Oxygen isotope composition of annually banded modern and mid-Holocene travertine and evidence of paleomonsoon floods, Grand Canyon, Arizona, USA

Gary R. O'Brien, Darrell S Kaufman, Warren D. Sharp, Viorel Atudorei, Roderic A Parnell, Laura J. Crossey

Research output: Contribution to journalArticle

47 Citations (Scopus)

Abstract

Holocene and modern travertine formed in spring-fed Havasu Creek of the Grand Canyon, Arizona, was studied to determine the factors governing its oxygen-isotope composition. Analysis of substrate-grown travertine indicates that calculated calcite-formation temperatures compare favorably with measured water temperatures, and include silt-rich laminae deposited by monsoon-driven floods. Ancient spring-pool travertine is dated by U-series at 7380 ± 110 yr and consists of 14 travertine-silt couplets of probable annual deposition. One hundred eighty high-resolution δ18O analyses of this mid-Holocene sample average -11.0‰ PDB. The average value for modern travertine is ∼0.5‰ lower, perhaps because mid-Holocene temperature was higher or there was proportionally greater summer recharge. δ18O cyclicity in the mid-Holocene travertine has average amplitude of 1.9 ± 0.5‰ PDB, slightly less than the inferred modern-day annual temperature range of Havasu Creek. The annual temperature range might have been reduced during the 14-yr interval compared to present, although other non-temperature factors could account for the muted annual variation. Silt-rich laminae within isotopically lower calcite in the modern and mid-Holocene travertine verifies the seasonal resolution of both samples, and suggests that similar temperature-precipitation conditions, as well as monsoon-generated summer floods, prevailed in the mid-Holocene as they do throughout the Grand Canyon region today.

Original languageEnglish (US)
Pages (from-to)366-379
Number of pages14
JournalQuaternary Research
Volume65
Issue number3
DOIs
StatePublished - May 2006

Fingerprint

travertine
canyon
oxygen isotope
Holocene
silt
monsoon
calcite
temperature
cyclicity
summer
Oxygen Isotopes
Travertine
Mid-Holocene
annual variation
Temperature
recharge
water temperature
substrate

Keywords

  • Grand Canyon
  • Holocene paleoclimate
  • Monsoon
  • Oxygen isotopes
  • Travertine

ASJC Scopus subject areas

  • Earth-Surface Processes
  • Earth and Planetary Sciences(all)

Cite this

Oxygen isotope composition of annually banded modern and mid-Holocene travertine and evidence of paleomonsoon floods, Grand Canyon, Arizona, USA. / O'Brien, Gary R.; Kaufman, Darrell S; Sharp, Warren D.; Atudorei, Viorel; Parnell, Roderic A; Crossey, Laura J.

In: Quaternary Research, Vol. 65, No. 3, 05.2006, p. 366-379.

Research output: Contribution to journalArticle

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