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damply [damp]

Pohnpei Starling

The Pohnpei Starling (Aplonis pelzelni), also known as Pohnpei Mountain Starling or Ponape Mountain Starling, is an extremely rare or possibly extinct bird from the family of starlings (Sturnidae). It is (or was) endemic to the island of Pohnpei (Federated States of Micronesia) in the Pacific Ocean. It was called "sie" (pronounced see-ah) by the Pohnpei islanders. It was named after the Austrian ornithologist August von Pelzeln (1825 - 1891).

Description

The Pohnpei Starling reached a size of 19 cm. It was generally dark with sooty brown upperparts. The head was darker and exhibit a black forehead and black lores. The wings, the rump, the uppertail coverts and the tail were paler and were showing a stronger brown colouring at the head. The underparts were washed olive brown. The bill and the feet were black. The iris was brown. The juveniles were looking similar to the adults except for the upperparts of there plumage which had exhibit a paler brown. Its call consists of a bell-like shrill see-ay.

Habitat

The Pohnpei Starling was native to dark damply mountain forests in altitudes above 425 m asl but it was also observed in plantages and in lower altitudes. The last specimen was shot in an altitude of 750 m asl.

Ecology and Diet

It was a non-migratory bird and it was defended its territory by pairs. It foraged diurnial and its diet consisted of flowers, berries and seeds of evergreen bushes and trees as well as insects and maggots. Reports that it has build its nest in tree holes are unconfirmed.

Threats and Extinction

The Pohnpei Starling was discovered by the Polish ethnographer John Stanislaw Kubary (1846 - 1896) and first described by German ornithologist Otto Finsch in 1876. The holotype which was deposited at the Godeffroy Museum in Hamburg, Germany for a while is now at the Museum Naturalis in Leiden, Netherlands. It seems that this bird was rather common at the beginning of the 1930s. 60 specimens were obtained during the Whitney South Seas Expedition led by William Coultas in 1930 and 1931. One specimen was shot by Lawrence P. Richards in 1948 who send the skin to the Bishop Museum in Honolulu, Hawaii. In 1956 ornithologist Joe T. Marshall was the last western scientist who saw this bird alive. Marshall shot two specimens and send the skins to the Smithsonian Institution in Washington. Afterwards this bird was lost. In 1973 or 1974 it was apparently sighted at the Nantolemal Point but this unconfirmed. After several unconfirmed reports by Pohnpei islanders there were surveys in 1976, 1977, and 1983 which were unfortunately failed. In 1990 it was classified as extinct by the IUCN until ornithologist William T. Buden obtained a dead female at July 4, 1995 which was shot by a native guide at a herpetological expedition during 1994. Therefor the IUCN has reclassified it as critically endangered in 2000. Nevertheless, this is currently the last liable evidence for that species.

The reasons for its vanishing remained unknown. Competition with other bird species and the bird hunting have played certainly an important role and as with many bird species on islands the clutches were plundered by rats. Habitat loss might have played a minor role because even if 37 percent of the highland forests were cleared between 1975 and 1995 a large part of its habitat is still remain.

References

  • Database entry includes justification for why this species is critically endangered

External links

Related Articles
IN AN ANTIQUE LAND NOVEMBER BRINGS A CERTAIN CLARITY TO THE NEW ENGLAND LANDSCAPE. THE SUN IS NOT YET QUITE SO LOW THAT IT OBSCURES THE SUBTLE FEATURES AT MIDDAY, AS IT WILL WHEN IT FALLS SO HEAVILY UPON THE EYE IN LATE DECEMBER. SNOW HAS NOT BLANKETED THE GROUND, AS IT WILL IN JANUARY. AND IT IS NOT SO BITTERLY, DAMPLY, COLD AS IT WILL BE IN MARCH. IT IS THE MONTH OF THE STONE WALL. NOT ONLY THE TREE LEAVES, BUT THE BLUEBERRY AND BRAMBLE LEAVES ARE OFF, AND NOTHING OBSCURES THE VIEW EXCEPT THE FEW SMALL OAKS AND BEECHES WHICH WILL HOLD THEIR LEAVES ALL WINTER, AND THE EVERGREENS, ALWAYS THE PINE AND HEMLOCK. THERE IS NO POINT IN WAITING FOR THEM; THEY WILL OUTLAST YOU. WE CLIMBED A MOUNTAIN IN WARWICK, NOT MUCH OF A FEAT, AND NOT MUCH OF A MOUNTAIN; IT IS ONLY CALLED THAT ON THE TOPOGRAPHICAL MAP. AN ORDINARY MAN WOULD CALL IT A HILL AND LEAVE IT AT THAT. IT IS STEEP ENOUGH, BUT LACKS REACH. AN OLD ROAD CARRIES UP TO THE TOP, ONE NOT TRAVELED FOR AT LEAST 50 YEARS, GUESSING BY THE SIZE OF THE WHITE PINE AND MAPLE TREES THAT HAVE GROWN UP DIRECTLY IN THE CENTER OF THE ROAD BETWEEN THE CART-TRACKS. A FEW MINUTES WITH A CHAINSAW AND A COUNTING OF TREE RINGS WOULD SETTLE IT, BUT WE DID NOT CLIMB IT FOR ROAD-SURVEYING, WE CLIMBED IT TO SURVEY A PROPERTY BOUNDED BY STONE WALLS. WE GOT A VIEW THAT WAS FREE. FROM THE TOP YOU COULD SEE TWO REAL MOUNTAINS, MONADNOCK TO THE NORTH, WACHUSETT TO THE SOUTHEAST. WE DID NOT BRING A SPY-GLASS IN ORDER TO SEE WACHUSETT UP CLOSE, WE CLIMBED TO SEE IT AT A DISTANCE. IT IS NOT REALLY OUR MOUNTAIN, EITHER LEGALLY OR PHILOSOPHICALLY. IT STILL BELONGS TO WHOEVER IT WAS WHO BUILT THE SUBSTANTIAL HOUSE ON THE TOP. IT IS A CURIOUS FLAT-TOPPED HILL, WITH CONSIDERABLE PHYSICAL EVIDENCE OF HAVING BEEN WELL-BURIED UNDER THE ICE ABOUT 12,000 YEARS AGO. IT IS NOT FLAT BECAUSE IT WAS SCRAPED OFF BY THE GLACIERS, IT IS FLAT BECAUSE, AT SOME POINT, IT WAS CARRYING THE OUTWASH OF A MASSIVE ICEFIELD. THE TOP HAS TWO TRUNCATED ESKERS, WHICH ARE OLD STREAMBEDS OF MELTWATER THAT ONCE FLOWED UNDERNEATH THE ICE. THE ESKERS STAND ABOVE THE GROUND AS THOUGH SOMEONE HAD BUILT A CELESTIAL STREETCAR LINE ON THE TOP OF THE HILL, SO MUCH DO THEY RESEMBLE RAILROAD BEDS ONLY LACKING THE TIES AND RAILS TO COMPLETE THE JOB. JUST TO THE NORTHWEST IS A FLAT OUTWASH PLAIN WITH A HANGING VALLEY IN THE MIDDLE OF IT, NARROWER TO THE NORTH, WIDER TO THE SOUTH. IT IS A PAMET, A RIVER VALLEY (WELL, REALLY, A CREEK VALLEY) SUBSEQUENTLY CUT OFF BY MORE SUBSTANTIAL MELTWATERS THAT DEFINED THE HILL, AND LEFT ALONE ON THE TOP OF THE FLATTISH MOUNTAIN. THIS SMALL VALLEY STILL COLLECTS WATER, AND MAKES AN ELEVATED SWAMP, SEVERAL HUNDRED FEET ABOVE ITS MODERN COUNTERPARTS, AND THEN THE WATER TUMBLES DOWN THE HILLSIDE, SEEKING THE SEA. THE HOUSE IS WHAT MAKES IT CLEAR YOU WOULD NOT OWN THE HILL EVEN IF YOU HAD A DEED TO IT. THE CELLAR HOLE IS STILL EMPTY AND CLEAN, WITHOUT SUBSTANTIAL TREES, ALTHOUGH A GREAT, DYING, MAPLE HAS GROWN UP DIRECTLY OUT OF THE CELLAR WAL

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