N. J. Jenkins et al.: A comprehensive global oceanic dataset of helium isotope and tritium measurements
444
Table 3. Contributing analysts that are not authors on this paper.
+
» 10 16 20 zo 30 35
S°He (%) on 2500 m
40
Figure 8. A map of 5°He values at approximately 2500 m depth.
The values plotted are simply an average of all measurements within
a 1° square between 2250 and 2750 dbar. Depths shallower than
2500 m are masked in gray, and sampling locations are indicated by
jight gray dots.
5 10 15 20 za 30 35
S°He (%) on 4000 m
40
Figure 9. A map of $°He values at approximately 4000 m depth.
The values plotted are simply an average of all measurements within
a 1° square between 3750 and 4250 dbar. Depths shallower than
4000 m are masked in gray, and sampling locations are indicated by
light gray dots.
5 Contributors and pioneers
This dataset represents the hard work over many decades of
numerous individuals that are not included in the authorship
list of this paper. We list their names and affiliations at the
time of their contributions in Table 3. The list focuses on
those who made the measurements rather than those who
may have used the data. We apologize if there are others that
we may have missed in this list.
We also would like to recognize that the ability to make the
measurements presented in this dataset was a consequence
of the pioneering work of more than a few inventive and tal-
ented individuals. While space does not permit mentioning
chem all here, we felt it appropriate to highlight a pair of pio-
neering scientists who conducted landmark studies on ocean
tritium and ?He measurements.
www.earth-syst-sci-data.net/11/441/20 19
Arnold E. Bainbridge
Reinhold Bayer
Friedrich Begemann
Ulrich Beyerle
Wallace S. Broecker
Martin Butzin
William Brian Clarke
K. O. Dockins
H. Gorman Dorsey
Eric Eriksson
Elise Fourre
Bruno J. Giletti
Aristid von Grosse
". R. Harries
TI. Kaji
Sheldon Kaufman
J. Laurence Kulp
Willard F. Libby
Dempsey E. Lott III
Andrea Ludin
Liliane Merlivat
Robert Michel
Yasuo Miyake
Karl-Otto Munnich
Alfred O. Nier
Masami Nonaka
Hans Göte Östlund
Clare F. Postlethwaite
Paul D. Quay
Rachel S. H. R. Stanley
Sheila Stark
Reiner Steinfeldt
Hans E. Suess
Turgen Sültenfuss
Naoto Takahata
A. Tamuly
C. B. Taylor
Zafer Top
Tom Torgersen
Kim A. Van Scoy
Carolyn Walker
Wolfgang Weiss
Peter M Williams
UCSD, La Jolla, CA, USA
U. Heidelberg, Heidelberg, Germany
U. Chicago, Chicago, IL, USA
ETH, Zurich, Switzerland
LDEO, Pallisades, NY, USA
University of Bremen, Bremen, Germany
McMaster University, Hamilton, ON, Canada
UCSD, La Jolla, CA, USA
RSMAS, Miami, FL, USA
IMS, Stockholm, Sweden
CEA-Saclay, France
LDEO, Pallisades, NY, USA
RITU, Philadelphia, PA, USA
Australian AEC, Sutherland, NSW, Australia
Kyushu University, Fukuoka, Japan
U. Chicago, Chicago, IL, USA
LDEO, Pallisades, NY, USA
U. Chicago, Chicago, IL, USA
WHOI, Woods Hole, MA, USA
LDEO, Pallisades, NY, USA
Sorbonne University, Paris, France
UCSD, La Jolla, CA, USA
GRA, Tokyo, Japan
U. Heidelberg, Heidelberg, Germany
U. Minnesota, Minneapolis, MN, USA
IPRC & SOES, Tokyo, Japan
RSMAS, Miami, FL, USA
NOC-SOES, Southampton, UK
University of Washington, Seattle, WA, USA
WHOI, Woods Hole, MA, USA
NOC-SOES, Southampton, UK
IUP, University of Bremen, Germany
UCSD, La Jolla, CA, USA
{UP, University of Bremen, Germany
ORI, University of Tokyo, Tokyo, Japan
University of Quebec, Rimouski, PQ, Canada
INS, Lower Hutt, New Zealand
RSMAS, Miami, FL, USA
WHOI, Woods Hole, MA, USA
RSMAS, Miami, FL, USA
WHOI, Woods Hole, MA, USA
UV. Heidelberg, Heidelberg, Germany
TICSD. La Talla. CA. USA
5.1 W. Brian Clarke (1937-2002)
Although not the first to measure °He/*He in the environ-
ment (that was done by Aldrich and Nier, 1948), Clarke made
the first reported helium isotope measurements in seawater
(Clarke et al., 1969). He made his first measurements us-
ing a modified single stage magnetic sector, single collector
mass spectrometer to a precision of about 2 %. Clarke de-
veloped the first compact all-metal branch tube mass spec-
trometer specifically designed to make °He/*He measure-
ments ultimately to a precision of 0.1 % to 0.2 %. At the
time, conventional wisdom dictated that such measurements
(let alone precision measurements) were not possible with a
single stage magnetic sector instrument for such high (10°)
abundance ratios, but Clarke forged ahead anyway. He ini-
tially constructed two instruments in the early 1970s, using
Earth Syst. Sci. Data, 11, 441-454, 2019