| Pisco Basin | |
| Other Name: | Cuenca de Pisco |
| Named For: | City of Pisco, Peru |
| Pushpin Map: | Peru |
| Pushpin Relief: | 1 |
| Coordinates: | -14.25°N -76°W |
| Location: | Western South America |
| State: | Ica Region |
| Cities: | Pisco |
| Onoffshore: | Both |
| Partof: | Circum-Pacific forearc basins |
| Seas: | Eastern Pacific Ocean |
| Rivers: | Pisco River |
| Area: | 300km (200miles) |
| Basin Type: | Forearc basin |
| Orogeny: | Andean |
| Age: | Eocene–Pliocene |
| Stratigraphy: | Stratigraphy |
Pisco Basin (es|Cuenca de Pisco) is a sedimentary basin extending over 300km (200miles) in southwestern Peru.[1] The basin has a 2km (01miles) thick sedimentary fill, which is about half the thickness of more northern foreland basins in Peru.
The oldest known sediments are the Eocene sandstones of the Caballas Formation, while the youngest deposits, the fossiliferous Pisco Formation, date to the Early Pleistocene. In relation to present-day, topography the fill of Pisco Basin makes the upper part of the Coastal Cordillera of southern Peru, the coastal plains, the Ica-Nazca Depression and the Andean foothills.[2]
The basin is renowned for hosting various highly fossiliferous stratigraphic units; the Pisco Formation has provided a wealth of marine mammals (including sloths), birds, fish and other groups, as have the Chilcatay, Otuma and Paracas Formations.
| Lagoonal to near-shore | Bioclastic conglomerate, sandstone | ||||
| Colloncuran | |||||
| Marine | Siltstone, sandstone | ||||
| Deseadan | |||||
| Marine embayment | Bioclastic sandstone, sandstone, silty sandstone, mudstone, dolomitic sediment | ||||
| Paracas | Yumaque | Mudrock, phosphatic shale, diatomite, porcellanite, chert | |||
| Los Choros | Bioclastic conglomerate, sandstone, siltstone, mudrock | ||||
| Fluvial | Sandstone, tuff, coal | ||||
The basin developed in a setting of extensional tectonics from Eocene to the Late Miocene with short-lived episode of basin inversion in the Middle Miocene.[6] Late Pliocene and Pleistocene uplift of the basin may be consequence of the subduction of Nazca Ridge.[3] [7]
Sedimentary strata of the basin shows evidence for a series of marine transgressions during the last 50 million years.[8] These marine transgressions occurred in a sequence 41-34 Ma, 31-28 Ma, 25-16 Ma, 15-11 Ma, 10-5 Ma, and 4-2 Ma.[8] The end of most of the marine transgressions is thought to be associated either with global sea level falls or compressional events in the Andes.[8]
The marine Oligo-Miocene (25–16 Ma[8]) marine transgression is evidenced by a series of sedimentary strata containing fossils of marine diatoms, Peruchilus snails and Pitar and Cucullaea clams.[9] Oligo-Miocene marine environments in the Pisco Basin range from littoral to shelf.[9] Moquegua Basin southeast of Pisco Basin appear to have been unaffected by the transgression.[9]
Within the Andean margin contemporary marine transgressions are also known from southern Chile, Patagonia and Colombia.[9] As such the marine transgression is thought to represent a regional phenomenon with the steadily rising central Andes being an exception.[9]
| Group | Fossils | Notes |
|---|---|---|
| Mammals | ||
| Birds | Palaeospheniscus sp. | |
| Reptiles | ||
| Fish | Carcharhinus cf. brachurus, Carcharodon hastalis, Carcharodon subauriculatus, Hemipristis cf. serra, Isurus desori | |
| Group | Fossils | Notes |
|---|---|---|
| Mammals | ||
| Birds | ||
| Fish | Engraulis sp., Sardinops sp. | |
| Group | Fossils | Notes |
|---|---|---|
| Mammals | Ocucajea picklingi, Supayacetus muizoni, Basilosauridae indet., Mystacodon selenensis, Peregocetus pacificus, Perucetus colossus | |
| Birds | Perudyptes devriesi | |
| Fish | Pristis sp., Myliobatis sp., Clupeiformes sp. | |