Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Andrea M. Stancin"'
Autor:
Steven D'Hondt, Lewis J. Abrams, Robert A. Pockalny, Jan Fischer, H. N. Schrum, Dennis Graham, Jens Kallmeyer, David C. Smith, Arthur J. Spivack, Timothy G. Ferdelman, Franciszek Hasiuk, Andrea M. Stancin
Publikováno v:
Proceedings of the National Academy of Sciences of the United States of America (PNAS)
The low-productivity South Pacific Gyre (SPG) is Earth's largest oceanic province. Its sediment accumulates extraordinarily slowly (0.1–1 m per million years). This sediment contains a living community that is characterized by very low biomass and
Autor:
Robert M. Owen, Chris M. Hall, Andrea M. Stancin, James D. Gleason, Joel D. Blum, David K. Rea, Theodore C. Moore, Steven A Hovan
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 261:218-233
A 14-meter long pelagic clay core recovered at Marlin Rise (40°00.531′S, 154°2.601′W; 4775 m water depth) in the Southwest Pacific Basin contains a record of eolian dust deposited since the early Miocene. Downcore analysis of detrital minerals
Autor:
Joel D. Blum, David K. Rea, Steven A Hovan, Andrea M. Stancin, Robert M. Owen, Theodore C. Moore, James D. Gleason
Publikováno v:
Earth and Planetary Science Letters. 248:840-850
Pelagic clay of the east-central Pacific province is shown to be a mixture of three primary detrital components, reflecting continental source areas in Asia, North America, and Central and South America. Relative contributions from each source area a
Publikováno v:
Paleoceanography. 23
Publikováno v:
Paleoceanography. 23
A large diameter piston core containing 8.35 m of metalliferous sediment has been recovered from a small abyssal valley in the remote Southwest Pacific Basin (31° 42.194′S, 143° 30° 331′W; 5082 m water depth), providing unique insight into hyd
Autor:
Ingrid L. Hendy, Deborah J Thomas, Christopher F. Paul, Mitchell W Lyle, James D. Gleason, Steven A Hovan, Jennifer C. Latimer, Lee M. Liberty, Andrea M. Stancin, Matthew P. Bolyn, Brandi M. Murphy, Robert M. Owen, David K. Rea, Thomas H.C. Rea
Publikováno v:
Geology. 34:873
A broad region, nearly the size of the Mediterranean Sea, exists in the central South Pacific Ocean that is devoid of sediment and has been so since the Late Cretaceous. The requirements for remaining sediment free are very low biological productivit