Revised Cenozoic hiatus database

DOI

The differential effects of climate change, sea level, and water mass circulation on deposition/erosion of marine sediments can be constrained from the distribution of unconformities in the world's oceans. I identified temporal and depth patterns of hiatuses ("hiatus events") from a large and chronologically well constrained stratigraphic database of deep-sea sediments. The Paleogene is characterized by few, several million year long hiatuses. The most significant Cenozoic hiatus event spans most of the Paleocene. The Neogene is characterized by short, frequent hiatus events nearly synchronous in shallow and deep water sediments. Epoch boundaries are characterized by peaks in deep water hiatuses possibly caused by an increased circulation of corrosive bottom water and sediment dissolution. The Plio-Pleistocene is characterized by a gradual decrease in the frequency of hiatuses. Future studies will focus on the regional significance of the hiatus events and their possible causes.

Compilation based on the subset of DSDP/ODP holes collected in the "Neptune" micropaleontology database of the ETH Zurich.

Supplement to: Spencer-Cervato, Cinzia (1998): Changing depth distribution of hiatuses during the Cenozoic. Paleoceanography, 13(2), 178-182

Identifier
DOI https://doi.org/10.1594/PANGAEA.860406
Related Identifier IsSupplementTo https://doi.org/10.1029/97PA03440
Related Identifier IsVariantFormOf https://doi.org/10.25921/BYSM-DC39
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.860406
Provenance
Creator Spencer-Cervato, Cinzia
Publisher PANGAEA
Publication Year 1998
Rights Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess true
Representation
Resource Type Supplementary Dataset; Dataset
Format text/tab-separated-values
Size 741 data points
Discipline Earth System Research
Spatial Coverage (-175.297W, -70.832S, 174.948E, 56.956N); North Pacific/RIDGE; North Pacific/BASIN; Mediterranean Sea/RIDGE; Mediterranean Sea/CONT RISE; North Pacific/SLOPE; North Pacific/PLAIN; Indian Ocean//RIDGE; Indian Ocean//FRACTURE ZONE; North Pacific/SEDIMENT POND; North Pacific/ESCARPMENT; North Pacific/ABYSSAL FLOOR; North Pacific Ocean; North Pacific/TRENCH; North Pacific/FLANK; South Atlantic/FLANK; South Atlantic Ocean; South Atlantic/CONT RISE; South Atlantic/PLATEAU; South Atlantic/CREST; Gulf of Mexico; North Atlantic/SPUR; North Atlantic/PLATEAU; North Atlantic/RIDGE; North Pacific/TROUGH; South Pacific/Tasman Sea/CONT RISE; South Pacific/Tasman Sea/PLATEAU; South Pacific/CONT RISE; North Atlantic Ocean; North Atlantic/FLANK; North Atlantic/SLOPE; Weddell Sea; South Indian Ridge, South Indian Ocean; Lakshadweep Sea; Arabian Sea; Indian Ocean; Japan Sea; Coral Sea; South Pacific Ocean
Temporal Coverage Begin 1969-08-15T00:00:00Z
Temporal Coverage End 1991-02-10T20:30:00Z