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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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Atlantic Ocean Islands
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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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North Atlantic
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Atlantic Ocean Islands
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Australasia
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carbon
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Cenozoic
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Tertiary
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Neogene
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upper Miocene
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Paleocene
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lower Paleocene
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Chordata
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Vertebrata
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Pisces
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Chondrichthyes
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Elasmobranchii (1)
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Europe
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Carpathian Foredeep (1)
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Carpathians
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Eastern Carpathians (1)
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Polish Carpathians (2)
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Central Europe
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Magura Nappe (1)
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Poland
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Opole Poland (1)
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Polish Carpathians (2)
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Tarnow Poland (1)
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Southern Europe
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Dobruja Basin
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Romanian Dobruja (1)
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Iberian Peninsula
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Spain
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Andalusia Spain
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Almeria Spain
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Sorbas Basin (1)
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Nevado-Filabride Complex (1)
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Betic Cordillera (3)
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Murcia Spain (1)
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Valencia region
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Alicante Spain (1)
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Italy
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Apennines
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Central Apennines (1)
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Northern Apennines (1)
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Emilia-Romagna Italy
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Parma Italy (1)
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Friuli-Venezia Giulia Italy
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Trieste Italy (1)
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Piemonte Italy
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Alessandria Italy (1)
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Umbria Italy
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Perugia Italy
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Gubbio Italy (1)
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Romania
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Rarau Massif (1)
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Romanian Dobruja (1)
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ichnofossils
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Chondrites ichnofossils (2)
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Planolites (2)
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Thalassinoides (2)
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Zoophycos (1)
-
-
Invertebrata
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Arthropoda
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Mandibulata
-
Crustacea
-
Malacostraca
-
Amphipoda (1)
-
-
-
Insecta
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Pterygota
-
Neoptera
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Endopterygota
-
Coleoptera (1)
-
-
Exopterygota
-
Dermaptera (1)
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-
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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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Foraminifera
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Textulariina (1)
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-
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Vermes
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Annelida (5)
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Polychaeta (5)
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Mesozoic
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Cretaceous
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Lower Cretaceous
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Aptian (1)
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Upper Cretaceous
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Cenomanian (1)
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Kodiak Formation (1)
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K-T boundary (1)
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Maestrichtian (2)
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Senonian (1)
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Turonian
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upper Turonian (1)
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Jurassic
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Lower Jurassic
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Toarcian
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lower Toarcian (1)
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upper Liassic (1)
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Upper Jurassic
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Oxfordian (1)
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Triassic
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Upper Triassic (1)
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metamorphic rocks
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gneisses (1)
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Mexico
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Baja California Sur Mexico (1)
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Pacific Ocean
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South Pacific
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Southwest Pacific (1)
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West Pacific
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paleoclimatology (1)
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algae (1)
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sea-level changes (1)
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sedimentary rocks
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sedimentary structures
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turbidity current structures
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sedimentation (2)
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sediments
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United States
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sedimentary rocks
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sedimentary rocks
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turbidite (1)
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sedimentary structures
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borings (2)
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burrows (10)
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sedimentary structures
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biogenic structures
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bioturbation (3)
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lebensspuren (1)
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turbidity current structures
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Bouma sequence (1)
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tracks (2)
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sediments
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sediments
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clastic sediments
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boulders (1)
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sand (1)
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turbidite (1)
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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
HYBRID NATURE OF A NEW JURASSIC–CRETACEOUS WORM BURROW INDICATED BY MICROBIAL MEDIATION OF ITS WALL FORMATION Available to Purchase
BURROWS AND TRACKWAYS OF THE DERMAPTERAN INSECT LABIDURA RIPARIA (PALLAS, 1773): A CONTRIBUTION TO THE ICHNOLOGY OF SANDY SUBSTRATES Available to Purchase
The trace fossil Polykampton recurvum n. isp. (sequestrichnia) from the Maastrichtian–Paleocene deep-sea deposits of NW Italy Open Access
A NEW TEICHICHNOID TRACE FOSSIL SYRINGOMORPHA CYPRENSIS FROM THE MIOCENE OF CYPRUS Available to Purchase
BURROWS OF THE POLYCHAETE PERINEREIS AIBUHIUTENSIS ON A TIDAL FLAT OF THE YELLOW RIVER DELTA IN CHINA: IMPLICATIONS FOR THE ICHNOFOSSILS POLYKLADICHNUS AND ARCHAEONASSA Available to Purchase
FEEDING TRACES OF RECENT RAY FISH AND OCCURRENCES OF THE TRACE FOSSIL PISCICHNUS WAITEMATA FROM THE PLIOCENE OF SANTA MARIA ISLAND, AZORES (NORTHEAST ATLANTIC) Available to Purchase
A RECORD OF SEQUESTRATION OF PLANT MATERIAL BY MARINE BURROWING ANIMALS AS A NEW FEEDING STRATEGY UNDER OLIGOTROPHIC CONDITIONS EVIDENCED BY PYRITE MICROTEXTURES Available to Purchase
Spirolites radwanskii n. igen. n. isp.: vermetid gastropod attachment etching trace from the middle Miocene rocky coast of the Paratethys, Poland Available to Purchase
Topological analysis of graphoglyptid trace fossils, a study of macrobenthic solitary and collective animal behaviors in the deep-sea environment Available to Purchase
Borings in gneiss boulders in the Miocene (Upper Tortonian) of the Sorbas Basin, SE Spain Available to Purchase
BEETLE BURROWS WITH A TERMINAL CHAMBER: A CONTRIBUTION TO THE KNOWLEDGE OF THE TRACE FOSSIL MACANOPSIS IN CONTINENTAL SEDIMENTS Available to Purchase
ICHNOLOGICAL ANALYSIS OF LATERAL ENVIRONMENTAL HETEROGENEITY WITHIN THE BONARELLI LEVEL (UPPERMOST CENOMANIAN) IN THE CLASSICAL LOCALITIES NEAR GUBBIO, CENTRAL APENNINES, ITALY Available to Purchase
ICHNOLOGICAL RECORD OF ENVIRONMENTAL CHANGES IN EARLY QUATERNARY (GELASIAN–CALABRIAN) MARINE DEPOSITS OF THE STIRONE SECTION, NORTHERN ITALY Available to Purchase
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 Available to Purchase
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 Available to Purchase
A larger agglutinated foraminifer originally described as a marine plant: the case of Arthrodendron Ulrich, 1904 (Foraminifera), its synonyms and homonyms Available to Purchase
A HIGHLY DIVERSE ICHNOFAUNA IN LATE TRIASSIC DEEP-SEA FAN DEPOSITS OF OMAN Available to Purchase
Bichordites and Bichordites-Rosselia Ichnoassemblages from the Lower Pleistocene Tursi Sandstone (Southern Italy) Available to Purchase
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.