Benthic foraminiferal biofacies and stable isotopic record of St. Stephens Quarry, Alabama

We integrate upper Eocene-lower Oligocene lithostratigraphic, magnetostratigraphic, biostratigraphic, stable isotopic, benthic foraminiferal faunal, downhole log, and sequence stratigraphic studies from the Alabama St. Stephens Quarry (SSQ) core hole, linking global ice volume, sea level, and temperature changes through the greenhouse to icehouse transition of the Cenozoic. We show that the SSQ succession is dissected by hiatuses associated with sequence boundaries. Three previously reported sequence boundaries are well dated here: North Twistwood Creek-Cocoa (35.4-35.9 Ma), Mint Spring-Red Bluff (33.0 Ma), and Bucatunna-Chickasawhay (the mid-Oligocene fall, ca. 30.2 Ma). In addition, we document three previously undetected or controversial sequences: mid-Pachuta (33.9-35.0 Ma), Shubuta-Bumpnose (lowermost Oligocene, ca. 33.6 Ma), and Byram-Glendon (30.5-31.7 Ma). An ~0.9 per mil d18O increase in the SSQ core hole is correlated to the global earliest Oligocene (Oi1) event using magnetobiostratigraphy; this increase is associated with the Shubuta-Bumpnose contact, an erosional surface, and a biofacies shift in the core hole, providing a first-order correlation between ice growth and a sequence boundary that indicates a sea-level fall. The d18O increase is associated with a eustatic fall of ~55 m, indicating that ~0.4 per mil of the increase at Oi1 time was due to temperature. Maximum d18O values of Oi1 occur above the sequence boundary, requiring that deposition resumed during the lowest eustatic lowstand. A precursor d18O increase of 0.5 per mil (33.8 Ma, midchron C13r) at SSQ correlates with a 0.5 per mil increase in the deep Pacific Ocean; the lack of evidence for a sea-level change with the precursor suggests that this was primarily a cooling event, not an ice-volume event. Eocene-Oligocene shelf water temperatures of ~17-19 °C at SSQ are similar to modern values for 100 m water depth in this region. Our study establishes the relationships among ice volume, d18O, and sequences: a latest Eocene cooling event was followed by an earliest Oligocene ice volume and cooling event that lowered sea level and formed a sequence boundary during the early stages of eustatic fall.

Vista general de Sn. Felipe [Material gráfico] = Vue genérale de St. Philippe = General view of St. Philip

Resumen: Descripción: vista general de la ciudad de San Felipe, Xátiva desde las afueras

Vista de la puerta de entrada de la fortaleza de Xativa [ [Material gráfico]= Vue de la porte d'entrèe de la forteresse de Xativa, et d'une partie de la ville de St. Philippe = View of the great gate of the fortress of Xativa, and of a part of the town of St. Philip

Datos de publicación tomados de la obra a la que pertenece

1.4 Gaines Family Home at 3932 Weest Belle Place, St. Louis, Missouri

Following the death of Lloyd's father, his family, the size of which is reported to be anywhere from five to 11 siblings, moved to St. Louis, Missouri in 1926, settling in the city's Central West End neighborhood.

2. 6 Memorial for Lloyd Gaines, St. Peter's Cemetery, Normandy, St. Louis County, Missouri

What happened to Gaines? There are many ideas ranging from being murdered or lynched, being bribed to run away, or disappearing on his own to get away from the pressure of celebrity. That final possibility was brought about by Dr. Greene, who claimed that a man who sounded like Gaines had phoned him while in Mexico and wished to meet. The man never showed up. A recent theory is one of where Lloyd was kidnapped by opponents of the Gaines court decision who took him to Jefferson City and lynched him in McClung Park. All of these theories are speculation and the fact remains that Lloyd Gaines’ whereabouts are a mystery to this day.

New Members and Foreign Associates Elected to the National Academy of Sciences on May 1, 2001: 72 New Members Chosen by the Academy

The Academy has elected 72 new members and 15 foreign associates from 10 countries in recognition of their distinguished and continuing achievements in original research. The election was held during the business session of the 138th annual meeting of the Academy. Election to membership in the Academy is considered one of the highest honors that can be accorded a U.S. scientist or engineer. Foreign associates are non-voting members of the Academy, with citizenship outside of the United States.