Frank, Tracy D; Thomas, Deborah J; Leckie, R Mark; Arthur, Michael A; Bown, Paul R; Jones, Kelly; Lees, Jackie A (2005): Stable carbon and oxygen isotope rates of Maastrichtian ODP samples from Shatsky Rise [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.837668, Supplement to: Frank, TD et al. (2005): The Maastrichtian record from Shatsky Rise (northwest Pacific): A tropical perspective on global ecological and oceanographic changes. Paleoceanography, 20(1), PA1008, https://doi.org/10.1029/2004PA001052
Always quote citation above when using data! You can download the citation in several formats below.
Abstract:
We present new isotopic and micropaleontological data from a depth transect on Shatsky Rise that record the response of the tropical Pacific to global biotic and oceanographic shifts during the mid-Maastrichtian. Results reveal a coupling between the upper ocean, characterized by a weak thermocline and low to intermediate productivity, and intermediate waters. During the earliest Maastrichtian, oxygen and neodymium isotope data suggest a significant contribution of relatively warm intermediate water from the North Pacific. Isotopic shifts through the early Maastrichtian suggest that this warmer water mass was gradually replaced by cooler waters originating in the Southern Ocean. Although the cooler water mass remained dominant through the remainder of the Maastrichtian, it was displaced intermittently at shallow intermediate depths by North Pacific intermediate water. The globally recognized "mid-Maastrichtian event" ~69 Ma, manifested by the brief appearance of abundant inoceramid bivalves over shallow portions of Shatsky Rise, is characterized by an abrupt increase (~2°-3°C) in sea surface temperatures, a greater flux of organic matter out of the surface ocean, and warmer (~4°C) intermediate waters. Results implicate simultaneous changes in surface waters and the sources/distribution patterns of intermediate water masses as an underlying cause for widespread biotic and oceanographic changes during mid-Maastrichtian time.
Other version:
Frank, Tracy D; Thomas, Deborah J; Leckie, R Mark; Arthur, Michael A; Bown, Paul R; Jones, Kelly; Lees, Jackie A (2007): Shatsky Rise Maastrichtian Isotope Data. NOAA National Centers for Environmental Information, https://doi.org/10.25921/K7Z5-B379
Project(s):
Ocean Drilling Program (ODP)
Coverage:
Median Latitude: 32.493840 * Median Longitude: 158.245759 * South-bound Latitude: 32.223600 * West-bound Longitude: 157.711660 * North-bound Latitude: 32.651660 * East-bound Longitude: 158.506080
Date/Time Start: 2001-09-18T08:00:00 * Date/Time End: 2001-10-01T23:30:00
Minimum DEPTH, sediment/rock: 111.80 m * Maximum DEPTH, sediment/rock: 302.40 m
Event(s):
198-1209A * Latitude: 32.651660 * Longitude: 158.505930 * Date/Time Start: 2001-09-18T08:00:00 * Date/Time End: 2001-09-19T13:35:00 * Elevation: -2387.2 m * Penetration: 259.6 m * Recovery: 262.27 m * Location: North Pacific Ocean * Campaign: Leg198 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 28 cores; 259.6 m cored; 0 m drilled; 101 % recovery
198-1209C * Latitude: 32.651650 * Longitude: 158.506080 * Date/Time Start: 2001-09-21T07:10:00 * Date/Time End: 2001-09-23T04:30:00 * Elevation: -2387.4 m * Penetration: 307.5 m * Recovery: 200.6 m * Location: North Pacific Ocean * Campaign: Leg198 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 23 cores; 202.2 m cored; 105.3 m drilled; 99.2 % recovery
198-1210 * Latitude: 32.223600 * Longitude: 158.259367 * Date/Time Start: 2001-09-23T00:00:00 * Date/Time End: 2001-09-27T00:00:00 * Elevation: -2573.4 m * Penetration: 619.4 m * Recovery: 625.7 m * Location: North Pacific Ocean * Campaign: Leg198 * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 69 cores; 606.9 m cored; 12.5 m drilled; 103.1% recovery
Parameter(s):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
1574 data points