Occurrence of hiatuses PH and NH 1 through NH 7 in DSDP holes

Miocene paleoceanographic evolution exhibits major changes resulting from the opening and closing of passages, the subsequent changes in oceanic circulation, and development of major Antarctic glaciation. The consequences and timing of these events can be observed in variations in the distribution of deep-sea hiatuses, sedimentation patterns, and biogeographic distribution of planktic organisms. The opening of the Drake Passage in the latest Oligocene to early Miocene (25-20 Ma) resulted in the establishment of the deep circumpolar current, which led to thermal isolation of Antarctica and increased global cooling. This development was associated with a major turnover in planktic organisms, resulting in the evolution of Neogene assemblages and the eventual extinction of Paleogene assemblages. The erosive patterns of two widespread hiatuses (PH, 23.0-22.5 Ma; and NH 1, 20-18 Ma) indicate that a deep circumequatorial circulation existed at this time, characterized by a broad band of carbonate-ooze deposition. Siliceous sedimentation was restricted to the North Atlantic and a narrow band around Antarctica. A major reorganization in deep-sea sedimentation and hiatus distribution patterns occurred near the early/middle Miocene boundary, apparently resulting from changes in oceanic circulation. Beginning at this time, deep-sea erosion occurred throughout the Caribbean (hiatus NH 2, 16-15 Ma), suggesting disruption of the deep circumequatorial circulation and northward deflection of deep currents, and/or intensification of the Gulf Stream. Sediment distribution patterns changed dramatically with the sudden appearance of siliceous-ooze deposition in the marginal and east equatorial North Pacific by 16.0 to 15.5 Ma, coincident with the decline of siliceous sedimentation in the North Atlantic. This silica switch may have been caused by the introduction of Norwegian Overflow Water into the North Atlantic acting as a barrier to outcropping of silica-rich Antarctic Bottom Water. The main aspects of the present oceanic circulation system and sediment distribution pattern were established by 13.5 to 12.5 Ma (hiatus NH 3), coincident with the establishment of a major East Antarctic ice cap. Antarctic glaciation resulted in a broadening belt of siliceous-ooze deposition around Antarctica, increased siliceous sedimentation in the marginal and east equatorial North Pacific and Indian Oceans, and further northward restriction of siliceous sediments in the North Atlantic. Periodic cool climatic events were accompanied by lower eustatic sea levels and widespread deep-sea erosion at 12 to 11 Ma (NH 4), 10 to 9 Ma (NH 5), 7.5 to 6.2 Ma (NH 6), and 5.2 to 4.7 Ma (NH 7).

Análisis de las trayectorias de dolor posoperatorio, primera hora vs. 24 horas. Estudio observacional en 234 pacientes

Introducción: El dolor posoperatorio no controlado es un predictor de dolor severo. La trayectoria de dolor durante la primera hora podría predecir el curso del dolor durante las primeras 24 horas. El control temprano del dolor posoperatorio facilita el manejo analgésico durante el primer día y mejora la experiencia del paciente, facilitando su recuperación y rehabilitación. Objetivo: Determinar la relación entre la trayectoria del dolor en la primera hora y durante las 24 horas post-operatorias. Material y métodos: Estudio analítico observacional prospectivo de 234 pacientes llevados a procedimientos quirúrgicos bajo anestesia general. Se registraron 8 intesidades de dolor durante las 24 horas. Se calcularon las pendientes y se estableció la relación entre ellas. Resultados: El 31,3% de pacientes tenían dolor no controlado al ingreso a recuperación. La intensidad del dolor al inicio se correlaciona de forma negativa con la trayectoria de la primera hora P1 rS= -0,657 (p=0.000). La intensidad de dolor inicial tiene una asociación negativa con P2 de rS= -0.141 (p=0.032). Al compararse las pendientes P1 y P2 y se encontró una correlación negativa muy baja rS= -0.126 (p=0.056). Conclusiones: Uno de cada tres pacientes presenta dolor severo durante el posoperatorio agudo. La trayectoria del dolor en la primera hora no permite predecir el comportamiento de la trayectoria durante el primer día posoperatorio. El comportamiento del dolor está relacionado con la intensidad al final de la anestesia. Cuando el dolor inicial es severo alcanzar la meta analgésica tarda más tiempo.