Long-term variability of temperature and (super 14) C in the Gulf Stream; oceanographic implications.
Variability in temperature and 14C levels are recorded in coralline aragonite that grew in the Gulf Stream during the past four centuries. In particular, 180/160 ratios reflect a decrease of ca 1°C in surface water temperature during the latter part of the Little Ice age. 14C levels also rose in the...
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eScholarship, University of California
1983
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| Online Access: | http://www.escholarship.org/uc/item/7366q8s4 |
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ftcdlib:qt7366q8s4 2023-05-15T17:29:10+02:00 Long-term variability of temperature and (super 14) C in the Gulf Stream; oceanographic implications. Druffel, Ellen R M 1983-01-01 application/pdf http://www.escholarship.org/uc/item/7366q8s4 english eng eScholarship, University of California qt7366q8s4 http://www.escholarship.org/uc/item/7366q8s4 Attribution (CC BY): http://creativecommons.org/licenses/by/3.0/ CC-BY Druffel, Ellen R M. (1983). Long-term variability of temperature and (super 14) C in the Gulf Stream; oceanographic implications. Radiocarbon, 25(2). UC Irvine: Department of Earth System Science, UCI. Retrieved from: http://www.escholarship.org/uc/item/7366q8s4 Physical Sciences and Mathematics currents Gulf Stream Montastrea Montastrea annularis Straits of Florida paleo oceanography Scleractinia Zoantharia X ray data O 18 O 16 temperature ocean circulation solar activity Anthozoa Coelenterata Atlantic Ocean North Atlantic sea water oxygen atmosphere C 14 carbon isotopes radioactive isotopes Invertebrata carbon dioxide stable isotopes geochemistry carbonates aragonite article 1983 ftcdlib 2016-04-02T18:18:37Z Variability in temperature and 14C levels are recorded in coralline aragonite that grew in the Gulf Stream during the past four centuries. In particular, 180/160 ratios reflect a decrease of ca 1°C in surface water temperature during the latter part of the Little Ice age. 14C levels also rose in the surface waters of the Gulf Stream and in atmospheric CO2 during the Maunder minimum. These observations indicate that ocean circulation may have been significantly different in the North Atlantic around the beginning of the 18th century. Article in Journal/Newspaper North Atlantic University of California: eScholarship |
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Open Polar |
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University of California: eScholarship |
| op_collection_id |
ftcdlib |
| language |
English |
| topic |
Physical Sciences and Mathematics currents Gulf Stream Montastrea Montastrea annularis Straits of Florida paleo oceanography Scleractinia Zoantharia X ray data O 18 O 16 temperature ocean circulation solar activity Anthozoa Coelenterata Atlantic Ocean North Atlantic sea water oxygen atmosphere C 14 carbon isotopes radioactive isotopes Invertebrata carbon dioxide stable isotopes geochemistry carbonates aragonite |
| spellingShingle |
Physical Sciences and Mathematics currents Gulf Stream Montastrea Montastrea annularis Straits of Florida paleo oceanography Scleractinia Zoantharia X ray data O 18 O 16 temperature ocean circulation solar activity Anthozoa Coelenterata Atlantic Ocean North Atlantic sea water oxygen atmosphere C 14 carbon isotopes radioactive isotopes Invertebrata carbon dioxide stable isotopes geochemistry carbonates aragonite Druffel, Ellen R M Long-term variability of temperature and (super 14) C in the Gulf Stream; oceanographic implications. |
| topic_facet |
Physical Sciences and Mathematics currents Gulf Stream Montastrea Montastrea annularis Straits of Florida paleo oceanography Scleractinia Zoantharia X ray data O 18 O 16 temperature ocean circulation solar activity Anthozoa Coelenterata Atlantic Ocean North Atlantic sea water oxygen atmosphere C 14 carbon isotopes radioactive isotopes Invertebrata carbon dioxide stable isotopes geochemistry carbonates aragonite |
| description |
Variability in temperature and 14C levels are recorded in coralline aragonite that grew in the Gulf Stream during the past four centuries. In particular, 180/160 ratios reflect a decrease of ca 1°C in surface water temperature during the latter part of the Little Ice age. 14C levels also rose in the surface waters of the Gulf Stream and in atmospheric CO2 during the Maunder minimum. These observations indicate that ocean circulation may have been significantly different in the North Atlantic around the beginning of the 18th century. |
| format |
Article in Journal/Newspaper |
| author |
Druffel, Ellen R M |
| author_facet |
Druffel, Ellen R M |
| author_sort |
Druffel, Ellen R M |
| title |
Long-term variability of temperature and (super 14) C in the Gulf Stream; oceanographic implications. |
| title_short |
Long-term variability of temperature and (super 14) C in the Gulf Stream; oceanographic implications. |
| title_full |
Long-term variability of temperature and (super 14) C in the Gulf Stream; oceanographic implications. |
| title_fullStr |
Long-term variability of temperature and (super 14) C in the Gulf Stream; oceanographic implications. |
| title_full_unstemmed |
Long-term variability of temperature and (super 14) C in the Gulf Stream; oceanographic implications. |
| title_sort |
long-term variability of temperature and (super 14) c in the gulf stream; oceanographic implications. |
| publisher |
eScholarship, University of California |
| publishDate |
1983 |
| url |
http://www.escholarship.org/uc/item/7366q8s4 |
| genre |
North Atlantic |
| genre_facet |
North Atlantic |
| op_source |
Druffel, Ellen R M. (1983). Long-term variability of temperature and (super 14) C in the Gulf Stream; oceanographic implications. Radiocarbon, 25(2). UC Irvine: Department of Earth System Science, UCI. Retrieved from: http://www.escholarship.org/uc/item/7366q8s4 |
| op_relation |
qt7366q8s4 http://www.escholarship.org/uc/item/7366q8s4 |
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Attribution (CC BY): http://creativecommons.org/licenses/by/3.0/ |
| op_rightsnorm |
CC-BY |
| _version_ |
1766122790982778880 |