An early Holocene sea-level jump and delta initiation

Kazuaki Hori, Yoshiki Saito

Research output: Contribution to journalArticlepeer-review

Abstract

Early Holocene sea-level change controlled the evolution of clastic coastal depositional systems. Radiocarbon-dated borehole cores obtained from three incised-valley-fill systems in Asia (Changjiang, Song Hong, and Kiso River) record very similar depositional histories, especially between about 9000 and 8500 cal BP. Sedimentary facies changes from estuarine sand and mud to shelf or prodelta mud suggest that the marine influence in the incised valleys increased during this period. In addition, large decreases in sediment accumulation rates occurred. A sea-level jump causes an estuarine system and its depocenter to move rapidly landward. It is possible that the final collapse of the Laurentide Ice Sheet, accompanied by catastrophic drainage of glacial lakes, at approximately 8500 cal BP caused such a jump. The jump was followed immediately by a period of decelerated sea-level rise that promoted delta initiation.

Original languageEnglish
Article numberL18401
JournalGeophysical Research Letters
Volume34
Issue number18
DOIs
Publication statusPublished - 2007 Sep 28
Externally publishedYes

ASJC Scopus subject areas

  • Geophysics
  • Earth and Planetary Sciences(all)

Fingerprint Dive into the research topics of 'An early Holocene sea-level jump and delta initiation'. Together they form a unique fingerprint.

Cite this