Crystals of suspended marine barite in the eastern equatorial Pacific: processes of dissolution and effects on crystal morphology

Xiaoxia Sun; Zuosheng Yang; Dejiang Fan; Yunhai Li

doi:10.1007/s00343-015-3353-1

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Crystals of suspended marine barite in the eastern equatorial Pacific: processes of dissolution and effects on crystal morphology

Updated：2023-05-16

- Crystals of suspended marine barite in the eastern equatorial Pacific: processes of dissolution and effects on crystal morphology
- Journal of Oceanology and Limnology Vol. 33, Issue 1, Pages: 194-203(2015)
- Affiliations：
  
  1. College of Marine Geosciences Ocean University of China
  2. Key Laboratory of Submarine Geosciences and Prospecting Technology Ministry of Education
  3. Third Institute of Oceanography State Oceanic Administration
- Author bio：
- Funds：
- DOI：10.1007/s00343-015-3353-1
  CLC：
- Online First：02 September 2014，
  
  Published：2015
- Accepted：
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Sun, X., Yang, Z., Fan, D. et al. Crystals of suspended marine barite in the eastern equatorial Pacific: processes of dissolution and effects on crystal morphology., Chin. J. Ocean. Limnol. 33, 194–203 (2015). https://doi.org/10.1007/s00343-015-3353-1
DOI：

Sun, X., Yang, Z., Fan, D. et al. Crystals of suspended marine barite in the eastern equatorial Pacific: processes of dissolution and effects on crystal morphology., Chin. J. Ocean. Limnol. 33, 194–203 (2015). https://doi.org/10.1007/s00343-015-3353-1 DOI：

摘要

Abstract

Suspended particulate substances were sampled in the eastern equatorial Pacific in water column from surface to near bottom in five stations in 2005

from which 868 barite crystals were recovered. The barite crystals were examined under scanning electron microscopy. About 61% of the total barites crystals contained detectable Sr by energy dispersive X-ray spectrometry. Barite crystals could be classified into four groups based on their morphology: 1) bladed; 2) ovoid or rounded; 3) arrow-like; and 4) irregularly shaped. The arrow-like barite crystals in natural environment has never been reported before. In addition

about a half of the studied crystals showed features of dissolution as cavities or holes inside of the crystals or around their edges. We found that differential dissolution of barite crystals is consequence of heterogeneous Sr distribution in barite crystals. Our results would help in understanding the biogeochemical processes of marine barite formation and preservation in seawater and marine sediments.

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references

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