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Title: Trace metals in contemporary and seventeenth-century Galapagos coral: Records of seasonal and annual variations

Journal Article · · Geochimica et Cosmochimica Acta; (USA)

The authors report trace element/calcium ratios for modern (Cu/Ca, Mn/Ca, Cd/Ca and Pb/Ca) and seventeenth-century (Cu/Ca, Mn/Ca, and Pb/Ca) specimens of Pavona clavus collected in the Galapagos Islands. These data include the first reliable measurements of Cu/Ca ratios in coralline aragonite. They estimate that the ratio of Cu/Ca in the lattice to that in seawater (i.e., the effective distribution coefficient) is {approx} 0.3, lower than the value of 1 observed for several other divalent elements; they estimate the effective distribution coefficient for Mn is {approx} 1. Distribution coefficients in coral aragonite for 8 divalent metals are near unity despite different ionic radii and chemical speciation in seawater. In a modern Hood Island coral, quarter-annually sampled from 1964-73, Cu/Ca ratios decrease twofold from the late 1960s to early 1970s. Mn/Ca and Cd/Ca ratios vary seasonally with upwelling and the generic El Nino. The El Nino Southern Oscillation (ENSO) events of 1965, 1969, and 1972 are marked by suppression of Cd/Ca ratios by about 2.5 nmol/mol, while the Mn/Ca ratio is highest during the strong 1972 ENSO. Pb/Ca ratios were relatively constant throughout this period. From the Cu/Ca record of a seventeenth-century Urvina Bay coral annually sampled from 1600-1725 and the estimated Cu distribution coefficient, surface seawater Cu concentrations at Galapagos during the seventeenth century were similar to present day at 0.7-1.4 nmol/kg. Estimated Pb concentrations were lower at 5-20 pmol/kg, and Mn concentrations were slightly higher at 1.6-2.8 nmol/kg.

OSTI ID:
7188929
Journal Information:
Geochimica et Cosmochimica Acta; (USA), Vol. 54:2; ISSN 0016-7037
Country of Publication:
United States
Language:
English