This book provides readers with a well-balanced blend of high-quality photographs, figures
and accompanying texts on the identification of trace fossils, both in core and in outcrop …

The deep-marine environment is a complex setting in which numerous processes—settling
of pelagic and hemipelagic particles in the water column, sediment gravity flows (downslope …

Abstract Marine Isotope Stage (MIS) 19 is an important analogue for the present interglacial
because of its similar orbital configuration, especially the phasing of the obliquity maximum …

Abstract The Executive Committee of the International Union of Geological Sciences on
January 17, 2020 ratified the Global Boundary Stratotype Section and Point (GSSP) defining …

The bathyal and abyssal environments represent an extent benthic habitat. The deep-sea
floor is a dynamic setting affected by fluctuations of organic-matter deposition, sedimentation …

The mixed siliciclastic–carbonate Teniet El Klakh Formation (Middle Jurassic, Bajocian)
mainly consists of a monotonous, clay and fine-grained sandstone alternation with some …

Naming trace fossils is necessary if we are to communicate ideas about them. In the
absence of DNA-based molecular analysis, ichnologists must rely on morphologic …

In part composed of Mg calcite and dolomite with a nearly continuous spectrum of MgCO3
contents, carbonates forming at marine methane seeps are ideal candidates to study the …

Slope settings are influenced by numerous factors, including sediment bypass, mass
wasting, incision by canyons and gullies, and/or widespread suspension settling of fine …

Ichnological analysis of the carbonate contourite drift at the Petra Tou Romiou outcrop
(southern Cyprus) reveals a relationship between sea level dynamics, shoreline position …