The disappearance of muntjac (Muntiacus reevesi) and roe deer (Capreolus capreolus) pellet groups in a pine forest of lowland England

Reliable knowledge of the disappearance rate of faecal pellets is essential for converting pellet density to deer density when using standing-crop pellet-group counts. Disappearance of muntjac and roe deer pellet groups was monitored in four growth stages of a pine forest of lowland England over a 15-month period. Time to disappearance of the pellet groups (days) of both species significantly differed between habitats and months; it was shorter in late summer to early autumn and in habitats with more ground vegetation. Muntjac pellet groups disappeared more quickly than roe deer pellet groups. Time to disappearance of roe deer pellet groups was negatively correlated with air and grass temperature in pre-thicket and pre-fell habitats, while time to disappearance of muntjac pellet groups was negatively correlated with frequency of rainfall and positively correlated with the run of wind (air passage over a site within a 24-h period measured in km) in pre-thicket habitats. It is the time of the standing-crop pellet-group counts and the disappearance rate of pellet groups deposited in different months and habitats that determine the appropriate method for conversion of pellet-group density to deer density

New palaeontological data from the excavation of the Late Glacial Glencrieff miring bone deposit, North Canterbury, South Island, New Zealand

The avifauna from the Glencrieff swamp deposit in North Canterbury, South Island, New Zealand, is described. Radiocarbon ages of moa bones bracket miring at the site to between 10,000 and 12,000 (uncalibrated) years BP. Heavy-footed moa (Pachyornis elephantopus) and eastern moa (Emeus crassus) dominated the moa assemblage at the site, while South Island giant moa (Dinornis robustus) and stout-legged moa (Euryapteryx curtus, formerly E. gravis (in part)) were rare. The total assemblage from the site consists of at least 1896 bones from 18 species of birds, of which nine are extinct and a further three locally extinct. In addition, we report on the discovery of the oldest known moa gizzard contents, the palynology of the Glencrieff deposit and comment on significant recent changes in site preservation conditions that are threatening the continued preservation of this significant fossil deposit.N. J. Rawlence, R. P. Scofield, J. R. Wood, J. M. Wilmshurst, N. T. Moar and T. H. Worth