PhotosLocation


ambolafotsy+formation Latitude and Longitude:

13°48′S 49°30′E / 13.8°S 49.5°E / -13.8; 49.5
From Wikipedia, the free encyclopedia
Ambolafotsy Formation
Stratigraphic range: Turonian
~93.52–89.77  Ma
O
S
D
C
P
T
J
K
N
Type Geological formation
Unit of Diego Basin
Sub-unitsLower, Middle and Upper units
Lithology
Primary Claystone, shale, sandstone
Location
Coordinates 13°48′S 49°30′E / 13.8°S 49.5°E / -13.8; 49.5
Approximate paleocoordinates 33°24′S 40°24′E / 33.4°S 40.4°E / -33.4; 40.4
Region Antsiranana Province
Country  Madagascar
Ambolafotsy Formation is located in Madagascar
Ambolafotsy Formation
Location of the formation in Madagascar

The Ambolafotsy Formation is a Turonian aged geological formation in the Diego Basin of Antsiranana Province in Madagascar. It is a mostly terrestrial unit deposited during a marine regression close to the shoreline. The dinosaur Dahalokely has been discovered in the formation. [1]

Description

The section containing the Dahalokely site is informally termed the "Ambolafotsy Formation" and is divided into lower, middle (containing the type locality), and upper units. The lower unit has produced several biostratigraphically informative foraminifera, including Whiteinella aprica, W. baltica, Helvetoglobotruncana praehelvetica, and H. helvetica, and the nannofossil Quadrum gartneri, placing the sample within the Q. gartneri and H. helvetica zones. The upper unit contains the ammonite Subprionocyclus neptuni. [1] [2]

The sediments of most of the middle unit of the Ambolafotsy Formation are interpreted as terrestrial, deposited during a marine regression. Carbonized plant fragments are quite common in the middle unit, along with claystones, shales, and cross-bedded sandstones. Marine microfossils and macrofossils are generally absent, although a deposit of ostreids several meters above the type locality for Dahalokely suggests that the area was deposited close to the shoreline. [1] [2]

See also

References

  1. ^ a b c Farke, Andrew A.; Sertich, Joseph J. W. (2013). "An Abelisauroid Theropod Dinosaur from the Turonian of Madagascar". PLOS ONE. 8 (4): e62047. Bibcode: 2013PLoSO...862047F. doi: 10.1371/journal.pone.0062047. ISSN  1932-6203. PMC  3630149. PMID  23637961.
  2. ^ a b Near Ampandriambengy, around the area of Antsiranana at Fossilworks.org

ambolafotsy+formation Latitude and Longitude:

13°48′S 49°30′E / 13.8°S 49.5°E / -13.8; 49.5
From Wikipedia, the free encyclopedia
Ambolafotsy Formation
Stratigraphic range: Turonian
~93.52–89.77  Ma
O
S
D
C
P
T
J
K
N
Type Geological formation
Unit of Diego Basin
Sub-unitsLower, Middle and Upper units
Lithology
Primary Claystone, shale, sandstone
Location
Coordinates 13°48′S 49°30′E / 13.8°S 49.5°E / -13.8; 49.5
Approximate paleocoordinates 33°24′S 40°24′E / 33.4°S 40.4°E / -33.4; 40.4
Region Antsiranana Province
Country  Madagascar
Ambolafotsy Formation is located in Madagascar
Ambolafotsy Formation
Location of the formation in Madagascar

The Ambolafotsy Formation is a Turonian aged geological formation in the Diego Basin of Antsiranana Province in Madagascar. It is a mostly terrestrial unit deposited during a marine regression close to the shoreline. The dinosaur Dahalokely has been discovered in the formation. [1]

Description

The section containing the Dahalokely site is informally termed the "Ambolafotsy Formation" and is divided into lower, middle (containing the type locality), and upper units. The lower unit has produced several biostratigraphically informative foraminifera, including Whiteinella aprica, W. baltica, Helvetoglobotruncana praehelvetica, and H. helvetica, and the nannofossil Quadrum gartneri, placing the sample within the Q. gartneri and H. helvetica zones. The upper unit contains the ammonite Subprionocyclus neptuni. [1] [2]

The sediments of most of the middle unit of the Ambolafotsy Formation are interpreted as terrestrial, deposited during a marine regression. Carbonized plant fragments are quite common in the middle unit, along with claystones, shales, and cross-bedded sandstones. Marine microfossils and macrofossils are generally absent, although a deposit of ostreids several meters above the type locality for Dahalokely suggests that the area was deposited close to the shoreline. [1] [2]

See also

References

  1. ^ a b c Farke, Andrew A.; Sertich, Joseph J. W. (2013). "An Abelisauroid Theropod Dinosaur from the Turonian of Madagascar". PLOS ONE. 8 (4): e62047. Bibcode: 2013PLoSO...862047F. doi: 10.1371/journal.pone.0062047. ISSN  1932-6203. PMC  3630149. PMID  23637961.
  2. ^ a b Near Ampandriambengy, around the area of Antsiranana at Fossilworks.org

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