Rivalry and red tape
Researchers are suffering as a result of the conflicts between funding agencies. T. V. Padma uncovers plans to heal the rift.
International Stem Cell Tourism and the Need for Effective Regulation: Part I: Stem Cell Tourism in Russia and India: Clinical Research, Innovative Treatment, or Unproven Hype?
Persons with serious and disabling medical conditions have traveled abroad in search of stem cell treatments in recent years. However, weak or nonexistent oversight systems in some countries provide insufficient patient protections against unproven stem cell treatments, raising concerns about exposure to harm and exploitation. The present article, the first of two, describes and analyzes stem cell tourism in Russia and India and addresses several scientific/medical, ethical, and policy issues raised by the provision of unproven stem cell-based treatments within them. The distinction between treatment based on proven clinical research and "innovative treatment" is addressed and the authors conclude that the innovations at issue constitute neither. Regulatory measures need to be developed or strengthened in accord with internationally accepted standards in such countries to protect those seeking stem cell treatments.
Mississippian Barnett Shale: Lithofacies and depositional setting of a deep-water shale-gas succession in the Fort Worth Basin, Texas
The Mississippian Barnett Formation of the Fort Worth Basin is a classic shale-gas system in which the rock is the source, reservoir, and seal. Barnett strata were deposited in a deeper water foreland basin that had poor circulation with the open ocean. For most of the basin's history, bottom waters were euxinic, preserving organic matter and, thus, creating a rich source rock, along with abundant framboidal pyrite. The Barnett interval comprises a variety of facies but is dominated by fine-grained (clay- to silt-size) particles. Three general lithofacies are recognized on the basis of mineralogy, fabric, biota, and texture: (1) laminated siliceous mudstone; (2) laminated argillaceous lime mudstone (marl); and (3) skeletal, argillaceous lime packstone. Each facies contains abundant pyrite and phosphate (apatite), which are especially common at hardgrounds. Carbonate concretions, a product of early diagenesis, are also common. The entire Barnett biota is composed of debris transported to the basin from the shelf or upper oxygenated slope by hemipelagic mud plumes, dilute turbidites, and debris flows. Biogenic sediment was also sourced from the shallower, better oxygenated water column. Barnett deposition is estimated to have occurred over a 25-m.y. period, and despite the variations in sublithofacies, sedimentation style remained remarkably similar throughout this span of time.