Opal Phytoliths in a North Atlantic Dust Fall

Minute bodies (less than 80 microns) of isotropic silica, originally precipitated by terrestrial plants, are found together with freshwater diatoms in falls of dust over the ocean. Eolian transport from Africa can explain the occurrence of similar plant remains in deep-sea sediments of the equatoria...

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Published in:Science
Main Authors: Folger, D. W., Burckle, L. H., Heezen, B. C.
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 1967
Subjects:
Online Access:http://dx.doi.org/10.1126/science.155.3767.1243
https://www.science.org/doi/pdf/10.1126/science.155.3767.1243
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spelling craaas:10.1126/science.155.3767.1243 2024-06-09T07:48:04+00:00 Opal Phytoliths in a North Atlantic Dust Fall Folger, D. W. Burckle, L. H. Heezen, B. C. 1967 http://dx.doi.org/10.1126/science.155.3767.1243 https://www.science.org/doi/pdf/10.1126/science.155.3767.1243 en eng American Association for the Advancement of Science (AAAS) Science volume 155, issue 3767, page 1243-1244 ISSN 0036-8075 1095-9203 journal-article 1967 craaas https://doi.org/10.1126/science.155.3767.1243 2024-05-16T12:54:30Z Minute bodies (less than 80 microns) of isotropic silica, originally precipitated by terrestrial plants, are found together with freshwater diatoms in falls of dust over the ocean. Eolian transport from Africa can explain the occurrence of similar plant remains in deep-sea sediments of the equatorial Atlantic as far west as the Mid-Atlantic Ridge. Article in Journal/Newspaper North Atlantic AAAS Resource Center (American Association for the Advancement of Science) Mid-Atlantic Ridge Science 155 3767 1243 1244
institution Open Polar
collection AAAS Resource Center (American Association for the Advancement of Science)
op_collection_id craaas
language English
description Minute bodies (less than 80 microns) of isotropic silica, originally precipitated by terrestrial plants, are found together with freshwater diatoms in falls of dust over the ocean. Eolian transport from Africa can explain the occurrence of similar plant remains in deep-sea sediments of the equatorial Atlantic as far west as the Mid-Atlantic Ridge.
format Article in Journal/Newspaper
author Folger, D. W.
Burckle, L. H.
Heezen, B. C.
spellingShingle Folger, D. W.
Burckle, L. H.
Heezen, B. C.
Opal Phytoliths in a North Atlantic Dust Fall
author_facet Folger, D. W.
Burckle, L. H.
Heezen, B. C.
author_sort Folger, D. W.
title Opal Phytoliths in a North Atlantic Dust Fall
title_short Opal Phytoliths in a North Atlantic Dust Fall
title_full Opal Phytoliths in a North Atlantic Dust Fall
title_fullStr Opal Phytoliths in a North Atlantic Dust Fall
title_full_unstemmed Opal Phytoliths in a North Atlantic Dust Fall
title_sort opal phytoliths in a north atlantic dust fall
publisher American Association for the Advancement of Science (AAAS)
publishDate 1967
url http://dx.doi.org/10.1126/science.155.3767.1243
https://www.science.org/doi/pdf/10.1126/science.155.3767.1243
geographic Mid-Atlantic Ridge
geographic_facet Mid-Atlantic Ridge
genre North Atlantic
genre_facet North Atlantic
op_source Science
volume 155, issue 3767, page 1243-1244
ISSN 0036-8075 1095-9203
op_doi https://doi.org/10.1126/science.155.3767.1243
container_title Science
container_volume 155
container_issue 3767
container_start_page 1243
op_container_end_page 1244
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