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An analysis of the movements of the Spangled Drongo in eastern Australia (late 1800s-mid 1990s)

机译:对东澳大利亚州亮斑燕鸥运动的分析(1800年代后期至1990年代中期)

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摘要

Movements of the Spangled Drongo Dicrurus bracteatus in eastern Australia were examined using records (n = 3461) from the first Atlas of Australian Birds of the Royal Australasian Ornithologists Union from 1977 to 1981, and records from Sydney and Wollongong, New South Wales, from 1981 to 1990 (n = 160), data from unpublished studies, banding information and a comprehensive review of the literature before 1995. Three distinct movements were recognised, all of which were linked to the breeding season in spring and summer. First, there was a southward migration in Queensland during spring, immediately before the breeding season, and a northward return movement in autumn. The southward migration comprised subspecies D.b. atrabectus andD.b. bracteatus north and south of the Burdekin Gap, QId, respectively. This movement was obvious from Torres Strait to Rockhampton and was concentrated near the coast, whereas the northward return movement in autumn was spatially more widespread. Second, there appeared to be an eastward movement immediately after the breeding season from the eastern slopes of the central Great Dividing Range to lower coastal areas within a few kilometres of the sea, and a corresponding westward movement in spring. This altitudinal movement comprised only the subspecies D.b. bracfeafus.lt was evident between latitudes 21°S (Mackay, QId) and 31°S (Nambucca Heads, NSW), and was sometimes small in scale with respect to distance from, or elevation above, the sea. Third, there was a small southward movement of birds of subspecies D.b. bracteatus in NSW in autumn, immediately after the breeding season, and a northward return movement in spring. This southward movement was evident from Forster (32°S) to the far south coast of NSW, whereas the corresponding northward return was less obvious. Spangled Drongos that moved southwards in NSW in autumn were confined mostly to coastal areas <15 km from the sea. It is proposed that the Drongos moving southwards in NSW in autumn are an extension of the D.b. bracteatus population that descends altitudinally eastwards and overwinters on the coast in southern Queensland and northern NSW.
机译:使用1977年至1981年皇家澳大利亚鸟类学会联合会的第一批澳大利亚鸟类地图集(n = 3461)以及1981年来自新南威尔士州悉尼和卧龙岗的记录(n = 3461)检查了澳大利亚东部亮片Drongo Dicrurus bracteatus的运动到1990年(n = 160),来自未发表研究的数据,带状信息和对1995年之前文献的全面回顾。人们认识到三个不同的运动,所有这些运动都与春季和夏季的繁殖季节有关。首先,在繁殖季节即将来临的春季,昆士兰州向南迁移,而秋季则向北迁移。向南迁移包括亚种D.b. atrabectus和D.b.布尔迪克特(Bracteatus)位于布尔德金峡(Bidekin Gap)北部和南部,分别为QId。该运动从托雷斯海峡到罗克汉普顿很明显,并且集中在海岸附近,而秋季的北向运动在空间上更广泛。其次,在繁殖季节之后,似乎出现了从大分水岭中央的东坡到海面几公里以内的沿海低端地区的向东运动,而在春季则出现了向西运动。这种垂直运动仅包括亚种D.b。 bracfeafus.lt在21°S(Mackay,QId)和31°S(Nambucca Heads,NSW)纬度之间很明显,有时离海面的距离或海拔高度较小。第三,亚种D.b.的鸟类有少量向南运动。繁殖季节后不久,秋天在新南威尔士州出现br,春季则向北返回。从福斯特(32°S)到新南威尔士州的最南海岸,这种向南的运动是明显的,而相应的向北返回则不太明显。秋季在新南威尔士州向南移动的带斑点的Drongos主要被限制在距海<15 km的沿海地区。建议Drongos在秋天在新南威尔士州向南移动是D.b的延伸。在昆士兰州南部和新南威尔士州北部沿海岸垂直下降并越冬的短尾act种群。

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