Dead delta's former productivity two trillon shells at the mouth of the Colorado River

M. Kowalewski, G. E. Avilla Serrano, K. W. Flessa, G. A. Goodfriend

Research output: Contribution to journalArticlepeer-review

140 Scopus citations

Abstract

The diversion of the Colorado River by dams and irrigation projects, started in the 1930s, triggered the collapse of the Colorado delta ecosystem. Paleontological, ecological, geochronological, stable isotope, field, and satellite image data provide estimates of the delta's benthic productivity during the 1 k.y. directly preceding the artificial shutdown of the river. At least 2 × 10 12 shells of bivalve mollusks make up the current beaches and islands of the delta. The 125 individual valves dated using 14 C-calibrated amino acid racemization indicate that these shells range in age from A.D. 950 to 1950. Seasonal intrashell cycles in δ 18 0 values indicate that average-sized bivalves lived at least 3 yr. The most conservative calculation based on these numbers indicates that during the time of natural river flow, an average standing population of ∼6 × 10 9 bivalve mollusks (population density ∼50/m 2 ) thrived on the delta. In contrast, the present abundance of shelly benthic macroinvertebrates is ∼94% lower (3/m 2 in 1999-2000). The dramatic decrease in abundance testifies to the severe loss of benthic productivity resulting from diversion of the river's flow and the inadequacy of its partial resumption (1981 to present). An integration of paleontological records with geomorphological, geochemical, and geochronological data can provide quantitative insights into human impact on coastal ecosystems.

Original languageEnglish (US)
Pages (from-to)1059-1062
Number of pages4
JournalGeology
Volume28
Issue number12
DOIs
StatePublished - 2000

Keywords

  • Colorado River
  • Estuary
  • Holocene
  • Paleoecology
  • Productivity

ASJC Scopus subject areas

  • Geology

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