Open AccessSedimentary noise and sea levels linked to land–ocean water exchange and obliquity forcing
Author(s) -
Mingsong Li,
Linda A. Hinnov,
Chunju Huang,
James G. Ogg
Publication year - 2018
Publication title -
nature communications
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 5.559
H-Index - 365
ISSN - 2041-1723
DOI - 10.1038/s41467-018-03454-y
Subject(s) - geology , sea level , sedimentary rock , climate change , structural basin , oceanography , stratigraphy , paleontology , orbital forcing , forcing (mathematics) , meltwater , glacial period , climatology , tectonics
In ancient hothouses lacking ice sheets, the origins of large, million-year (myr)-scale sea-level oscillations remain a mystery, challenging current models of sea-level change. To address this mystery, we develop a sedimentary noise model for sea-level changes that simultaneously estimates geologic time and sea level from astronomically forced marginal marine stratigraphy. The noise model involves two complementary approaches: dynamic noise after orbital tuning (DYNOT) and lag-1 autocorrelation coefficient ( ρ 1 ). Noise modeling of Lower Triassic marine slope stratigraphy in South China reveal evidence for global sea-level variations in the Early Triassic hothouse that are anti-phased with continental water storage variations in the Germanic Basin. This supports the hypothesis that long-period (1-2 myr) astronomically forced water mass exchange between land and ocean reservoirs is a missing link for reconciling geological records and models for sea-level change during non-glacial periods.