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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American Association for the Advancement of Science (AAAS)
1967
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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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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 |
_version_ |
1801379618992685056 |