Revisiting five decades of 234 Th data: a comprehensive global oceanic compilation
We present here a global oceanic compilation of 234Th measurements that collects results from researchers and laboratories over a period exceeding 50 years. The origin of the 234Th sampling in the ocean goes back to 1967, when Bhat et al. (1969) initially studied 234Th distribution relative to its p...
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Published in | Earth system science data Vol. 14; no. 6; pp. 2639 - 2679 |
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Main Authors | , , |
Format | Journal Article |
Language | English |
Published |
09.06.2022
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Online Access | Get full text |
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Summary: | We present here a global oceanic compilation of 234Th
measurements that collects results from researchers and laboratories over a
period exceeding 50 years. The origin of the 234Th sampling in the
ocean goes back to 1967, when Bhat et al. (1969) initially studied 234Th distribution relative to its parent
238U in the Indian Ocean. However, it was the seminal work of
Buesseler et al. (1992) – which
proposed an empirical method to estimate export fluxes from 234Th
distributions – that drove the extensive use of the 234Th–238U
radioactive pair to evaluate the organic carbon export out of the surface
ocean by means of the biological carbon pump. Since then, a large number of
234Th depth profiles have been collected using a variety of sampling
instruments and strategies that have changed during the past 50 years. The
present compilation is made of a total 223 data sets: 214 from studies
published in either articles in refereed journals, PhD theses, or
repositories, as well as 9 unpublished data sets. The data were compiled from over
5000 locations spanning all the oceans for total 234Th profiles,
dissolved and particulate 234Th activity concentrations (in dpm L−1), and POC:234Th ratios (in µmol dpm−1) from both
sediment traps and filtration methods. A total of 379 oceanographic
expeditions and more than 56 600 234Th data points have been gathered in
a single open-access, long-term, and dynamic repository. This paper
introduces the dataset along with informative and descriptive graphics.
Appropriate metadata have been compiled, including geographic location,
date, and sample depth, among others. When available, we also include water
temperature, salinity, 238U data (over 18 200 data points), and
particulate organic nitrogen data. Data source and method information
(including 238U and 234Th) is also detailed along with valuable
information for future data analysis such as bloom stage and
steady-/non-steady-state conditions at the sampling moment. The data are
archived on the PANGAEA repository, with the dataset DOI https://doi.org/10.1594/PANGAEA.918125
(Ceballos-Romero et al., 2021). This provides a
valuable resource to better understand and quantify how the contemporary
oceanic carbon uptake functions and how it will change in future. |
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ISSN: | 1866-3516 1866-3516 |
DOI: | 10.5194/essd-14-2639-2022 |