Revised Cenozoic hiatus database
Fuente:
PANGAEA
Guardado en:
| Autor principal: | |
|---|---|
| Formato: | Dataset Open Access |
| Lenguaje: | en |
| Publicado: |
PANGAEA
1998
|
| Materias: | |
| Acceso en línea: | |
| Etiquetas: |
Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
|
| _version_ | 1867168173232488448 |
|---|---|
| author | Spencer-Cervato, Cinzia |
| author_facet | Spencer-Cervato, Cinzia |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | 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. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_860406 |
| institution | PANGAEA |
| language | en |
| publishDate | 1998 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Revised Cenozoic hiatus database Spencer-Cervato, Cinzia 105-647A; 108-659A; 113-689B; 113-690B; 113-693A; 114-699A; 114-700B; 114-703A; 115-707A; 115-707C; 115-709C; 115-710A; 115-710B; 115-711A; 115-714A; 117-721B; 117-728A; 117-731A; 119-737A; 119-738B; 119-738C; 119-744A; 119-745B; 119-746A; 120-747A; 120-747C; 120-748B; 120-748C; 120-749B; 120-751A; 122-762B; 122-762C; 125-786A; 127-797B; 130-803D; 130-806B; 13-125; 13-132; 132-810C; 133-815A; 134-832B; 135-841B; 16-158; 18-173; 18-178; 22-216; 22-217; 24-238; 60-459B; 61-462; 63-469; 63-470; 66-493; 67-495; 67-499; 68-503A; 68-503B; 71-513A; 71-514; 72-516F; 72-517; 73-522; 74-525A; 7-62A; 7-63; 77-540; 80-548; 80-548A; 80-549A; 81-552A; 82-558; 82-563; 85-572A; 85-573; 85-573B; 85-574; 85-574C; 86-577; 86-581; 90-588C; 90-590A; 90-592; 90-593; 90-594; 90-594A; 93-605; 94-607; 94-608; 95-612; Age, maximum/old; Age, minimum/young; Arabian Sea; Coral Sea; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; Elevation of event; Event label; Glomar Challenger; Gulf of Mexico; Indian Ocean; Indian Ocean//FRACTURE ZONE; Indian Ocean//RIDGE; Japan Sea; Joides Resolution; Lakshadweep Sea; Latitude of event; Leg105; Leg108; Leg113; Leg114; Leg115; Leg117; Leg119; Leg120; Leg122; Leg125; Leg127; Leg13; Leg130; Leg132; Leg133; Leg134; Leg135; Leg16; Leg18; Leg22; Leg24; Leg60; Leg61; Leg63; Leg66; Leg67; Leg68; Leg7; Leg71; Leg72; Leg73; Leg74; Leg77; Leg80; Leg81; Leg82; Leg85; Leg86; Leg90; Leg93; Leg94; Leg95; Longitude of event; Mediterranean Sea/CONT RISE; Mediterranean Sea/RIDGE; North Atlantic/FLANK; North Atlantic/PLATEAU; North Atlantic/RIDGE; North Atlantic/SLOPE; North Atlantic/SPUR; North Atlantic Ocean; North Pacific/ABYSSAL FLOOR; North Pacific/BASIN; North Pacific/ESCARPMENT; North Pacific/FLANK; North Pacific/PLAIN; North Pacific/RIDGE; North Pacific/SEDIMENT POND; North Pacific/SLOPE; North Pacific/TRENCH; North Pacific/TROUGH; North Pacific Ocean; Ocean Drilling Program; ODP; Paleoelevation; South Atlantic/CONT RISE; South Atlantic/CREST; South Atlantic/FLANK; South Atlantic/PLATEAU; South Atlantic Ocean; South Indian Ridge, South Indian Ocean; South Pacific/CONT RISE; South Pacific/Tasman Sea/CONT RISE; South Pacific/Tasman Sea/PLATEAU; South Pacific Ocean; Weddell Sea 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. |
| title | Revised Cenozoic hiatus database |
| topic | 105-647A; 108-659A; 113-689B; 113-690B; 113-693A; 114-699A; 114-700B; 114-703A; 115-707A; 115-707C; 115-709C; 115-710A; 115-710B; 115-711A; 115-714A; 117-721B; 117-728A; 117-731A; 119-737A; 119-738B; 119-738C; 119-744A; 119-745B; 119-746A; 120-747A; 120-747C; 120-748B; 120-748C; 120-749B; 120-751A; 122-762B; 122-762C; 125-786A; 127-797B; 130-803D; 130-806B; 13-125; 13-132; 132-810C; 133-815A; 134-832B; 135-841B; 16-158; 18-173; 18-178; 22-216; 22-217; 24-238; 60-459B; 61-462; 63-469; 63-470; 66-493; 67-495; 67-499; 68-503A; 68-503B; 71-513A; 71-514; 72-516F; 72-517; 73-522; 74-525A; 7-62A; 7-63; 77-540; 80-548; 80-548A; 80-549A; 81-552A; 82-558; 82-563; 85-572A; 85-573; 85-573B; 85-574; 85-574C; 86-577; 86-581; 90-588C; 90-590A; 90-592; 90-593; 90-594; 90-594A; 93-605; 94-607; 94-608; 95-612; Age, maximum/old; Age, minimum/young; Arabian Sea; Coral Sea; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; Elevation of event; Event label; Glomar Challenger; Gulf of Mexico; Indian Ocean; Indian Ocean//FRACTURE ZONE; Indian Ocean//RIDGE; Japan Sea; Joides Resolution; Lakshadweep Sea; Latitude of event; Leg105; Leg108; Leg113; Leg114; Leg115; Leg117; Leg119; Leg120; Leg122; Leg125; Leg127; Leg13; Leg130; Leg132; Leg133; Leg134; Leg135; Leg16; Leg18; Leg22; Leg24; Leg60; Leg61; Leg63; Leg66; Leg67; Leg68; Leg7; Leg71; Leg72; Leg73; Leg74; Leg77; Leg80; Leg81; Leg82; Leg85; Leg86; Leg90; Leg93; Leg94; Leg95; Longitude of event; Mediterranean Sea/CONT RISE; Mediterranean Sea/RIDGE; North Atlantic/FLANK; North Atlantic/PLATEAU; North Atlantic/RIDGE; North Atlantic/SLOPE; North Atlantic/SPUR; North Atlantic Ocean; North Pacific/ABYSSAL FLOOR; North Pacific/BASIN; North Pacific/ESCARPMENT; North Pacific/FLANK; North Pacific/PLAIN; North Pacific/RIDGE; North Pacific/SEDIMENT POND; North Pacific/SLOPE; North Pacific/TRENCH; North Pacific/TROUGH; North Pacific Ocean; Ocean Drilling Program; ODP; Paleoelevation; South Atlantic/CONT RISE; South Atlantic/CREST; South Atlantic/FLANK; South Atlantic/PLATEAU; South Atlantic Ocean; South Indian Ridge, South Indian Ocean; South Pacific/CONT RISE; South Pacific/Tasman Sea/CONT RISE; South Pacific/Tasman Sea/PLATEAU; South Pacific Ocean; Weddell Sea |
| url | https://doi.org/10.1594/PANGAEA.860406 |