Rhizocorallium is one of the oldest known trace fossils, with wide distribution through the
Phanerozoic and all over the world. Originally introduced from the epicontinental Triassic of …

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 …

The ichnofacies paradigm has evolved over a six-decade period since its original inception
by Dolf Seilacher. It is a multidimensional framework underpinned by recurring, facies …

The analysis of macroinvertebrates, trace fossils, calcareous nannofossils and geochemistry
from Pliensbachian to Lower Toarcian deposits of the Subbetic (Southern Spain) allows us …

Turbiditic depositional systems are characterized by diverse, pre-and post-depositional trace
fossils dominated by pascichnia, fodinichnia, agrichnia, and chemichnia. They belong …

Trace fossils are an in-situ record of the infaunal ecosystem and can be used to constrain
paleoenvironmental conditions at the time of animal colonization. However, in …

Abstract The Mesozoic Marine Revolution (MMR) was a major evolutionary episode
involving the large-scale restructuring of shallow-marine benthic communities and the rise to …

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 …

Zoophycos, the latter two have an open tube. Each of these activities leads to intense
sediment mixing and prevents or disturbs the formation of near-surface burrows including …