Winckler, Gisela; Anderson, Robert F; Stute, Martin; Schlosser, Peter (2004): Helium isotope record, CaCO3 concentration and accumulation rate of ODP Site 138-849 (Table 2) [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.742954, Supplement to: Winckler, G et al. (2004): Does interplanetary dust control 100 kyr glacial cycles? Quaternary Science Reviews, 23(18-19), 1873-1878, https://doi.org/10.1016/j.quascirev.2004.05.007
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Published: 2004 (exact date unknown) • DOI registered: 2010-08-06
Abstract:
The cause of the 100 kyr glacial–interglacial cycles during the past 800 kyr is one of the fundamental puzzles in paleoclimatology. The widely accepted Milankovitch theory, relating earth's climate cycles to variations in insolation caused by periodic changes in orbital parameters, has difficulties to explain the predominant 100 kyr rhythm. Although earth's eccentricity varies with a period of 100 kyr, the resulting change in insolation is too small to produce the corresponding climate cycle by direct forcing (Imbrie et al., 1993; doi:10.1029/93PA02751. In order to solve the '100 kyr problem', Muller and MacDonald (1995, doi:10.1038/377107b0; 1997, doi:10.1126/science.277.5323.215; Proc. Nat. Acad. Sci. USA 94 (1997b) 8329) proposed an alternative orbital but non-Milankovitch mechanism attributing the glacial cycles to regular variations in the accretion of interplanetary dust particles (IDP) caused by 100 kyr cycles in the orbital inclination of the earth. To test this controversial hypothesis, we study the IDP accumulation in deep-sea sediments from a period in the early Pleistocene. We find apparent 41 kyr cycles but no 100 kyr periodicity in the IDP accumulation rate. As there is no known mechanism to produce 41 kyr cycles in IDP supply from space, we conclude that the 41 kyr cycles are caused by the dynamics of sediment accumulation, and that changes in the IDP flux do not drive the Pleistocene glacial cycles.
Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: 0.183330 * Longitude: -110.518330
Date/Time Start: 1991-06-12T00:00:00 * Date/Time End: 1991-09-07T00:00:00
Minimum DEPTH, sediment/rock: 38.98 m * Maximum DEPTH, sediment/rock: 44.62 m
Event(s):
138-849 * Latitude: 0.183330 * Longitude: -110.518330 * Date/Time Start: 1991-09-07T00:00:00 * Date/Time End: 1991-06-12T00:00:00 * Elevation: -3839.0 m * Penetration: 791.4 m * Recovery: 777.62 m * Location: North Pacific Ocean * Campaign: Leg138 * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 83 cores; 786.4 m cored; 0 m drilled; 98.9 % recovery
Comment:
Age after Mix et al., (1995). Sediment depth is revised composite depth (rmcd). For stable oxygen isotope record see Mix et al. (1995) dataset: doi:10.1594/PANGAEA.60255
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Sample code/label | Sample label | Winckler, Gisela | DSDP/ODP/IODP sample designation | ||
| 2 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 3 | AGE | Age | ka BP | Geocode | ||
| 4 | Helium-3 | 3He | 10-10 cm3/g | Winckler, Gisela | Mass spectrometer MAP215-50 | |
| 5 | Helium-3, standard deviation | 3He std dev | ± | Winckler, Gisela | Mass spectrometer MAP215-50 | |
| 6 | Helium-3/Helium-4 ratio | 3He/4He | 10-4 | Winckler, Gisela | ||
| 7 | Helium-3/Helium-4 ratio, standard deviation | 3He/4He std dev | ± | Winckler, Gisela | ||
| 8 | Calcium carbonate | CaCO3 | % | Winckler, Gisela | Coulometry | |
| 9 | Accumulation rate, mass | MAR | g/cm2/ka | Winckler, Gisela | Calculated | |
| 10 | Comment | Comment | Winckler, Gisela |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
333 data points