><spage>106</spage><epage>113</epage><pages>106-113</pages><issn>0380-1330</issn><abstract>Most of the large lakes lie in glacial scour basins in the northern hemisphere. These lakes are closely similar in physicochemical characteristics and in their biota. Most of the other large lakes are tectonic in origin and they differ greatly among themselves and from other lakes since they occur in a diversity of terrestrial environments under a broad range of climatic conditions. Large lakes have a great diversity of habitats resulting in great species diversity and endemism in ancient lakes. The pronounced horizontal gradients in physicochemical conditions in large lakes contribute to the diversity of habitats. Conditions found in Lakes Michigan and Skadar are examples.</abstract><pub>Elsevier B.V</pub><doi>10.1016/S0380-1330(84)71817-X</doi><tpages>8</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0380-1330 |
| ispartof | Journal of Great Lakes research, 1984, Vol.10 (2), p.106-113 |
| issn | 0380-1330 |
| language | eng |
| recordid | cdi_proquest_miscellaneous_14362306 |
| source | Elsevier ScienceDirect Journals Complete - AutoHoldings |
| subjects | Freshwater geography lakes Limnology morphometry ponds water quality |
| title | The World's Great Lakes |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-16T08%3A44%3A56IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=The%20World's%20Great%20Lakes&rft.jtitle=Journal%20of%20Great%20Lakes%20research&rft.au=Beeton,%20Alfred%20M.&rft.date=1984&rft.volume=10&rft.issue=2&rft.spage=106&rft.epage=113&rft.pages=106-113&rft.issn=0380-1330&rft_id=info:doi/10.1016/S0380-1330(84)71817-X&rft_dat=%3Cproquest_cross%3E14132073%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=14132073&rft_id=info:pmid/&rft_els_id=S038013308471817X&rfr_iscdi=true |