A glossary for biometeorology

Here we present, for the first time, a glossary of biometeorological terms. The glossary aims to address the need for a reliable source of biometeorological definitions, thereby facilitating communication and mutual understanding in this rapidly expanding field. A total of 171 terms are defined, with reference to 234 citations. It is anticipated that the glossary will be revisited in coming years, updating terms and adding new terms, as appropriate. The glossary is intended to provide a useful resource to the biometeorology community, and to this end, readers are encouraged to contact the lead author to suggest additional terms for inclusion in later versions of the glossary as a result of new and emerging developments in the field.     

The role of local environment and geographical distance in determining community composition of arbuscular mycorrhizal fungi at the landscape scale

Arbuscular fungi have a major role in directing the functioning of terrestrial ecosystems yet little is known about their biogeographical distribution. The Baas-Becking hypothesis (‘everything is everywhere, but, the environment selects'') was tested by investigating the distribution of arbuscular mycorrhizal fungi (AMF) at the landscape scale and the influence of environmental factors and geographical distance in determining community composition. AMF communities in Trifolium repens and Lolium perenne roots were assessed in 40 geographically dispersed sites in Ireland representing different land uses and soil types. Field sampling and laboratory bioassays were used, with AMF communities characterised using 18S rRNA terminal-restriction fragment length polymorphism. Landscape-scale distribution of AMF was driven by the local environment. AMF community composition was influenced by abiotic variables (pH, rainfall and soil type), but not land use or geographical distance. Trifolium repens and L. perenne supported contrasting communities of AMF, and the communities colonising each plant species were consistent across pasture habitats and over distance. Furthermore, L. perenne AMF communities grouped by soil type within pasture habitats. This is the largest and most comprehensive study that has investigated the landscape-scale distribution of AMF. Our findings support the Baas-Becking hypothesis at the landscape scale and demonstrate the strong influence the local environment has on determining AMF community composition.     

The twenty-four hour activity cycle of captive coypus (Myocastor coypus)

The twenty-four hour activity cycle of captive coypus was investigated by direct visual observation, automatic recording and by measuring the amount of faeces eliminated at hourly intervals. Coypus were active from just before sunset and the "Zeitgeber" or cue for activity onset may be declining light. The activity period usually ended before sunrise and the interval between the end of the period and dawn was inversely related to temperature. The animals fed and defaecated throughout the active period and 80–86 % of the faecal pellets were produced in water. Refection started shortly after the end of the feeding period, when the animals had returned to the nest, and continued until an hour or two after midday.
A model is suggested which involves two passages of food through the gut and a cycle length of 24 hours from ingestion to defaecation. The feeding and defaecation periods were equal in duration, but the refection period was 40% shorter. Hypothetically this may be due to a caecum by-pass mechanism during the second passage of food through the gut so that the defaecation period, like the feeding period, is controlled by the rate at which food passes through the pyloric sphincter. In contrast the period of refection may be controlled by the rate at which food remains are voided from the caecum. Coypus spent the pre-dawn and daylight hours on nests and in contact with familiar conspecifics. These behaviours may have the function of temperature maintenance in the coldest part of the night and of avoiding diurnal predators.     

Long‐term drivers of change in Polylepis woodland distribution in the central Andes

Question: Is the modern patchy distribution of highly biodiverse Polylepis woodlands a consequence of human activity or natural fluctuations in environmental conditions? What are the consequences of changing climate for the tree genus Polylepis? Location: High central tropical Andes. Methods: We characterized the ecological baseline conditions for Polylepis woodlands over the last ca. 370 000 years through: (i) examination of fossil pollen records (Salar de Uyuni and Lake Titicaca) and (ii) a review of autecological information concerning Polylepis. Results: Fossil pollen data revealed fluctuations in the abundance (ca. 0‐34%) of Polylepis pollen before the arrival of humans in South America (>12 000 years ago), indicating that Polylepis did not form permanent continuous woodland before the arrival of humans and that climatic factors can drive rapid vegetation change. Autecological assessment of Polylepis revealed: (i) negative moisture balance, (ii) fire, (iii) waterlogging, and (iv) cloud cover to be critical in determining the niche space available for Polylepis. Conclusions: Polylepis niche space in the central Andes was at a maximum during warm and wet conditions in the past, but might be at a minimum during the warmer and drier than modern conditions predicted for later this century. The sensitivity to past global climate change emphasizes the need for conservation planners to consider model predictions of a warmer central Andes in the coming decades when developing planting schemes. Natural fluctuations in woodland abundance suggest the most effective way for conservation efforts to “mimic” the natural baseline would be to develop a reproductively connected patchwork of communities.