Paleontologic Technique for Defining Ancient Ocean Currents
Subtraction from the new data, of a quadratic surface fitted to the taxonomic diversity data of recent planktonic foraminifera yields a residual surface closely related to ocean current systems. This technique could be applied to fossil materials to develop knowledge of ocean circulation patterns du...
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| Veröffentlicht in: | Science (American Association for the Advancement of Science) 1965-05, Vol.148 (3672), p.943-946 |
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| container_end_page | 946 |
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| container_issue | 3672 |
| container_start_page | 943 |
| container_title | Science (American Association for the Advancement of Science) |
| container_volume | 148 |
| creator | Stehli, F. G. |
| description | Subtraction from the new data, of a quadratic surface fitted to the taxonomic diversity data of recent planktonic foraminifera yields a residual surface closely related to ocean current systems. This technique could be applied to fossil materials to develop knowledge of ocean circulation patterns during glacial and interglacial climatic episodes. |
| doi_str_mv | 10.1126/science.148.3672.943.b |
| format | Article |
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| fulltext | fulltext |
| identifier | ISSN: 0036-8075 |
| ispartof | Science (American Association for the Advancement of Science), 1965-05, Vol.148 (3672), p.943-946 |
| issn | 0036-8075 1095-9203 |
| language | eng |
| recordid | cdi_proquest_miscellaneous_733164096 |
| source | American Association for the Advancement of Science; JSTOR |
| subjects | Chondrites Feldspars Mars Mathematical surfaces Meteorites Ocean currents Oceans Olivine Plagioclase Planetary temperature |
| title | Paleontologic Technique for Defining Ancient Ocean Currents |
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