Biogenic sedimentary structures are evidence of organism–substrate interactions preserved in rocks and sediments, including those recorded in estuarine environments. Their study is termed “paleoichnology” (from the Greek palaios ¼ old, ancient and ichnos ¼ a trace, a track), whereas similar studies in modern sediments are referred to as “neoichnology.” Markings that do not reflect the behavior of organisms (e.g., marks made by the shells of dead mollusks passively transported on the seafloor by waves and/or currents) are excluded from the trace fossils. In addition, biogenic sedimentary structures do not include body fossils (direct remains, such as shells, bones, teeth, etc.) or molds of organism bodies
Bioerosion is a common process in lithified substrates. Nevertheless, organic shelly substrates can ...
This field and laboratory study examines whether regularly patterned biofilms on present-day interti...
Organism-substrate interactions and their products \u2013 biogenic structures \u2013 are important b...
Biogenic sedimentary structures are evidence of organism–substrate interactions preserved in rocks ...
Conical sedimentary structures are widespread in the geological column. Those that are mediated by o...
Bioerosion trace fossils in bones are defined as biogenic structures that cut or destroy hard bone t...
There are different criteria that are usually analysed independently before identifying a new trace ...
International audienceMorphologically diverse organo-sedimentary structures (including microbial mat...
Traces of organisms ’ burrowing movements in the once-soft sediment are most commonly manifested as ...
Organism-substrate interactions and their products – biogenic structures – are important biosignatur...
This study documents the processes involved in forming flaser and wavy bedding governed by microbial...
Bioerosion is a common process in lithified substrates. Nevertheless, organic shelly substrates can ...
This field and laboratory study examines whether regularly patterned biofilms on present-day interti...
Organism-substrate interactions and their products \u2013 biogenic structures \u2013 are important b...
Biogenic sedimentary structures are evidence of organism–substrate interactions preserved in rocks ...
Conical sedimentary structures are widespread in the geological column. Those that are mediated by o...
Bioerosion trace fossils in bones are defined as biogenic structures that cut or destroy hard bone t...
There are different criteria that are usually analysed independently before identifying a new trace ...
International audienceMorphologically diverse organo-sedimentary structures (including microbial mat...
Traces of organisms ’ burrowing movements in the once-soft sediment are most commonly manifested as ...
Organism-substrate interactions and their products – biogenic structures – are important biosignatur...
This study documents the processes involved in forming flaser and wavy bedding governed by microbial...
Bioerosion is a common process in lithified substrates. Nevertheless, organic shelly substrates can ...
This field and laboratory study examines whether regularly patterned biofilms on present-day interti...
Organism-substrate interactions and their products \u2013 biogenic structures \u2013 are important b...