POST-PLEISTOCENE DIATOM SUCCESSION IN DOUGLAS LAKE, MICHIGAN 1 , 2
dc.contributor.author | Stoermer, Eugene F. | en_US |
dc.date.accessioned | 2010-04-01T15:13:16Z | |
dc.date.available | 2010-04-01T15:13:16Z | |
dc.date.issued | 1977-03 | en_US |
dc.identifier.citation | Stoermer, E. F . (1977). "POST-PLEISTOCENE DIATOM SUCCESSION IN DOUGLAS LAKE, MICHIGAN 1 , 2 ." Journal of Phycology 13(1): 73-80. <http://hdl.handle.net/2027.42/65690> | en_US |
dc.identifier.issn | 0022-3646 | en_US |
dc.identifier.issn | 1529-8817 | en_US |
dc.identifier.uri | https://hdl.handle.net/2027.42/65690 | |
dc.description.abstract | Analysis of fossil diatom assemblages recovered from a 12.2 m core reveals a series of distinct floristic associations. The associations present are correlated with sediment type and reflect successive stages in the development of the lake. A basal red clay sediment contains a planktonic association characteristic of large, proglacial lakes. At 10.0 m core depth, sediment type changes to fine sand containing a higher abundance of benthic species indicating reduction of water depth at the deposition site. Marl sediments begin at 9.7 m and contain an association characteristic of a small, shallow, oligotrophic lake. At 8.8 m the marl sequence is interrupted by highly organic sediment containing a eutrophic plankton association. From 8.5 to 7.6 m the sediment type grades from marl to organic, apparently reduced sediments and diatom associations present contain successively higher percentages of planktonic species associated with eutrophic habitats. By the 7.6 m level a eutrophic plankton association, similar to the modern flora, is established and remains remarkably constant to the surface of the section. | en_US |
dc.format.extent | 1385189 bytes | |
dc.format.extent | 3110 bytes | |
dc.format.mimetype | application/octet-stream | |
dc.format.mimetype | text/plain | |
dc.publisher | Blackwell Science Inc | en_US |
dc.rights | 1977, by the Phycological Society of America, Inc. | en_US |
dc.subject.other | Diatoms | en_US |
dc.subject.other | Douglas Lake | en_US |
dc.subject.other | Eutrophication | en_US |
dc.subject.other | Holocene | en_US |
dc.subject.other | Species Succession | en_US |
dc.title | POST-PLEISTOCENE DIATOM SUCCESSION IN DOUGLAS LAKE, MICHIGAN 1 , 2 | en_US |
dc.type | Article | en_US |
dc.rights.robots | IndexNoFollow | en_US |
dc.subject.hlbsecondlevel | Natural Resources and Environment | en_US |
dc.subject.hlbtoplevel | Science | en_US |
dc.description.peerreviewed | Peer Reviewed | en_US |
dc.contributor.affiliationum | Great Lakes Research Division, The University of Michigan Ann Arbor, Michigan 48109 | en_US |
dc.description.bitstreamurl | http://deepblue.lib.umich.edu/bitstream/2027.42/65690/1/j.1529-8817.1977.tb02890.x.pdf | |
dc.identifier.doi | 10.1111/j.1529-8817.1977.tb02890.x | en_US |
dc.identifier.source | Journal of Phycology | en_US |
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dc.owningcollname | Interdisciplinary and Peer-Reviewed |
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