溶解跃面

溶跃面（lysocline）是海洋中碳酸盐溶解速率随深度突然增大的水平深度的界面，Broecker, W. S. (2003), Holland, Heinrich D.; Turekian, Karl K. (eds.), "6.19 - The Oceanic CaCO3 Cycle", Treatise on Geochemistry, Pergamon, pp. 529–549, doi:10.1016/b0-08-043751-6/06119-3, ISBN 9780080437514, retrieved 2019-10-17其深度一般在碳酸鹽補償深度之上。溶跃面也是海底沉积物中古生物钙质壳保存完好与遭受溶蚀的分界面Sigman, D. M.; Boyle, E. A. (2000). "Glacial/interglacial variations in atmospheric carbon dioxide". Nature. 407 (6806): 859–869. Bibcode:2000Natur.407..859S. doi:10.1038/35038000. ISSN 1476-4687. PMID 11057657. S2CID 7136822.
參考文獻

Category:海洋学