Zohar 1 Well, Core 9 (Jurassic to of Israel)

Where: Negev, Israel (31.6° N, 34.7° E: paleocoordinates 10.4° N, 29.3° E)

• coordinate estimated from map

When: Kidod Formation (Arad Group), Callovian to Callovian (166.1 - 157.3 Ma)

Environment/lithology: shallow subtidal; lithified shale

• Since the Late Jurassic, the Middle East has been under the influence of a tensional tectonic regime that resulted in normal faulting throughout the region (Freund et al., 1975). During the Jurassic and Cretaceous a depositional axis developed roughly parallel to the Israeli shoreline (Bein and Gvirztman, 1977; Gvirtzman and Klang, 1972). This "hingeline" formed the boundary between two types of marine environments. The area to the southeast of this boundary was a shallow, shelf environment in which clay and sand were deposited. To the northwest of the hingeline a deep water, slope-type environment existed, in which the percentage of marine carbonates and clays become more abundant.

Size class: microfossils

Preservation: soft parts, original sporopollenin

Collection methods: core, chemical

Primary reference: G. J. Brenner and I. S. Bickoff. 1992. Palynology and age of the Lower Cretaceous basal Kurnub Group from the coastal plain to the Northern Negev of Israel. Palynology 16:137-185 [C. Jaramillo/G. Doria/A. Cardenas ]more details

Purpose of describing collection: biostratigraphic analysis

PaleoDB collection 140282: authorized by Carlos Jaramillo, entered by Gabriela Doria on 07.03.2013

Creative Commons license: CC BY (attribution)

Taxonomic list

unclassified
  -
Pinopsida
 Pinales - Cheirolepidiaceae
Pteridopsida
 Gleicheniales - Gleicheniaceae