The carbonate-dominated Albian to Turonian succession is one of the key petroleum
systems of the Arabian Plate. It is dominated by shallow water platform carbonates that were …

The Hesperornithiformes (sometimes referred to as Hesperornithes) are the first known birds
to have adapted to a fully aquatic lifestyle, appearing in the fossil record as flightless, foot …

Mafic igneous rocks of Cretaceous age (80–130 Ma) scattered around the Arctic Ocean are
commonly referred to as the High Arctic Large Igneous Province (HALIP). We have mapped …

Understanding the behavior of the global climate system during extremely warm periods is
one of the major themes of paleoclimatology. Proxy data demonstrate that the equator-to …

The Cretaceous Sarvak Formation (and its equivalents on the Arabian platform) is one of the
most important carbonate reservoirs to have developed under the warm equable climate …

Organic-walled dinoflagellate cyst (dinocyst) and geochemical records across the
Cenomanian–Turonian boundary (CTB) are presented for the NW European reference …

A review of short-term (< 3 myr: c. 100 kyr to 2.4 myr) Cretaceous sea-level fluctuations of
several tens of metres indicates recent fundamental progress in understanding the …

Carbonate sediments within the Mid‐Cretaceous Sarvak Formation form an important
reservoir at the Abteymour oilfield in the western Dezful Embayment, SW Iran. The poroperm …

Understanding of the role of ocean circulation on climate during the Late Cretaceous is
contingent on the ability to reconstruct its modes and evolution. Geochemical proxies used …

Cretaceous carbonates host major hydrocarbon reserves in SW Iran and elsewhere in the
Arabian Plate. Tectonic activity combined with eustatic sea‐level changes resulted in …