P. Louchouarn et al., EARLY DIAGENETIC PROCESSES IN RECENT SEDIMENTS OF THE GULF OF ST-LAWRENCE - PHOSPHORUS, CARBON AND IRON BURIAL RATES, Marine geology, 139(1-4), 1997, pp. 181-200
Selective extraction procedures were used to quantify different forms
of solid-phase phosphorus, carbon and iron in marine sediments, and to
evaluate the impact of authigenic formation of mineral forms such as
carbonate fluorapatite (CFA), calcium carbonate (CaCO3) and pyrite (Fe
S2) on major elemental cycles during early diagenesis. Detrital P and
Fe phases were successfully used as indicators of the constancy or var
iability of detrital inputs to several sedimentary environments from t
he deep channels of the Gulf of St-Lawrence. In cores characterized by
near steady state influx rates, solid-phase P, C and Fe data and sedi
ment burial rates indicate that CFA, CaCO3 and probably FeS2 are curre
ntly forming in the sediments of the Gulf. However, high concentration
s and/or formation of CaCO3 in marine sediments appear to inhibit the
formation of authigenic CFA. On the other hand, the formation of FeS2
does not influence authigenic CFA precipitation. In the deep troughs o
f the Gulf of St-Lawrence, total P burial rates range from approximate
to 50 to 500 mgP/m(2)/yr. Truly authigenic precipitation of CFA, when
observed, may represent up to approximate to 25% of the total burial
rate of P. Bioturbation of sub-surface sediments reduces the potential
for authigenic precipitation of CFA and CaCO3, thus affecting immobil
ization reactions that have a strong impact on the global oceanic cycl
es of C and P. The spatial heterogeneity of diagenetic reactions precl
udes the establishment of an accurate quantification of P removal on t
he scale of a continental shelf such as the Gulf of St-Lawrence. (C) 1
997 Elsevier Science B.V. All rights reserved.