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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Asia
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Arabian Peninsula
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Oman
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Oman Mountains (1)
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Far East
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China
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Mexico
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elements, isotopes
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fossils
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ichnofossils
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Primary terms
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Asia
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Arabian Peninsula
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Oman
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Oman Mountains (1)
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Far East
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China
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Shandong China
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Huang He delta (1)
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Middle East
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Cyprus (1)
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Atlantic Ocean
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Chordata
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Europe
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Poland
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Southern Europe
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Italy
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Emilia-Romagna Italy
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Umbria Italy
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ichnofossils
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Zoophycos (1)
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Invertebrata
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Arthropoda
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Mandibulata
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Crustacea
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Malacostraca
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Amphipoda (1)
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Insecta
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Pterygota
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Neoptera
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Endopterygota
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Coleoptera (1)
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Exopterygota
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Mollusca
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Bivalvia (1)
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Cephalopoda
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Ammonoidea (1)
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Gastropoda (1)
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Protista
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Textulariina (1)
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Vermes
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Annelida (4)
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Polychaeta (4)
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Mesozoic
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Cretaceous
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Upper Cretaceous
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Cenomanian (1)
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Kodiak Formation (1)
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Maestrichtian (2)
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Turonian
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upper Turonian (1)
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Jurassic
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Toarcian
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upper Liassic (1)
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turbidity current structures
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sediments
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clastic sediments
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BURROWS AND TRACKWAYS OF THE DERMAPTERAN INSECT LABIDURA RIPARIA (PALLAS, 1773): A CONTRIBUTION TO THE ICHNOLOGY OF SANDY SUBSTRATES
The trace fossil Polykampton recurvum n. isp. (sequestrichnia) from the Maastrichtian–Paleocene deep-sea deposits of NW Italy
A NEW TEICHICHNOID TRACE FOSSIL SYRINGOMORPHA CYPRENSIS FROM THE MIOCENE OF CYPRUS
BURROWS OF THE POLYCHAETE PERINEREIS AIBUHIUTENSIS ON A TIDAL FLAT OF THE YELLOW RIVER DELTA IN CHINA: IMPLICATIONS FOR THE ICHNOFOSSILS POLYKLADICHNUS AND ARCHAEONASSA
FEEDING TRACES OF RECENT RAY FISH AND OCCURRENCES OF THE TRACE FOSSIL PISCICHNUS WAITEMATA FROM THE PLIOCENE OF SANTA MARIA ISLAND, AZORES (NORTHEAST ATLANTIC)
A RECORD OF SEQUESTRATION OF PLANT MATERIAL BY MARINE BURROWING ANIMALS AS A NEW FEEDING STRATEGY UNDER OLIGOTROPHIC CONDITIONS EVIDENCED BY PYRITE MICROTEXTURES
Spirolites radwanskii n. igen. n. isp.: vermetid gastropod attachment etching trace from the middle Miocene rocky coast of the Paratethys, Poland
Topological analysis of graphoglyptid trace fossils, a study of macrobenthic solitary and collective animal behaviors in the deep-sea environment
Borings in gneiss boulders in the Miocene (Upper Tortonian) of the Sorbas Basin, SE Spain
BEETLE BURROWS WITH A TERMINAL CHAMBER: A CONTRIBUTION TO THE KNOWLEDGE OF THE TRACE FOSSIL MACANOPSIS IN CONTINENTAL SEDIMENTS
ICHNOLOGICAL ANALYSIS OF LATERAL ENVIRONMENTAL HETEROGENEITY WITHIN THE BONARELLI LEVEL (UPPERMOST CENOMANIAN) IN THE CLASSICAL LOCALITIES NEAR GUBBIO, CENTRAL APENNINES, ITALY
ICHNOLOGICAL RECORD OF ENVIRONMENTAL CHANGES IN EARLY QUATERNARY (GELASIAN–CALABRIAN) MARINE DEPOSITS OF THE STIRONE SECTION, NORTHERN ITALY
Arthrodendron maguricum n. sp., a New Larger Agglutinated Foraminifer from the Eocene Magura Flysch of the Polish Carpathians and its Relationship to Komokiaceans and Trace Fossils
ICHNOFABRIC EVIDENCE FOR THE LACK OF BOTTOM ANOXIA DURING THE LOWER TOARCIAN OCEANIC ANOXIC EVENT IN THE FUENTE DE LA VIDRIERA SECTION, BETIC CORDILLERA, SPAIN
A larger agglutinated foraminifer originally described as a marine plant: the case of Arthrodendron Ulrich, 1904 (Foraminifera), its synonyms and homonyms
A HIGHLY DIVERSE ICHNOFAUNA IN LATE TRIASSIC DEEP-SEA FAN DEPOSITS OF OMAN
Bichordites and Bichordites-Rosselia Ichnoassemblages from the Lower Pleistocene Tursi Sandstone (Southern Italy)
Abstract: A section approximately 30 m thick in the uppermost part of the deltaic lower Pleistocene Tursi Sandstone at Rabatana has been analyzed. It contains Bichordites monastiriensis, rare Macaronichnus segregatis, and very rare Rosselia socialis (Bichordites ichnoassemblage) in the lower part, and abundant B. monastiriensis and R. socialis, and rare M. segregatis ( Bichordites-Rosselia ichnoassemblage), in the upper part. Ichnofabric and sedimentologic features indicate upper- to middle-shoreface conditions in the lower part of the section, decreasing in energy up section to lower-shoreface conditions. The Bichordites ichnoassemblage is related to unstable conditions on the sea floor, which favored infaunal colonization by vagile irregular echinoids. The Bichordites-Rosselia ichnoassemblage is related to more stable conditions in a probably deeper and / or protected environment, and to clearer waters in a declining deltaic system. Under such conditions, colonization by sedentary ?terebelloid tracemakers of R. socialis, which fed on the sea floor, was possible. The low trace-fossil diversity is related to intense bioturbation by echinoids, which prevented colonization by other tracemakers, except for the Rosselia tracemakers.
SURFACE LEBENSSPUREN PRODUCED BY AMPHIPODS AND ISOPODS (CRUSTACEANS) FROM THE ISONZO DELTA TIDAL FLAT, ITALY
Trace fossils after the K–T boundary event from the Agost section, SE Spain
Abstract The Phanerozoic diversity of deep-sea trace fossils, based on 151 flysch formations, displays distinct, non-linear changes through the Phanerozoic, with peaks in the Ordovician-Early Silurian and Early Carboniferous, lowered in the Permian-older Late Jurassic, a peak in the Tithonian-Aptian, lowered in the Albian, and the maximum in the Eocene. The contribution of graphoglyptids in trace fossil assemblages rises gradually up to the end of the Cretaceous, shows a peak in the Palaeocene-Eocene but a depression in the Oligocene. All the changes were probably influenced by competition for food and food supply, bottom water temperatures and oxygenation, and frequency of flysch habitats. There is no clear influence of major biotic crises (Ordovician/Silurian, Cretaceous/Tertiary, Palaeo-cene/Eocene) on the diversity of deep trace fossils, except the Eocene/Oligocene crisis.