Not logged in
PANGAEA.
Data Publisher for Earth & Environmental Science

Bourlès, Didier L; Brown, E T; Raisbeck, Grant M; Yiou, Françoise; Gieskes, Joris M (1992): 10Be and 9Be concentrations and ratios of hydroxylamine leachable and residual phases of DSDP Site 64-477 (Table 1) [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.712137, Supplement to: Bourlès, DL et al. (1992): Beryllium isotope geochemistry of hydrothermally altered sediments. Earth and Planetary Science Letters, 109(1-2), 47-56, https://doi.org/10.1016/0012-821X(92)90073-5

Always quote citation above when using data! You can download the citation in several formats below.

Published: 1992 (exact date unknown)DOI registered: 2009-03-04

RIS CitationBibTeX Citation ShareShow MapGoogle Earth

Abstract:
Profiles of both10Be and9Be concentrations have been measured in sediments from the DSDP, Leg 64, Site 477 core. Established in the deep Guaymas Basin, in an area of high heat flow, this site offers the opportunity of studying hydrothermal alteration induced by two distinct hydrothermal systems, those caused (I) by the intrusion of hot sills into porous sediments and (I) by heat associated with a magma chamber.
The results show that the distribution of both beryllium isotopes between two operationally defined sedimentary phases (material susceptible to hydroxylamine leaching and residual material) changes with the degree of hydrothermal alteration. A decrease in10Be/9Be in the leachable phase of altered sediments relative to unaltered sediments indicates that hydrothermal alteration is not limited to a simple chemical leaching but involves redistribution of the beryllium isotopes between metamorphosed sedimentary phases. In addition, the similarity of the mean10Be/9Be ratios associated with the leachable and the residual phases in the part of the core which has experienced greenschist facies metamorphism suggests that this process leads in the prevailing geophysical conditions to isotopic homogenization.
A close relationship exists between10Be and MgO concentrations in altered sediments from this core. This supports earlier observations that beryllium is not easily removed from the sedimentary column and indicates that this remains the case even under the conditions encountered in submarine hydrothermal systems.
Project(s):
Coverage:
Latitude: 27.030033 * Longitude: -111.399433
Date/Time Start: 1978-12-18T00:00:00 * Date/Time End: 1978-12-18T00:00:00
Minimum DEPTH, sediment/rock: 21.5 m * Maximum DEPTH, sediment/rock: 240.0 m
Event(s):
64-477_Site * Latitude: 27.030033 * Longitude: -111.399433 * Date/Time: 1978-12-18T00:00:00 * Elevation: -2003.0 m * Penetration: 4.626 m * Recovery: 0.701 m * Location: North Pacific/Gulf of California/BASIN * Campaign: Leg64 * Basis: Glomar Challenger * Method/Device: Composite Core (COMPCORE) * Comment: 33 cores; 287.6 m cored; 28.5 m drilled; 24.4% recovery
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
DEPTH, sediment/rockDepth sedmGeocode
Sample commentSample commentBourlès, Didier L
Beryllium-99Be109 atoms/gBourlès, Didier LAtomic absorption spectrometry (AAS)Hydroxylamine leachable phase
Beryllium-99Be109 atoms/gBourlès, Didier LAtomic absorption spectrometry (AAS)Residual pahse
Beryllium-9, standard deviation9Be std dev±Bourlès, Didier LAtomic absorption spectrometry (AAS)Hydroxylamine leachable phase
Beryllium-9, standard deviation9Be std dev±Bourlès, Didier LAtomic absorption spectrometry (AAS)Residual pahse
Beryllium-1010Be109 atoms/gBourlès, Didier LAccelerator mass spectrometry (AMS)Hydroxylamine leachable phase
Beryllium-1010Be109 atoms/gBourlès, Didier LAccelerator mass spectrometry (AMS)Residual phase
Beryllium-10, standard deviation10Be std dev±Bourlès, Didier LAccelerator mass spectrometry (AMS)Hydroxylamine leachable phase
10 Beryllium-10, standard deviation10Be std dev±Bourlès, Didier LAccelerator mass spectrometry (AMS)Residual phase
11 Beryllium-10/Beryllium-910Be/9Be10-9 atoms/atomsBourlès, Didier LCalculatedHydroxylamine leachable phase
12 Beryllium-10/Beryllium-910Be/9Be10-9 atoms/atomsBourlès, Didier LCalculatedResidual phase
13 Beryllium-10/Beryllium-9 ratio, standard deviation10Be/9Be std dev±Bourlès, Didier LCalculatedHydroxylamine leachable phase
14 Beryllium-10/Beryllium-9 ratio, standard deviation10Be/9Be std dev±Bourlès, Didier LCalculatedResidual phase
15 Beryllium-99Be%Bourlès, Didier LResidual phase, % of the total 9Be
16 Beryllium-1010Be%Bourlès, Didier LResidual phase, % of the total 10Be
Size:
225 data points

Data

Download dataset as tab-delimited text — use the following character encoding:


Depth sed [m]

Sample comment

9Be [109 atoms/g]
(Hydroxylamine leachable phase...)

9Be [109 atoms/g]
(Residual pahse, Atomic absorp...)

9Be std dev [±]
(Hydroxylamine leachable phase...)

9Be std dev [±]
(Residual pahse, Atomic absorp...)

10Be [109 atoms/g]
(Hydroxylamine leachable phase...)

10Be [109 atoms/g]
(Residual phase, Accelerator m...)

10Be std dev [±]
(Hydroxylamine leachable phase...)
10 
10Be std dev [±]
(Residual phase, Accelerator m...)
11 
10Be/9Be [10-9 atoms/atoms]
(Hydroxylamine leachable phase...)
12 
10Be/9Be [10-9 atoms/atoms]
(Residual phase, Calculated)
13 
10Be/9Be std dev [±]
(Hydroxylamine leachable phase...)
14 
10Be/9Be std dev [±]
(Residual phase, Calculated)
15 
9Be [%]
(Residual phase, % of the tota...)
16 
10Be [%]
(Residual phase, % of the tota...)
21.5Unaltered sediment2860000065200000140000033000000.323000.107000.018000.0100011.3001.6400.8000.17069.524.9
32.5Contact metamorphism3160000082900000160000041000000.148000.067300.010000.003804.6800.8100.4000.06072.431.3
51.5Contact metamorphism2030000060700000100000030000000.098200.130000.005800.007004.8402.1400.3700.16074.956.9
52.0Contact metamorphism19900000101000000100000050000000.070300.125000.004400.007003.5301.2400.2800.09083.564.0
60.0Dolerite sill88000006360000040000032000000.000480.000470.000130.000130.0550.0080.0160.00287.950.3
106.0Contact metamorphism34500000118000000170000059000000.109000.204000.006000.012003.1601.7300.2300.13077.465.2
120.0Hydrothermal alteration2390000091900000120000046000000.040900.172000.002700.010001.7701.8700.1400.14079.480.8
126.0Hydrothermal alteration35100000104300000180000052000000.067100.199000.004100.018001.9101.9100.1500.20074.874.8
146.0Hydrothermal alteration1620000010690000080000053000000.020300.097800.001800.006101.2500.9100.1300.07086.882.8
155.0Greenschist facies1590000014870000080000074000000.036900.344000.002500.019002.3202.3100.2000.17090.390.3
173.0Greenschist facies950000014560000050000073000000.014400.312000.001300.018001.5202.1400.1600.16093.995.6
185.0Greenschist facies900000017440000050000087000000.016000.299000.001300.017001.7701.7100.1700.13095.194.9
212.0Greenschist facies550000012910000030000064000000.007910.103000.000810.006001.4500.8000.1600.06095.992.8
231.0Greenschist facies740000014820000040000074000000.008430.215000.000850.013001.1401.4500.1300.11095.296.2
240.0Greenschist facies490000014250000020000071000000.007290.233000.000800.014001.5001.6300.1800.13096.796.9