Aquatic chemistry is becoming both a rewarding and substantial area of inquiry and is drawing many prominent scientists to its fold. Its literature has changed from a compilation of compositional tables to studies of the chemical reactions occurring within the aquatic environments. But more than this is the recognition that human society in part is determining the nature of aquatic systems. Since rivers deliver to the world ocean most of its dissolved and particulate components, the interactions of these two sets of waters determine the vitality of our coastal waters. This significant vol ume provides not only an introduction to the dynamics of aquatic chem istries but also identifies those materials that jeopardize the resources of both the marine and fluvial domains. Its very title provides its emphasis but clearly not its breadth in considering natural processes. The book will be of great value to those environmental scientists who are dedicated to keeping the resources of the hydrosphere renewable. As the size of the world population becomes larger in the near future and as the uses of materials and energy show parallel increases, the rivers and oceans must be considered as a resource to accept some of the wastes of society. The ability of these waters and the sediments below them to accommodate wastes must be assessed continually. The key questions relate to the capacities of aqueous systems to carry one or more pollutants."

Metal pollution in the aquatic environment

Communities of microscopic plant life, or phytoplankton, dominate the Earth's aquatic ecosystems. This important new book by Colin Reynolds covers the adaptations, physiology and population dynamics of phytoplankton communities in lakes and rivers and oceans. It provides basic information on composition, morphology and physiology of the main phyletic groups represented in marine and freshwater systems and in addition reviews recent advances in community ecology, developing an appreciation of assembly processes, co-existence and competition, disturbance and diversity. Although focussed on one group of organisms, the book develops many concepts relevant to ecology in the broadest sense, and as such will appeal to graduate students and researchers in ecology, limnology and oceanography.

/pdf/the-ecology-of-phytoplankton-4ev70n3jsq.pdf

The Ecology of Phytoplankton

Palaeolimnological diatom data comprise counts of many species expressed as percentages for each sample. Reconstruction of past lake-water pH from such data involves two steps; (i) regression, where responses of modern diatom abundances to pH are modelled and (ii) calibration where the modelled responses are used to infer pH from diatom assemblages preserved in lake sediments. In view of the highly multivariate nature of diatom data, the strongly nonlinear response of diatoms to pH, and the abundance of zero values in the data, a compromise between ecological realism and computational feasability is essential. The two numerical approaches used are (i) the computationally demanding but formal statistical approach of maximum likelihood (ML) Gaussian logit regression and calibration and (ii) the computationally straightforward but heuristic approach of weighted averaging (WA) regression and calibration. When the Surface Water Acidification Project (SWAP) modern training set of 178 lakes is reduced by data-screening to 167 lakes, WA gives superior results in terms of lowest root mean squared errors of prediction in cross-validation. Bootstrapping is also used to derive prediction errors, not only for the training set as a whole but also for individual pH reconstructions by WA for stratigraphic samples from Round Loch of Glenhead, southwest Scotland covering the last 10 000 years. These reconstructions are evaluated in terms of lack-of-fit to pH and analogue measures and are interpreted in terms of rate of change by using bootstrapping of the reconstructed pH time-series.

/pdf/diatoms-and-ph-reconstruction-1r5ff7fdn6.pdf

Diatoms and pH Reconstruction

Quantitative interpretation of fossil pollen spectra: Dissimilarity coefficients and the method of modern analogs

A highly T-lymphotropic virus was isolated from cats in a cattery in which all the animals were seronegative for feline leukemia virus. A number of cats in one pen had died and several had an immunodeficiency-like syndrome. Only 1 of 18 normal cats in the cattery showed serologic evidence of infection with this new virus, whereas 10 of 25 cats with signs of ill health were seropositive for the virus. Tentatively designated feline T-lymphotropic lentivirus, this new feline retrovirus appears to be antigenically distinct from human immunodeficiency virus. There is no evidence for cat-to-human transmission of the agent. Kittens experimentally infected by way of blood or plasma from naturally infected animals developed generalized lymphadenopathy several weeks later, became transiently febrile and leukopenic, and continued to show a generalized lymphadenopathy 5 months after infection.

http://science.sciencemag.org/content/sci/235/4790/790.full.pdf

Isolation of a T-lymphotropic virus from domestic cats with an immunodeficiency-like syndrome.

137Cs and 210Pb dating of sediments from soft-water lakes in New England (U.S.A.) and Scandinavia, a failure of 137Cs dating

The Surface Waters Acidification Project Palaeolimnology Programme: Modern Diatom / Lake-Water Chemistry Data-Set

Experiments conducted with natural mixed populations of 800 and 1,800 tubificids m−2 in sediment from Messalonskee Lake, Maine, showed average sediment transport by alimentation at 10°C 2–3 times greater than highest rates previously reported. More than 95% of feeding on introduced pollen was at depths above 7 cm, with greatest feeding at 3–4 cm. Small amounts of pollen were raised to the surface from as deep as 15 cm. Downward transport was 14 and 19% of upward. Small pollen grains (< 40 µ) were fed upon and displaced at higher rates than large grains. Organic matter was less in the surface layer of feces than in sediment from feeding depths and in surface sediment where no worms were present. A mathematical model was used to appraise the stratigraphic effects of the worms by deriving age-frequency composition of sediment at various depths.

https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.4319/lo.1974.19.3.0466

Stratigraphic effects of tubificids in profundal lake sediments1

The contemporary distribution of pollen in eastern North America: A comparison with the vegetation

https://www.cambridge.org/core/services/aop-cambridge-core/content/view/99F0CC646A0A9635CE0E9DBC89D96489/S0033589400017373a.pdf/div-class-title-late-glacial-and-early-holocene-landscapes-in-northern-new-england-and-adjacent-areas-of-canada-div.pdf

Ronald B. Davis

Papers

137Cs and 210Pb dating of sediments from soft-water lakes in New England (U.S.A.) and Scandinavia, a failure of 137Cs dating

The Surface Waters Acidification Project Palaeolimnology Programme: Modern Diatom / Lake-Water Chemistry Data-Set

Stratigraphic effects of tubificids in profundal lake sediments1

The contemporary distribution of pollen in eastern North America: A comparison with the vegetation

Late glacial and early Holocene Landscapes in northern New England and adjacent areas of Canada