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Farley, Kenneth A; Patterson, D B (1995): (Table 1) Helium concentration and flux in DSDP Hole 94-607 samples [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.769857, Supplement to: Farley, KA; Patterson, DB (1995): A 100-kyr periodicity in the flux of extraterrestrial 3He to the sea floor. Nature, 378(6557), 521-644, https://doi.org/10.1038/378600a0

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Abstract:
Most of the helium-3 in oceanic sediments conies from interplanetary dust particles (IDPs), and can therefore be used to infer the accretion rate of dust to the Earth through time (Ozima et al., 1984, doi:10.1038/311448a0; Takayanagi and Ozima, 1987, doi:10.1029/JB092iB12p12531; Farley, 1995, doi:10.1038/376153a0). 3He records from slowly accumulating pelagic clays indicate that the accretion rate varies considerably over millions of years, probably owing to cometary and asteroidal break-up events3. Muller and MacDonald have proposed (Muller and MacDonald, 1995, doi:10.1038/377107b0) that periodic changes in this accretion rate due to a previously unrecognized 100-kyr periodicity in the Earth's orbital inclination might account for the prominence of this frequency in climate records of the past million years (Imbrie et al., 1993, doi:10.1029/93PA02751). Here we report variations in the 3He flux to the sea floor that support this idea. We find that the flux recorded in rapidly accumulating Quaternary sediments from the Mid-Atlantic Ridge oscillates with a period of about 100 kyr. We cannot yet say, however, whether the 100-kyr climate cycle is a consequence of, a cause of, or an effect independent of these periodic changes in the rate of delivery of interplanetary dust to the sea floor.
Project(s):
Coverage:
Latitude: 41.001200 * Longitude: -32.957300
Date/Time Start: 1983-07-06T00:00:00 * Date/Time End: 1983-07-06T00:00:00
Minimum Elevation: -3427.0 m * Maximum Elevation: -3427.0 m
Event(s):
94-607 * Latitude: 41.001200 * Longitude: -32.957300 * Date/Time: 1983-07-06T00:00:00 * Elevation: -3427.0 m * Penetration: 284.4 m * Recovery: 248.6 m * Location: North Atlantic/FLANK * Campaign: Leg94 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 30 cores; 284.4 m cored; 0 m drilled; 87.4 % recovery
Comment:
Core disruption between cores 94-607-2 and 94-607-3 precludes accurate determination of sedimentation rates in this interval; the mean value of the other 10 cycles has been adopted for this cycle.
Size:
148 data points

Data

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Age [ka BP]

Age min [ka]

Age max [ka]

Sample label

Sample label 2

N cyc

N [#]

3He [10-10 cm3/g]

3He std dev [±]
10 
3He/4He [10-4]
11 
3He/4He std dev [±]
12 
3He ET [%]
13 
3He flux [10-12 cm3/cm2/ka]
14 
3He flux std dev [±]
15 
MAR [g/cm2/ka]
260.525326894-607-2-1,0-91010.004240.000100.000910.00005781.340.054.05
280.026829294-607-2-1,88-15094-607-2-2,0-8140.002080.000140.001730.00013870.490.042.76
303.029231494-607-2-2,8-106270.003060.000280.001610.00015871.080.114.06
325.031433694-607-2-2,106-15094-607-2-3,0-53340.004430.000090.002040.00004891.740.044.31
345.033635494-607-2-3,53-150440.004400.000140.001270.00005851.570.074.70
363.535437394-607-2-4,0-78540.003460.000140.001570.00006861.180.053.62
381.037338994-607-2-4,78-121650.002110.000230.001950.00018890.510.062.72
399.038940994-6072-4,121-15094-607-2-5,0-69740.002230.000180.002810.00018921.020.084.85
418.540942894-607-2-5,69-15094-607-2-6,0-8880.002680.000220.000890.00001750.940.104.66
436.542844594-607-2-6,8-91940.003740.000100.001240.00005821.020.033.31
451.544545894-607-2-6,91-15094-607-2-7,0-261060.002730.000230.001040.00007800.880.094.01