Journal article icon

Journal article

Large fractionation of calcium isotopes during cave-analogue calcium carbonate growth

Abstract:

We have measured δ44/42Ca of laboratory-precipitated calcite grown in an experimental setup that closely replicates stalagmite formation. Calcium solutions were dripped onto two different substrates in tightly-controlled conditions and calcite precipitated due to rapid CO2 degassing. With seeded glass slides as the substrate, we observe a Ca isotope ratio in the calcite which is ∼0.5‰ per amu lower than that in the growth solution. This fractionation is generally almost twice that observed in previously published calcite growth experiments and indicates a large kinetic effect on Ca isotopes in the stalagmite growth environment. The precipitate forming near the spot where the drip lands shows slightly greater solution-to-precipitate fractionation than calcite further from the drip reflecting a decrease in this kinetic fractionation as precipitation continues. We interpret these results in the context of the model of Fantle and DePaolo (2007) which involves surface entrapment of light Ca isotopes to decrease calcite δ44/42Ca, and depletion of Ca from the solution in the direct vicinity of the growing calcite to increase calcite δ44/42Ca. In the stalagmite setting, the second of these effects is minimized so that calcite Ca isotope ratios are unusually light. This interpretation suggests that stalagmite Ca isotope ratios should decrease with the saturation state of the drip water (i.e. with the growth rate of calcite). Ca isotopes might therefore allow reconstruction of surface entrapment of trace metals and isotopes more generally and might, for instance, allow an assessment of the appropriate relationship between oxygen isotope fractionation and temperature for periods of past growth in stalagmites.

Publication status:
Published
Peer review status:
Peer reviewed

Actions

Access Document

Files:
Publisher copy:
10.1016/j.gca.2011.04.010

Authors

More by this author
Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Role:
Author
More by this author
Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Role:
Author
ORCID:
0000-0002-6279-7137


Publisher:
Elsevier
Journal:
Geochimica et Cosmochimica Acta More from this journal
Volume:
75
Issue:
13
Pages:
3726-3740
Publication date:
2011-04-19
Acceptance date:
2011-04-05
DOI:
ISSN:
0016-7037


Keywords:
Pubs id:
pubs:149840
UUID:
uuid:28d0681c-606c-4c19-b918-de4522cb33fd
Local pid:
pubs:149840
Source identifiers:
149840
Deposit date:
2018-07-05
ARK identifier:

Terms of use


Views and Downloads






If you are the owner of this record, you can report an update to it here: Report update to this record

TO TOP