Showing posts with label Tytonidae. Show all posts
Showing posts with label Tytonidae. Show all posts

Thursday, 26 February 2015

The diet of breeding Grass Owls in Thailand.

Grass Owls are members of the Barn Owl family, Tytonidae, distinguished by their habit of roosting and nesting in tall grasses or other ground-cover plants, rather than trees. Until fairly recently all Grass Owls were thought to belong to a single species, but there are now two species recognised, the African Grass Owl, Tyto capensis, which is found across much of Africa, and the Eastern Grass Owl, Tyto longimembris, which is found in south China, Nepal, India, Myanmar, Southeast Asia, Indonesia, the Philippines, New Guinea, New Caledonia and Australia. The Eastern Grass Owl was first discovered in Thailand as recently as 2006, where a small colony was found nesting in a small area of marsh grassland called Nong Lom in Mae Jan District in Chiang Rai Province in the north of the country. 

In a paper published in the Raffles Bulletin of Zoology on 17 February 2015, Akalak Kunsorn of the Department of Biology at Chiang Mai University and the Environmental Ornithology Research Unit at Mahidol University, Siriwadee Chomdej of the Department of Biology and the Materials Science Research Center at Chiang Mai University, Narit Sitasuwan, Prasit Wangpakapattawong and Chatmongkon Suwannapoom, also of the Department of Biology at Chiang Mai University and Brett Sandercock of the Division of Biology at Kansas State University, describe the results of a study of the diet of the Grass Owls of Nom Long carried out by examining Owl pellets from the site during the breeding season.

Eastern Grass Owl, Tyto longimembris, in flight. Rob Hutchinson/The Owl Pages.

Birds lack teeth with which to process food like mammals, instead grinding it up in a muscular gizzard before it is passed to the stomach. As flying animals they are obliged to keep their weight to a minimum, and therefore need to dispose of inedible parts of their prey as quickly as possible, and so both Owls and Raptors regurgitate pellets comprising indigestible items such as fur and bone without passing them through the stomach and gut.

As well as Grass Owls the Nom Long site is also home to four species of Harriers; the Eastern Marsh Harrier, Circus spilonotus, the Pied Harrier, Circus melanoleucos, the Hen Harrier, Circus cyaneus and the Western Marsh Harrier, Circus aeruginosus. Grass Owl pellets tend to be larger and more elongate than Harrier pellets, but to avoid confusion Kunsorn et al. collected pellets only from the nests of Owls.

Kunsorn et al. carried out DNA tests on bones recovered from Owl pellets at Nom Long, in order to determine identify animals being consumed by the Owls. They were able to identify three species of Rodent by this method, the Black Rat, Rattus rattus, the Asian House Mouse, Mus musculus, and the Ricefield Mouse, Mus caroli. In addition wings and tails of Barn Swallows, Hirundo rustica, were also found in the Owl nests, suggesting that these Birds were also being consumed.

Pellets of the Eastern Grass Owl, Tyto longimembris, collected from nests at Nom Long. Kunsorn et al. (2015).

The diet of Eastern Grass Owls has previously been studied in southern Taiwan, where they were found to be consuming Lesser Rice-field Rats, Rattus losea, Ricefield Mice, Mus caroli, Formosan Blind Moles, Mogera insularis, House Shrews, Suncus murimus, Shrews Crocidura spp. and juvenile Formosan Hares, Lepus sinensis, as well as small Birds. This is a far larger range of prey than consumed at the Thai site, which Kunsorn et al. attribute to the more varied hunting grounds available to the Taiwan Owls. Nom Long is largely surrounded by grasslands and wetlands, with some Orange orchard about a kilometre away to the northwest, while the Taiwan site was within easy reach of shrubland, Rice paddies, Bamboo forest, Sugarcane fields, Mango orchards and Human settlements.

See also…

Owls (Stringiformes) first appear in the fossil record in the Palaeocene and become quite common in the fossil record in the Eocene and Oligocene of Eurasia and North America. The modern Owl families Strigidae and Tytonidae first appear in the fossil record in the...


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Tuesday, 26 August 2014

Fossil Owls from the Early Pliocene of Langebaanweg, South Africa.

Owls (Stringiformes) first appear in the fossil record in the Palaeocene and become quite common in the fossil record in the Eocene and Oligocene of Eurasia and North America. The modern Owl families Strigidae and Tytonidae first appear in the fossil record in the Miocene and Eocene respectively. Like all Birds, Owls have rather delicate, lightweight skeletons well suited to flying, but with rather poor preservational potential. However the leg bones of Owls are somewhat more robust, being used to strike an subdue prey, and most fossil Owls are known entirely from their legs. 

In a paper published in the journal Acta Palaeontologica Polonica on 13 June 2014 Marco Pavia of the Dipartimento di Scienze della Terra at the Università degli Studi di Torino, Albrecht Manegold of the Senckenberg Forschungsinstitut und Naturmuseum and the Staatliches Museum für Naturkunde Karlsruhe, and Pippa Haarhoff of the West Coast Fossil Park, describe a series of Owl remains from the Early Pliocene Upper Varswater Formation at Langebaanweg in Western Cape, South Africa. The Langebaanweg deposits have produced over 90 species of Birds in 35 families, making them the most important pre-Pleistocene deposits for the study of Avian faunas in Africa and one of the most important in the world. They are also important in that they are a mixture of coastal and near-coastal river deposits, whereas most locations with rich Avian faunas are karsts (limestone cave systems), which tend to produce rather different assemblages.

The first fossils described are placed within the Barn Owl genus Tyto, and placed in a new species, richae, named in honour of Patricia Vickers-Rich, who carried out the first work on the Avian fauna of Langebaanweg in 1980, and who has made significant contributions to the study of fossil Birds in Africa. The new species is described from the distal end of a right tarsometatarsus (in anatomy the distal end of a bone is the end furthest from the head), a complete left coracoid, the distal end of a left ulna, the distal ends of two left tibiotarsi and the distal end of a right tibiotarsus.

Tyto richae from the Upper Varswater Formation at Langebaanweg, South Africa; Early Pliocene. (A) Left coracoid in dorsal (A1), lateral (A2), medial (A3), and ventral (A4) views. (B) Left ulna in dorsal (B1), caudal (B2), ventral (B3), and cranial (B4) views. (C) Left tibiotarsus in cranial (C1), lateral (C2), caudal (C3), medial (C4), and distal (C5) views. (D) Left tibiotarsus in cranial (D1), lateral (D2), caudal (D3), medial (D4), and distal (D5) views. (E) Right tarsometatarsus in dorsal (E1), lateral (E2), plantar (E3), medial (E4), proximal (E5), and distal (E6) views. Pavia et al. (2014).

Barn Owls first appear in the fossil record of Europe in the Middle Miocene, with most known fossil species from Europe, the Mediterranean and North Africa (including several species from Mediterranean islands with very restricted distributions). The modern Barn Owl, Tyto alba first appears in the fossil record in Morocco in the latest Pliocene or earliest Pleistocene, while the African Grass Owl, Tyto capensis, first appears in the latest Pleistocene in Tanzania. An as yet undescribed species of Tyto is also known from the Early Pliocene of Ethiopia, and two further undescribed species from the early Pleistocene of Kromdraai and Swartkrans in South Africa.

The second species described is placed in the Little Owl genus Athene and given the specific name inexpectata, meaning ‘unexpected’. To date the earliest known Little Owl is a specimen from Bulgaria from the Late Pliocene, which has not been assigned to a specific species (a claimed specimen from the Miocene of Hungary is not generally accepted); and the closest relatives in the fossil record are thought to be fossils from the Pliocene of Idaho, Kansas and Nebraska. The modern Little Owl, Athene noctua first appears in the Early Pleistocene in Italy, and several apparently endemic species are known from Mediterranean islands in the Pleistocene. As such Athene inexpecta is both the oldest member of the genus, and the first recorded specimen from Africa, raising questions about our understanding of the history of the genus. This is not entirely a surprise, as the Langebaanweg deposits have produced other fossils with apparent close affinities to Northern Hemisphere faunas, notably the Bear Agriotherium africanum and the Wolverine Plesiogulo monspessulanus. 

Athene inexpectata from the Upper Varswater Formation at Langebaanweg, South Africa; Early Pliocene , (A, C–F, H) and Athene noctua, Recent (B). (A) Left tibiotarsus in cranial (A1), lateral (A2), caudal (A3), medial (A4), and distal (A5) views. (C) Left scapula in medial (C1), cranial (C2) and lateral (C3) views. (D) Right in dorsal (D1), caudal (D2), ventral (D3) and cranial (D4) views. (E) Right tibiotarsus in cranial (E1), lateral (E2), caudal (E3), medial (E4), and proximal (E5) views. (F) Right tarsometatarsus in dorsal (F1), lateral (F2), plantar (F3), medial (F4), proximal (F5), and distal (F6) views. (H) Right humerus in cranial (H1), dorsal (H2) caudal (H3), ventral (H4), and distal (H5) views. (B) Reversed right tibiotarsus in cranial view (B1), left tarsometatarsus in dorsal view (B2). Pavia et al. (2014).

Athene noctua is described from two complete right tarsometatarsi, the cranial part of a sternum (the cranial part being the part closest to the cranium), the cranial end of a right scapula, the distal half of a right humerus, the distal half of a right ulna, an almost complete left tibiotarsus, lacking the distal end, the proximal end of a right tibiotarsus (the proximal end being closest to the body), the distal end of a right tibiotarsus, and the distal half of a left tarsometatarsus.

Thirdly the distal end of a left tibiotarsus is assigned to the genus Bubo (Eagle Owls), but not assigned to a specific species, the material being too fragmentary. The oldest members of this genus previously described have been Pleistocene in age, though this includes specimens from Laetoli and Olduvai in Tanzania.

Bubo sp., left tibiotarsus in cranial view, from the Upper Varswater Formation at Langebaanweg, South Africa; Early Pliocene. Pavia et al. (2014).

Fourthly the shaft of a left tibiotarsus and distal end of a right tibiotarsus assigned to the genus Asio (Long-eared Owls), but again not assigned to a specific genus. Asio first appears in the fossil record in the Early Miocene of Germany, and the genus appears to have become widespread by the Plio-Pleistocene, with several species recorded from Europe and North America, and as well as Laetoli in Africa.

Asio sp., right tibiotarsus in cranial (A1), lateral (A2), caudal (A3), medial (A4), and distal (A5) views, from the Upper Varswater Formation at Langebaanweg, South Africa; Early Pliocene. Pavia et al. (2014).

Finally the distal end of a left tibiotarsus is recorded and assigned to the Strigidae (the family which includes all modern Owls except Barn Owls), but not to any specific genus or species.

Unassigned left tibiotarsus in cranial view from the Upper Varswater Formation at Langebaanweg, South Africa; Early Pliocene. Pavia et al. (2014).

See also…


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The La Brea Tar Pits are located in what is now central Los Angeles, California. They are essentially oil deposits identical to those worked by oil drills in other parts of the world, but exposed at the surface. When oil deposits are exposed in this way the lighter fractions (crude oil is made up of a mixture of different oils, known as 'fractions' due to the process used to separate them, fractional distillation) such as petroleum evaporate off, leaving the heavier fractions, known as tar, or...




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