This paper reports on research that investigates the effectiveness of residential field courses in geography, earth science and environmental science courses at UK institutions of higher education. The research focuses on the effects of fieldwork in the affective domain, which is thought to be linked to the adoption of effective approaches to learning. Approximately 300 students were surveyed immediately before and after a field class, enabling analysis of changes in responses brought about as a result of the field experience. Potential differences were looked for between groups of students determined by gender, age, previous experience of fieldwork and place of residence. The research finds that fieldwork leads to significant effects in the affective domain. In general, student responses were very positive prior to fieldwork and became more positive as a result of the field experience. Some groups exhibited higher levels of anxiety about this learning method prior to the field class; however, such differences were mitigated by the field experience. This study concludes that fieldwork is good.

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Fossil plankton are difficult to identify but have formed a major component of most marine ecosystems throughout geological time. The earliest fossil heterotrophs include planktic forms, and subsequent adaptive innovations quickly appeared in the plankton; these include metazoans and animals with hard parts. Movement into the plankton occurred sporadically throughout geological history and seems to have been independent of any biological or environmental forcing mechanism. Subsequent radiations and extinctions in the cohort of plankton closely reflect events in the benthos. The diversity of zooplankton rose quickly during the early Paleozoic era, but low plankton diversity characterized the late Paleozoic. Significant radiations during early Mesozoic times led to an overall increase in diversity through the Phanerozoic eon. As the composition of the zooplankton has changed, so has their effect on biogeochemical cycles.

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Jamaica has the best-known fauna of fossil crinoids of the Antillean islands. Two Cretaceous species have been reexamined on the basis of new material. Lower Cretaceous Apiocrinites sp., previously referred to Austinocrinus n. sp. and first documented from a short pluricolumnal, is now known from brachials and further fragments of column. This is the first millericrinid, and only the second non-isocrinid stalked crinoid, to be identified from the Jamaican and Antillean fossil record. Other ossicles may be derived from the cirri of a comatulid. Applinocrinus cretacea (Bather) is well known from the upper Senonian of England, North America and the West Indies, although Caribbean specimens have not been figured previously. Functional interpretations of the mode of life of Applinocrinus suggest that it was a benthic crinoid, presumably with arms. It lived embedded in the sediment.

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