Some of the material in is restricted to members of the community. By logging in, you may be able to gain additional access to certain collections or items. If you have questions about access or logging in, please use the form on the Contact Page.
Some of the material in is restricted to members of the community. By logging in, you may be able to gain additional access to certain collections or items. If you have questions about access or logging in, please use the form on the Contact Page.
During IODP Leg 317 off the east coast of New Zealand, three continental shelf sites (U1351, U1353 and U1354) and one continental slope site were cored. Sedimentary sequences representing shallow water depositional cycles were recovered...
The Citronelle Formation is the most widely occurring, surficial geologic unit along the northeast Gulf of Mexico. It is a siliciclastic unit consisting primarily of sands and gravels with varying amounts of clay and minor amounts of...
The objective of this study is to study spatial and temporal paleontological distributions as they relate to the histories of Ninetyeast Ridge and Broken Ridge from ODP Leg 121. This study is important for establishing connections...
A greatly expanded section of Holocene sediment was recovered at Site NBP0602-8 in the Firth of Tay near the tip of the West Antarctic Peninsula during the SHALDRIL II cruise aboard the R/V Nathaniel B. Palmer, 2006. Recovery in the four...
International Ocean Discovery Program (IODP) Expedition 355 drilled two sites (U1456 and U1457) in Laxmi Basin, located in the eastern Arabian Sea. The primary objective of Expedition 355 is to better understand the impact that the...
Investigation and Interpretation of Variations in NE Gulf of Mexico Nannoplankton Assemblages Following the Macando Well Blowout: Months of August-November
The biodiversity and biomass of coccolithophore species observed in the NE Gulf of Mexico during the months of August through November from 2011 to 2013 are quite dynamic. Following the Macondo well blow out in 2010, analyses have been...
Calcareous nannofossils and stable isotopes were analyzed to determine the timing and causes of extensive Miocene debris flows and Oligocene slumps recovered by Ocean Drilling Program (ODP), cruise Leg 207 to Demerara Rise along French...
The Brazos River area is located at the entrance of the former Western Interior Seaway on the shallow northern Gulf of Mexico shelf. Marine sediments in the region were deposited in a middle to outer shelf environment. Outcrops on the...
ABSTRACT The Ocean Drilling Program (ODP) Leg 154 in the western equatorial Atlantic cored Paleocene - Holocene strata at Site 929 on the Ceara Rise. The calcareous nannofossil biostratigraphy of the Oligocene - lower Miocene sequence at...
There are no published quantitative studies of coccolithophore standing crops in the North East Gulf of Mexico (NE GOM). When the Macondo oil spill happened in April of 2010 researchers scrambled to determine what effect it would have on...
Pliocene-Pleistocene Calcareous Nannofossil Biostratigraphy of IODP Hole 1396C Adjacent to Montserrat Island in the Lesser Antilles, Caribbean Sea, Plus Experimentally Induced Diagenesis
Integrated Ocean Drilling Program Hole 1396C, adjacent to Montserrat Island, provides a lower Pliocene to Pleistocene record of calcareous nannofossil assemblages (CN11 to CN15). The nannofossil assemblages are generally common to...
IODP Expedition 334 drilled west of the Costa Rican coast just offshore of the Osa Peninsula with Hole U1381A being the focus for this study. The preservation of the calcareous nannofossils at this hole ranges from moderate to good, ...
High-resolution Holocene sediment cores from the continental shelf of Antarctica are integral to the study of recent climate transitions, but such records are rare. The inaugural SHALDRIL I cruise to Maxwell Bay along the Northern...
Some of the material in is restricted to members of the community. By logging in, you may be able to gain additional access to certain collections or items. If you have questions about access or logging in, please use the form on the Contact Page.
