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| 02037cam 2200373zi 4500 |
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| 001 | 9.874934 |
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| 003 | CaOODSP |
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| 005 | 20221107164328 |
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| 006 | m o d f |
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| 007 | cr |n||||||||| |
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| 008 | 190614e197703##onca |ot f00| 0 eng d |
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| 040 | |aCaOODSP|beng|erda|cCaOODSP |
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| 043 | |an-cn--- |
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| 086 | 1 |aEn13-7/77-2E-PDF |
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| 100 | 1 |aMacInnis, G. A., |eauthor. |
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| 245 | 12|aA method for fossil pollen extraction from sand-rich sediments / |cauthors: G.A. MacInnis and N.A. Rukavina. |
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| 264 | 1|a[Burlington, Ont.] : |bHydraulics Research Division, [National Water Research Institute], |cMarch 1977. |
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| 300 | |a1 online resource (8 pages, 3 unnumbered pages) : |billustrations. |
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| 336 | |atext|btxt|2rdacontent |
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| 337 | |acomputer|bc|2rdamedia |
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| 338 | |aonline resource|bcr|2rdacarrier |
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| 490 | 1 |aTechnical note ; |vno. 77-2 |
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| 500 | |aDigitized edition from print [produced by Environment and Climate Change Canada]. |
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| 500 | |aTitle from cover. |
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| 504 | |aIncludes bibliographical references. |
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| 520 | |a"Fossil pollen concentration is relatively low in cores of sand-rich nearshore lacustrine sediment because pollen is hydraulically equivalent to, and tends to be associated with, the silt-clay component of the sediment. Concentration can be increased to levels suitable for pollen dating by removing the sand fraction by decantation and then applying the standard Quaternary pollen-preparation procedure (Faegri and Iversen, 1964) to the silt-clay residue"--Introduction, page 1. |
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| 653 | 0|aFossil pollen |
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| 692 | 07|2gccst|aExtraction |
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| 700 | 1 |aRukavina, N. A., |eauthor. |
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| 710 | 1 |aCanada. |bEnvironment Canada. |
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| 710 | 2 |aNational Water Research Institute (Canada). |bHydraulics Research Division. |
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| 830 | #0|aTechnical note (National Water Research Institute (Canada). Hydraulics Research Division)|vno. 77-2.|w(CaOODSP)9.865405 |
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| 856 | 40|qPDF|s676 KB|uhttps://publications.gc.ca/collections/collection_2019/eccc/En13-7-77-2-eng.pdf |
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