study several coastal oceanic regimes. The work of
Fairbanks (1982) is one of the earliest of these efforts.
See also
Cenozoic Climate – Oxygen Isotope Evidence.
River Inputs.
Further Reading
Craig H and Gordon LI (1965) Deuterium and oxygen-18
variations in the ocean and marine atmosphere. Stable
Isotopes in Oceanographic Studies and Paleotemperatures, Consiglio Nazionale Delle Ricerche, Laboratorio
di Geologia Nucleare-Pisa, 122 pp. (Also in Symposium
on Marine Chemistry, Publ. 3., Kingston, Graduate
School of Oceanography, University of Rhode Island,
277--374).
Fairbanks RG (1982) The origin of continental shelf and
slope water in the New York Bight and Gulf of Maine:
evidence from H 2
18 O/H 2
16
O ratio measurements. Journal
of Geophysical Research 87: 5796--5808.
GEOSECS Atlantic, Pacific, and Indian Ocean Expeditions,
Volume 7, Shorebased Data and Graphics (1987)
National Science Foundation. 200pp.
OXYGEN ISOTOPES IN THE OCEAN 565
Fairbanks (1982) is one of the earliest of these efforts.
See also
Cenozoic Climate – Oxygen Isotope Evidence.
River Inputs.
Further Reading
Craig H and Gordon LI (1965) Deuterium and oxygen-18
variations in the ocean and marine atmosphere. Stable
Isotopes in Oceanographic Studies and Paleotemperatures, Consiglio Nazionale Delle Ricerche, Laboratorio
di Geologia Nucleare-Pisa, 122 pp. (Also in Symposium
on Marine Chemistry, Publ. 3., Kingston, Graduate
School of Oceanography, University of Rhode Island,
277--374).
Fairbanks RG (1982) The origin of continental shelf and
slope water in the New York Bight and Gulf of Maine:
evidence from H 2
18 O/H 2
16
O ratio measurements. Journal
of Geophysical Research 87: 5796--5808.
GEOSECS Atlantic, Pacific, and Indian Ocean Expeditions,
Volume 7, Shorebased Data and Graphics (1987)
National Science Foundation. 200pp.
OXYGEN ISOTOPES IN THE OCEAN 565