Chemical properties of the water column were examined at the Indian Deep-se
a Environment Experiment (INDEX) site in the Central Indian Basin (CIB), as
a part of baseline studies prior to the benthic disturbance experiment for
the environmental impact assessment of mining of polymetallic nodules. The
study shows three equatorward moving water masses. (a) The Subsurface Sali
nity Maximum in the depth range 125-200 m, characterized by high salinity (
34.74-34.77 psu) and oxygen minimum associated with weak maxima in nutrient
s. (b) The Deep Oxygen Maximum (234-245 muM) in the depth range 250-750 m,
associated with minima in nutrients and relatively high pH. (c) The Salinit
y Minimum Water (34.714-34.718 psu) corresponding to the Antarctic Intermed
iate Water (AAIW) at depths 800-1200 m in the density (sigma (theta)) range
27.2-27.5. Progressive changes in these characteristics are attributed to
mixing with waters above and below, and to oxidation of organic detritus en
route. Among the three water masses, the oxygen maximum water shows the lo
west changes in its properties, which may suggest that this water mass is m
oving the fastest. (C) 2001 Elsevier Science Ltd. All rights reserved.