A Fossil Vertebrate Fauna Accumulated by Laughing Owls (Sceloglaux Albifacies) on the Gouland Downs, Northwest Nelson, South Island
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WORTHY Palaeofaunal Surveys, 2A Willow Park Drive, Masterton, New Zealand [email protected] Abstract A rich fossil fauna accumulated by laughing owls (Sceloglaux albfacies) during the Holocene, is described from GDlOl Cave, on the Gouland Downs, northwest Nelson, South Island, New Zealand. Twenty-eight species of bird, a tuatara, 3 frogs, at least 4 geckos, 1 skink, 2 bats, and 2 fish contribute to the species diversity. The fauna includes the first inland fossil record of New Zealand dotterel (Charadrius obscurus).The taphonomy of the deposit and the diet of the owl are discussed. Worthy, T.H. 2001. Afossil vertebrate fauna accumulated by laughing owls (Sceloglaux albfacies) on the Gouland Downs, northwest Nelson, New Zealand. Notornis 48(4): 225-233. Keywords fossil fauna; prey remains; Sceloglaux; laughing owl; taphonomy; Gouland Downs; New Zealand INTRODUCTION The exceptions are the 3 faunas from Takaka Hill, Fossil faunas reveal something of the past life in a which have been attributed to laughing owls region and provide valuable insights on past dis- (Sceloglaux albifacies). Two of these, Predator Cave tributions and ecology of animals. In addition, and Hawke's Cave owl deposits, have been de- where a fossil deposit results from the feeding ac- scribed (Worthy & Holdaway 1994a, 1996), but a tivities of a predator, it can be invaluable in under- 3rd in Kairuru Cave, has been only recently exca- standing that predator's biology. This paper de- vated by the author and R. N. Holdaway (MNZ scribes a unique fossil fauna from the Gouland collection, unpubl. data). Downs in Northwest Nelson, South Island, New The fauna described here from the Gouland Zealand. Downs is attributed to the activities of laughing owls Although fossil faunas have not been described and comes from a site at relatively high altitude in from the Gouland Downs area before, others have an area with both open and forested habitats. Laugh- been from Honeycomb Hill Cave in the Oparara ing owls preyed on a wide variety of species (Wor- Basin (Worthy & Mildenhall 1989; Worthy 1993)and thy & Holdaway 1994a,b; Holdaway &Worthy 1996), Megamania Cave in the Gunner River Valley to the and so deposits accumulating their prey remains south (Worthy 1998). To the west, small faunal as- differ greatly from the pitfall trapped faunas more semblages are known from caves on the coast near commonly found in caves. The latter are dominated Paturau (author's unpubl. data). East of Gouland by flightless species and there is a heavy bias towards Downs, faunas are known from Mt Arthur and Mt larger species being both preserved and found. The Owen (Worthy 1989) and the Takaka region (Wor- rich and diverse fauna reported here adds signifi- thy & Holdaway 199413). However, except for 3 on cantly to knowledge of the prehuman fauna of the Takaka Hill, these sites are not comparable. The area, particularly of the small vertebrates, and to many sites in Honeycomb Hill Cave are all at a knowledge of the diet of the laughing owl. lower elevation, and those at Megamania lower still. All are primarily pitfall deposits with the occasional SITE LOCATION vagrant death represented as well. On the high al- The fossil site is in GDlOl Cave at an elevation of titude sites on Mt Arthur and Mt Owen, all faunas c.620 m on the Gouland Downs, Northwest Nelson, have a pitfall origin, as do most in the Takaka area. South Island (Fig. 1). The cave lies within an out- crop of limestone about 250 m wide and 1km long in the floor of the Gouland Downs and it carries a Received 3 October 2000; accepted 23 March 2001 stream westward through a beech forest remnant. 226 Worthy Cape Farewell Tasman Mountains Gunner Downs LPJKaramea River Fig. 1 The location of GDlOl Cave, South Island, New Zealand, showing major rivers and the nearby major fossil sites of Megamania Cave and Honeycomb Hill Cave. Other major fossil localities include Mount Arthur, about 40 km east of Honeycomb Hill Cave, and Takaka Hill on the range east of and parallel to Takaka River. New Zealand metric grid. Fossil vertebrates from Gouland Downs 227 The fossils were found in the resurgence entrance rocky outcrops support a low, sparse forest of of this cave, NZMS 260,1:50,000, M26 554350. The Nothofagus spp. and Dacrydium spp. The Downs are entrance is c.10 m wide and is c.6 m high in the crossed at regular intervals by swift-flowing middle and opens to the west, so receiving after- streams with gravel or stony beds. noon sun. The floor of the entrance is, at its lowest The native avifauna of the Gouland Downs area point, c.3 m above the ground below, but the fossil- is limited at present. On 6 September 1999, I saw or bearing ledges are c.5 m above the ground and face heard the following birds within 1 km of the cave: towards the centre of the entrance. The edge of the great spotted kiwi (Apteryx haastii), blue duck ledge is U-shaped, so is furthest back from the en- (Hymenolaimus malacorhynchos), morepork (Ninox trance drip-line in the centre and converges on the novaeseelandiae), weka (Gallirallus australis), kea drip-line at either side. Walking or climbing access (Nestor notabilis), rifleman (Acanthisitta chloris) [very is not possible from this western opening, but rather common], tomtit (Petroica macrocephala), welcome is effected through a tom0 entrance c.20 m back from swallow (Hirundo tahitica), pipit (Anthus the cliff edge, and then negotiating a series of novaeseelandiae), fernbird (Bowdleria punctata), grey rockfall slopes. warbler (Gerygone igata), bellbird (Anthornis The fossil deposit is on the ledge on the true right melanura), silvereye (Zosterops lateralis), blackbird (northern) side of the entrance where the sediment (Turdus merula), and goldfinch (Carduelis carduelis). slopes down from the wall for c.3 m to the vertical Of other species, yellow-crowned parakeets drop. The sediment is composed of the weathering (~~anoram~kusauriceps) are uncommon in the area, products of the Oligocene limestone roof and walls. and kaka (Nestor meridionalis) and falcon (Falco It is a yellowish-brown sandy loam with many frag- novaeseelandiae) could be expected to visit the area. ments of barnacles, and includes many pieces of Brown creeper (Mohoua novieseelandiae) are present limestone spalled from the roof. Material that has in nearby forests. slid downslope off the ledge has been washed away The extant herpetofauna in the area is unknown. by the stream flowing from the waterfall in the cen- tre of the entrance. Fossils were found along c.5 m METHODS of this ledge from a point where the sediment ex- I first identified fossil bones at the site on 6 Sep- tends closest to the drip-line of the entrance on the tember 1999 and found that the deposit contained northern wall. Sieving of test samples showed that a diverse fauna of birds and reptiles. On 9 May bones were concentrated in the middle of the zone 2000, Don Fraser and I excavated about 2.5 m2 of around a hollow c.500 mm across and 200 mm deep the site, leaving fossiliferous sediment extending against the cave wall. The top 150 mm of the de- at least 2 m on either side. Within the 2.5 m2, work- posit in this region had a ge-ater organic compo- ing upslope from the cliff-edge, all sediment nent appearing as a reddish loam, but below this trapped behind larger limestone blocks was sieved the sediments were yellowish and had no bone. The first, followed by an area c.1 m wide about the 'nest- hollow was probably a nest. hollow'. The sediment was excavated to a depth of c.250 mm because bones were concentrated in the Extant vegetation and fauna of the study area top 150 mm; the sediment below 250 mm was bar- Druce & Simpson (1974) described the vegetation ren. The sediment was passed through a sieve (6 of the Gouland Downs. The limestone areas are mm-mesh) onto a 2 mm-mesh sieve. Bones were vegetated in a mixed silver beech (Nothofagus sorted on site from the material retained in the 6 menziesii) and mountain beech (N.