Trace fossils, sedimentary facies and parasequence architecture from the Lower Cretaceous Mulichinco Formation of Argentina: The role of fair-weather waves in shoreface deposits

• Autores: Wesolowski, Lindsey J. N.; Buatois, Luís Alberto; Mángano, María Gabriela; Ponce, Juan José; Carmona, Noelia Beatriz
• Año de publicación: 2018
• Idioma: inglés
• Tipo de recurso: artículo
• Materia: Ciencias Exactas y Naturales; Parasequences; Shoreface Variability; Fair-weather Waves; Mulichinco Formation; Neuquén Basin; Ciencias Exactas y Naturales
• Institución: Universidad Nacional de Río Negro

Fil: Wesolowski, Lindsey J. N. University of Saskatchewan. Department of Geological Sciences. Saskatoon, Canada.
Fil: Buatois, Luís Alberto. University of Saskatchewan. Department of Geological Sciences. Saskatoon, Canada.
Fil: Mángano, María Gabriela. University of Saskatchewan. Department of Geological Sciences. Saskatoon, Canada.
Fil: Ponce, Juan José. Universidad Nacional de Río Negro. Instituto de Investigación en Paleobiología y Geología. Río Negro, Argentina.
Fil: Ponce, Juan José. Consejo Nacional de Investigaciones Científicas y Técnicas de Argentina. Buenos Aires, Argentina.
Fil: Carmona, Noelia Beatriz. Universidad Nacional de Río Negro. Instituto de Investigación en Paleobiología y Geología. Río Negro, Argentina.
Fil: Carmona, Noelia Beatriz. Consejo Nacional de Investigaciones Científicas y Técnicas de Argentina. Buenos Aires, Argentina.
Shorefaces can display strong facies variability and integration of sedimentology and ichnology provides a high resolution model to identify variations among strongly storm-dominated (high energy), moderately storm- affected (intermediate energy), and weakly storm-affected (low energy) shoreface deposits. In addition, ichnology has proved to be of help to delineate parasequences as trace-fossil associations are excellent indicators of environmental conditions which typically change along the depositional profile. Shallow-marine deposits and associated ichnofaunas from the Mulichinco Formation (Valanginian, Lower Cretaceous) in Puerta Curaco, Neuquén Basin, western Argentina, were analyzed to evaluate stress factors on shoreface benthos and parasequence architecture. During storm-dominated conditions, the Skolithos Ichnofacies prevails within the offshore transition and lower shoreface represented by assemblages dominated by Thalassinoides isp. and Ophiomorpha irregulaire. Under weakly storm-affected conditions, the Cruziana Ichnofacies is recognized, characterized by assemblages dominated by Thalassinoides isp. and Gyrochorte comosa in the offshore transition, and by Gyrochorte comosa within the lower shoreface. Storm-influenced conditions yield wider ichnologic variability, showing elements of both ichnofacies. Storm influence on sedimentation is affected by both allogenic (e.g. tectonic subsidence, sealevel, and sediment influx) and autogenic (e.g. hydrodynamic) controls at both parasequence and intraparasequence scales. Four distinct types of parasequences were recognized, strongly stormdominated, moderately stormaffected, moderately storm-affected – strongly fair-weather reworked, and weakly stormaffected, categorized based on parasequence architectural variability derived from varying degrees of storm and fair-weather wave influence. The new type of shoreface described here, the moderately storm-affected – strongly fair-weather reworked shoreface, features storm deposits reworked thoroughly by fair-weather waves. During fair-weather wave reworking, elements of the Cruziana Ichnofacies are overprinted upon relict elements of the Skolithos Ichnofacies from previous storm induced deposition. This type of shoreface, commonly overlooked in past literature, expands our understanding of the sedimentary dynamics and stratigraphic architecture in a shoreface susceptible to various parasequence and intra-parasequence scale degrees of storm and fair-weather wave influence.
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