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Primary terms
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BIVALVES ON THE MOVE: THE INTERPLAY OF EXTRINSIC AND INTRINSIC FACTORS ON THE MORPHOLOGY OF THE TRACE FOSSIL PROTOVIRGULARIA
LATE DEVONIAN AND EARLY MISSISSIPPIAN ECHINODERMS FROM CENTRAL AND NORTHERN IRAN
BIOSTRATIGRAPHY, PALEOECOLOGY, AND TAXONOMY OF DEVONIAN (EMSIAN AND FAMENNIAN) CRINOIDS FROM SOUTHEASTERN MOROCCO
Collections, Data, and Metadata—Time to Fish or Cut Bait!
REDESCRIPTION OF DEVONIAN AND CARBONIFEROUS (PENNSYLVANIAN) BLASTOIDS FROM WESTERN YUNNAN, CHINA
A QUADRUPLING OF FAMENNIAN PELMATOZOAN DIVERSITY: NEW LATE DEVONIAN BLASTOIDS AND CRINOIDS FROM NORTHWEST CHINA
EVALUATING INTERNAL VERSUS EXTERNAL CHARACTERS: PHYLOGENETIC ANALYSES OF THE ECHINOCONCHIDAE, BUXTONIINAE, AND JURESANIINAE (PHYLUM BRACHIOPODA)
A NEW ICHNOSPECIES OF NEREITES FROM CARBONIFEROUS TIDAL-FLAT FACIES OF EASTERN KANSAS, USA: IMPLICATIONS FOR THE NEREITES – NEONEREITES DEBATE
Hexactinellid and calcareous sponges from the Pennsylvanian (Moscovian) Dikanre Formation from Xinjiang-Uygur Autonomous Region, northwestern People's Republic of China
Sedimentary geology; strength in numbers, strength in diversity, and a future for us all
Contrasting behavioral and feeding strategies recorded by tidal-flat bivalve trace fossils from the Upper Carboniferous of eastern Kansas
The ichnogenus Curvolithus revisited
Ichnology of an Upper Carboniferous fluvio-estuarine paleovalley; the Tonganoxie Sandstone, Buildex Quarry, eastern Kansas, USA
The paradox of nonmarine ichnofaunas in tidal rhythmites; integrating sedimentologic and ichnologic data from the Late Cretaceous of eastern Kansas, USA
A camerate-rich Late Carboniferous (Moscovian) crinoid fauna from volcanic conglomerate, Xinjiang, People's Republic of China
Paleoautecology and systematic re-evaluation of Camptocrinus alabamensis (Mississippian: Chesterian) from northern Alabama
A tidal model of Carboniferous Konservat-Lagerstaetten formation
Raymond C. Moore was among the most important stratigraphers and paleontologists of the twentieth century. Yet, he was among the last of his contemporaries (1892 to 1974) to accept the importance of glacial eustasy for sea-level changes during the late Paleozoic. Moore staunchly defended the concept that sea-level changes and resultant lithologic changes were caused primarily by orogenic and diastrophic processes, noting that orogeny in one part of the world could affect sea level globally. Our impression is that Moore was loath to change his mind once he had reached a decision and was a commanding force who could not be ignored easily. Moore was among the many geologists who operated under an epistomological paradigm of their time—if a single action could explain all results, they refused to complicate the issue by invoking multiple causes. Moore’s principal concerns were not the causes of sea-level change, but the effects, especially the great lateral persistence of thin stratigraphic units throughout the midcontinent.