Host specificity of the symbiotic cyanobacterium<Emphasis Type="Italic"> Oscillatoria spongeliae</Emphasis> in marine sponges,<Emphasis Type="Italic"> Dysidea</Emphasis> spp.

Marine sponges can host a variety of cyanobacterial and bacterial symbionts, but it is often unclear whether these symbionts are generalists that occur in many host species or specialists that occur only in certain species or populations of sponges. The filamentous cyanobacterium Oscillatoria spongeliae is found in the sponges Dysidea n. sp. aff. herbacea 1A and 1B, and similar cyanobacteria are found in D. n. sp. aff. granulosa. We amplified and sequenced sponge nuclear ribosomal DNA (rDNA) and cyanobacterial 16S rDNA from specimens of these three sponges. We then used these sequences to construct phylogenies for host sponges and their symbiotic cyanobacteria. Each of these three sponge species hosts a distinct cyanobacterial clade, suggesting a high degree of host specificity and potential coevolution between symbiotic cyanobacteria and their host sponges.     

Sources and Quantities of Fluorides Evolved from the Manufacture of Fertilizer and Related Products

Fluoride emission rates from the manufacture of phosphoric acid, run-of-pile triple super-phosphate, diammonium phosphate, and granular triple super-phosphate are presented in tabular form. In discussing the information, variations to the usual arrangements and operating practices are mentioned. Fluoride emissions from the manufacturing or producing of related phosphatic products such as defluorinated and calcined phosphate rock, normal super-phosphate, super-phosphoric acid and elemental phosphorus are also discussed. The information is based entirely upon the fertilizer and related phosphate products manufactured in Polk and Hillsborough Counties in Florida. This area produces 75% of the marketable phosphate rock in the United States. Some 40% of the rock remains in these two counties for chemical or thermal processing. The phosphate industry is required to report on fluoride emission levels found by their sampling and monitoring programs. These values are compared with those found by the Florida State Board of Health’s source sampling and monitoring program.     

Phytoextraction of excess soil phosphorus

In the search for a suitable plant to be used in P phytoremediation, several species belonging to legume, vegetable and herb crops were grown in P-enriched soils, and screened for P accumulation potentials. A large variation in P concentrations of different plant species was observed. Some vegetable species such as cucumber (Cucumis sativus) and yellow squash (Cucurbita pepo var. melopepo) were identified as potential P accumulators with >1% (dry weight) P in their shoots. These plants also displayed a satisfactory biomass accumulation while growing on a high concentration of soil P. The elevated activities of phosphomonoesterase and phytase were observed when plants were grown in P-enriched soils, this possibly contributing to high P acquisition in these species. Sunflower plants also demonstrated an increased shoot P accumulation. This study shows that the phytoextraction of phosphorus can be effective using appropriate plant species.     

Advancing the Integration of History and Ecology for Conservation

Abstract: The important role of humans in the development of current ecosystems was recognized decades ago; however, the integration of history and ecology in order to inform conservation has been difficult. We identified four issues that hinder historical ecological research and considered possible solutions. First, differences in concepts and methods between the fields of ecology and history are thought to be large. However, most differences stem from miscommunication between ecologists and historians and are less substantial than is usually assumed. Cooperation can be achieved by focusing on the features ecology and history have in common and through understanding and acceptance of differing points of view. Second, historical ecological research is often hampered by differences in spatial and temporal scales between ecology and history. We argue that historical ecological research can only be conducted at extents for which sources in both disciplines have comparable resolutions. Researchers must begin by clearly defining the relevant scales for the given purpose. Third, periods for which quantitative historical sources are not easily accessible (before AD 1800) have been neglected in historical ecological research. Because data from periods before 1800 are as relevant to the current state of ecosystems as more recent data, we suggest that historical ecologists actively seek out data from before 1800 and apply analytic methods commonly used in ecology to these data. Fourth, humans are not usually considered an intrinsic ecological factor in current ecological research. In our view, human societies should be acknowledged as integral parts of ecosystems and societal processes should be recognized as driving forces of ecosystem change.