P. Loubere, THE SURFACE OCEAN PRODUCTIVITY AND BOTTOM WATER OXYGEN SIGNALS IN DEEP-WATER BENTHIC FORAMINIFERAL ASSEMBLAGES, Marine micropaleontology, 28(3-4), 1996, pp. 247-261
A previous study of the relative abundances of benthic foraminifera in
the deep Pacific revealed that surface ocean productivity and bottom
water oxygen signals were strongly imbedded in the foraminiferal data.
The present report examines the nature of the species associations th
at carry the productivity and bottom water oxygen concentration signal
s. Principal components analysis is used to define species association
s independently of the environmental variables. Principal components a
nalysis of the correlation and the covariance matrices of species perc
ents, and of taxon accumulation rate indices, was undertaken. The corr
elation analysis gives equal weight to all taxa while the covariance a
nalysis weights results to the more abundant species. The accumulation
rate index analysis reduces the distorting effects of calculating per
cents, and matrix closure, on the taxon abundance patterns. Deep water
benthic foraminiferal assemblages from the Eastern Pacific Ocean show
species distribution patterns dominated by a response to surface ocea
n productivity. Principal components analysis of either relative abund
ances or accumulation rate indices reveals a consistent set of species
bearing the productivity signal. These include species normally found
at depth (e.g. hispid Uvigerina) and taxa more commonly found on cont
inental margins which are associated with infaunal microhabitats. The
principal components analysis of both relative abundance and accumulat
ion rate indices also shows that there are no taxa which are exclusive
ly responsive to changing bottom water oxygen concentration. Rather, t
his factor acts in concert with other environmental variables (product
ivity in this study) to control benthic assemblage abundance patterns.
Using relative abundance data convolves the oxygen concentration sign
al with the productivity response of the benthic assemblage. However,
experimentation with absolute abundance indices suggests that the oxyg
en signal can be extracted from the assemblage data. This result is co
nsistent with the previous analysis (Loubere, 1994) which yielded an r
(2) of 0.96 for regression of assemblages against oxygen.