Bristle-thighed Curlew Numenius tahitiensis Scientific name definitions

Jeffrey S. Marks, T. Lee Tibbitts, Robert E. Gill, and Brian J. McCaffery
Version: 1.0 — Published March 4, 2020
Text last updated January 1, 2002

Movements and Migration

Migration Overview

Long-distance transoceanic migrant between breeding grounds in w. Alaska and wintering grounds in central and s. Oceania. Birds migrating between southernmost wintering islands and Alaska (>8,500 km) possibly use stopover sites in Central Pacific (Marks and Redmond Marks and Redmond 1994a, Marks and Redmond 1994b). Few coastal spring records in Alaska indicate direct flight most years to breeding grounds (Gill and Handel 1981a). Young birds typically remain on wintering grounds until 3–4 yr old before making first northward migration (Marks and Redmond Marks and Redmond 1996).

Timing and Routes of Migration

Follows Central Pacific Flyway. Exact routes unknown. Migration largely oceanic, presumably in direct line between wintering islands and breeding grounds, with birds seldom landing in Americas outside of Alaska (but see below).

From 1988 to 2002, 7 birds color-banded on southern breeding grounds in Nulato Hills seen in Northwestern Hawaiian Is. (JSM, S. Bailey, B. Casler, and J. Gilardi pers. comm.). Similarly, 7 birds color-banded in Northwestern Hawaiian Is. seen in Nulato Hills (BJM). Four individuals marked in Alaska seen in winter 1992 at Palmyra Atoll, 2,000 km south of Hawaiian Is. (E. Flint pers. comm.); 2 were from Neva Creek on Seward Peninsula, but breeding origin of other 2 not determined. Thus, birds that winter in Northwestern Hawaiian Is. seem to come from southern breeding population in Nulato Hills, and those that breed on Seward Peninsula apparently winter south of Hawaiian Is., suggesting leapfrog migration. Birds from the 2 breeding populations must overlap in distribution somewhere in Central Pacific, but data lacking. Some movement among Hawaiian Is., especially during southward migration by adults and by nonbreeding 2-yr-olds in late summer (see below), but such movements poorly understood.

Spring

Peak in numbers Apr–May on Christmas I. (Gallagher 1960) and at several sites in Northwestern Hawaiian Is. (Ely and Clapp 1973, Amerson et al. 1974, Clapp and Wirtz Clapp and Wirtz II 1975), but birds unmarked. Northward departure of marked birds monitored closely at Laysan I. in 1991 (Marks and Redmond 1994b). The 16 observed departures occurred 1–13 May, with most (75% of departures, 91% of individuals) occurring 1–9 May. Observations at French Frigate Shoals, Laysan I., and Midway Atoll in other years also support notion that departure from Northwestern Hawaiian Is. typically occurs during first 2 wk of May (JSM).

Most northbound migrants overfly Aleutian Is. to arrive at breeding areas in first 3 wk of May. At Mountain Village, AK, at southern end of breeding range, first birds seen 9–18 May from 1944 to 1947 (Kyllingstad 1987). More recently, first arrivals 3–6 May 1988–1991 in Nulato Hills 32 km north of Mountain Village and 8–18 May 1990–1992 at Neva Creek, suggesting earlier arrival for southern population. First spring birds in Nulato Hills probably passage migrants rather than local breeders. Over 3 yr at 1 site, first returning marked breeders arrived average of 4 d after species first detected (range 0–8 d; BJM). Arrival of returning breeders highly synchronous. Last returning breeders arrived average of 9 d after species first detected (range 5–16 d), but only 5 d (range 2–8) after first known breeders (BJM). At Neva Creek, all resident breeders present 12–14 d after first arrival (REG, TLT). Records elsewhere in w. Alaska generally consistent with arrival dates on breeding grounds, but nowhere reported in large enough numbers to suggest regular stopover; e.g., casual (1–4 individuals/sighting) mid- to late May on Aleutian Is., including Attu I., Amchitka I., Shemya I., Buldir I., and Adak I. (Gibson 1981, Byrd and Day 1986, Tobish and Isleib 1992a, UAM unpubl.); small numbers almost every year on Pribilof Is. in mid-May (UAM unpubl.), earliest 5 May 2001 (P. Tomkovich pers. comm.); a few records 9–18 May from Izembek Lagoon on north side of Alaska Peninsula (UAM unpubl., TLT). Recorded Yukon Delta most years, but numbers irregular (mean arrival 14 May ± 7 d SD [range 3–21 May 1985–1996]; C. Ely unpubl.).

North of Yukon Delta, recorded at St. Michael, 24 May 1880 (Nelson 1887a), at Golovin, 13 May 1981 (Kessel 1989), and in Nome area, 23 May 1905 and 28 May 1922 (Bent 1929). Interesting “shortstop” by migrants in 1992 occurred at Alaska Peninsula estuaries where species previously unrecorded, including earliest Alaska record, a bird at Port Heiden 24 Apr (Tobish and Isleib 1992a), and several groups of 1–6 seen 2–23 May (UAM unpubl., REG); occurrence apparently related to late spring throughout w. Alaska and near-record late snow on northern breeding area that year (REG). Elsewhere in Alaska, small numbers regularly recorded early May at n. Gulf of Alaska (Middleton I., Kachemak Bay), 900–1,100 km east of breeding range (West 1993a, UAM unpubl.).

Before 1998, only one verified record from Pacific Northwest, a bird collected on Vancouver I., British Columbia, 31 May 1969 (Richardson 1970). Six other records from Pacific Northwest, 3 each from spring and fall, possibly valid (Paulson 1993, Mlodinow et al. 1999). Unprecedented “fallout” of ≥13 birds (perhaps up to 25) along Pacific Coast from Point Reyes, CA, to Tatoosh I., WA, 6–25 May 1998, coincided with extreme weather over Pacific Ocean that presumably pushed birds far east of normal migration path (Mlodinow et al. 1999).

Fall

Stages from Jun to Aug along coastal Yukon Delta (Handel and Dau 1988); small groups occur Jul-Aug along coastal Seward Peninsula (Kessel 1989). Best information from study conducted 1975–1979 at central Yukon Delta (Handel and Dau 1988). Birds typically arrive in 2 or 3 peaks mid-Jun to early Aug. First arrivals probably early failed breeders or nonbreeders followed by late failed breeders and then successful breeders and juveniles; first juveniles seen 26 Jul. At Neva Creek (1988–1992), failed nesters left study area in mid-Jun, successful nesters in late Jul, and most juveniles during first week of Aug (REG, TLT). Latest departures from Yukon Delta typically 8–31 Aug (Handel and Dau 1988). Latest record on Yukon Delta 10 Sep (REG, BJM); latest Alaska record 5 Oct on Middleton I. (UAM unpubl.).

Use of Seward Peninsula during postbreeding period poorly known; small numbers of Bristle-thighed Curlews recorded along northern and southern coasts of peninsula in Jul and Aug, including Safety Sound, 3 birds, 22 Jun 1970; Cape Espenberg, 1 and 3 birds, 30 Jun 1976 and 3 Jul 1973, respectively; Lopp Lagoon, 1 and 11 birds, 3 Jul 1974 and 12 Jul 1974, respectively (Kessel 1989). Latest specimen a juvenile male from Safety Sound, 1 Sep 1911 (U.S. Natl. Mus. 2339810; Kessel 1989). Farther north, C. Townsend shot juvenile at Kobuk River mouth near Kotzebue 26 Aug 1885 (Ridgway 1919), and R. Beck collected “quite a series” of birds near Nome in Aug 1911 (Bent 1929). Nine curlews seen 19 Aug 1988 near Cape Krusenstern, AK (UAM unpubl.), almost certainly juveniles, but ages unknown.

Limited information from 4 adults (2 successful nesters, 2 failed) radio-tagged on breeding grounds in 1989 suggests length of stay on Yukon Delta staging area 2–3 wk (TLT, REG, BJM). Nushagak Peninsula area, n. Bristol Bay, only other site where curlews known to occur in late summer (Murie 1959, T. Pogson unpubl.), but extent and duration unknown. Paucity of Jul–Sep records elsewhere in Alaska (e.g., none on Aleutian Is.; occasional on Alaska Peninsula, Pribilof Is., Kodiak I., Nunivak I., Kachemak Bay) indicates migration to wintering islands largely direct from w. Alaska (UAM unpubl., R. MacIntosh unpubl., REG, BJM, TLT).

Based on specimens, Stickney (Stickney 1943) posited that southbound birds arrive in Oceania from late Jul to early Aug. Presumed migratory influxes noted Jul–Sep in Northwestern Hawaiian Is. (Woodward 1972b, Ely and Clapp 1973, Clapp and Wirtz Clapp and Wirtz II 1975) and Sep–Oct in Line Is. (Kirby 1925, Gallagher 1960) and Samoa (Muse and Muse 1982). These and other reports of southbound “arrivals” based on unmarked birds of unknown age. Arrival of migrants on wintering grounds best known from study at Laysan I., Northwestern Hawaiian Is., 1988–1991 (Marks and Redmond 1994b). Adults arrived in 2 peaks, first 18–24 Jul and second 16–23 Aug; all returning marked adults arrived by first week of Sep. Juveniles arrived mid-Aug to early Sep, earliest 19 Aug. Several arriving flocks consisted entirely of juveniles (JSM), and arrival dates of adults versus juveniles strongly suggest that juveniles undertake southward migration unaccompanied by adults (contra Johnsgard 1981, Hayman et al. 1986; see Marks and Redmond 1994b).

Inter-island Movements

Amadon (Amadon 1953b) speculated that Bristle-thighed Curlews stopped in Hawaiian Is. and eventually wintered farther south. Based on counts of unmarked birds in spring and fall, Amadon's view supported for Northwestern Hawaiian Is. (Amerson 1971, Woodward 1972b, Ely and Clapp 1973, Amerson et al. 1974, Clapp and Wirtz Clapp and Wirtz II 1975) and echoed by Handel and Dau (Handel and Dau 1988). Studies of marked birds, however, show that Northwestern Hawaiian Is. are migratory terminus rather than stopover, and that most curlews wintering farther south overfly Hawaiian Is. in spring and fall (Marks and Redmond 1994b). High counts of curlews in Northwestern Hawaiian Is. in spring and fall result from flocking of local birds at traditional roost sites rather than influxes of transients (see below). Bristle-thighed Curlew banded on Lisianski I. 25 Sep 1967 (Clapp and Wirtz Clapp and Wirtz II 1975) and found in Marshall Is. in 1981 (Dunning 1988a) is only record of bird from Northwestern Hawaiian Is. occurring in tropical Pacific outside Hawaiian Is.

Three marked adults from Laysan I. seen on main Hawaiian Is. during southward migration, including bird on O‘ahu 8 Aug 1990 that reoriented to Laysan I. and wintered there (JSM). Adults highly faithful to wintering islands (Marks and Redmond 1996), but numerous records of marked birds moving among islands in Northwestern chain, especially 2-yr-olds (i.e., 24–27 mo old) that move in late summer at same time adults are migrating south (JSM).

Migratory Behavior

Data from Laysan I. in spring 1991 (Marks and Redmond 1994b). No pattern in daily timing of departures, with half of flocks leaving before 14:00 and half after (n = 16 departures). Earliest departure at 09:10 on 7 May and latest at 17:30 on 6 May; no significant relationship between daily timing and date of departure. Unlike in other shorebirds (Lank 1989, Alerstam et al. 1990, Piersma et al. 1990b), diurnal timing of Bristle-thighed Curlew departures unrelated to tidal cycle or sunset.

Just prior to departing, typically stopped at staging site at north end of Laysan I., a spot not used by curlews at other times of year (JSM). Only 4 of 16 departing flocks failed to stop at staging site; these flocks among latest to depart island (9–13 May). Other 12 flocks stopped at staging site for 7–75 min (mean 36 min). Staging birds typically stood quietly in loose flock, facing north. Departures always preceded by increased vocal activity; flocks circled above island as they gained altitude, with birds uttering chiu-eet and klee calls incessantly (see Sounds and Vocal Behavior: Vocalizations, below). All departing flocks flew to north or north-northwest in loose cluster and then formed Vs or echelons, continuing to ascend before disappearing from view.

Some members of departing flocks (5–62%) returned to island in 12 of 16 departures. Nine of these returning flocks scrutinized for color-bands; 58–100% of birds individually marked, and each flock had 1- and 2-yr-olds that were noticeably thinner than adults. These subadults made up large proportion of birds that returned to island after departures. Mean size of flocks 14.1 at first departure (range 1–31) and 10.7 for birds disappearing from view (range 1–22). Mean flock size experienced by average bird (Ýg2/Ýg, where g = flock size) 20.5 and 16.2 for departing and disappearing flocks, respectively. Sizes of departing flocks substantially smaller than in other shorebird species (Alerstam et al. 1990, Blomert et al. 1990), despite theoretical benefits of large flock size at departure (Piersma et al. 1990b).

Upon arrival at Laysan I. from Alaska, incoming birds highly vocal, being audible from >1 km as flocks descend to island (JSM). First landing by adults and juveniles typically occurs at traditional roosting site at south end of island, where curlews congregate year-round (although numbers highest in spring and fall; JSM, Marks and Redmond 1994b). Arriving birds invariably drink seawater from tide pools at roosting site within minutes of landing (JSM).

Migrating Bristle-thighed Curlews presumably do not land on water and thus fly night and day. Altitude and flight speed during migration unknown. Based on radar studies, shorebirds fly at altitudes up to 6 km and at ground speeds >70 km/h (Williams and Williams Williams and Williams 1988, Williams and Williams 1990). Birds flying from Laysan I. at 75 km/h (Castro and Myers 1989) would reach Alaska in 53 h.

Control and Physiology of Migration

Clearly a calendar migrant in spring, based on narrow time window of departure from Laysan I. and arrival in Alaska. On Laysan I., color-banded curlew with broken wing traversed entire island on foot (>3 km) and staged with volant curlews during peak of northward migration, later returning to home range (Marks 1995). This injury was ≥1.5 yr old, yet bird deposited fat and “migrated,” indicating that spring migration controlled by endogenous circannual clock (Marks 1995). Marked adult with leg injury that affected foraging rate and slowed molt made ≥3 migratory flights between Laysan I. and Alaska (Marks and Underhill 1994).

Gains mass steadily throughout winter following completion of molt in late autumn (Marks 1993), unlike other shorebirds that maintain low mass in winter and fatten rapidly in spring (e.g., Pienkowski et al. 1979, Summers and Waltner 1979). Presumed gradual accumulation of fat thought to result from relatively unproductive foraging conditions on oceanic islands that preclude rapid fattening in spring (Marks 1993). Six adults collected at Laysan I. and Midway Atoll during peak of spring migration had lipid indices (fat mass/body mass) ranging from 36.3 to 47.0% (mean 42.5%), among highest fat loads ever measured in shorebirds (Marks and Redmond 1994b, Piersma and Gill 1998). Lipid indices of 7 curlews collected mid-Jul 1973 on Eniwetok Atoll ranged from 3.3 to 10.8% (Johnson and Morton 1976); birds appeared to be subadults based on molt (Johnson 1977a, Marks 1993) and thus were in nonmigratory state.

Measurements from the 6 birds collected in Northwestern Hawaiian Is. indicate that Bristle-thighed Curlews reduce size of gizzard, intestines, and liver in preparation for transoceanic flights (see Piersma 1998, Piersma and Gill 1998). Stomachs of these birds empty, consistent with observations that Bristle-thighed Curlews forgo foraging for at least 1 d before migratory departure (Marks and Redmond 1994b, JSM).

Based on lipid indices of these 6 birds, flight-range estimates of 3,000–10,000 km (Marks and Redmond 1994b). Lower estimates clearly wrong, given that curlews were about to fly 4,000 km over ocean, whereas upper estimates perhaps unrealistically far. However, recent evidence that Bar-tailed Godwits capable of flying 11,000 km nonstop (Piersma and Gill 1998) raises possibility that Bristle-thighed Curlews fly nonstop to southern end of winter range >8,500 km from Alaska. Likely that assistance from winds aloft important factor in transoceanic migration (Piersma and Sant 1992, Marks and Redmond 1994b).

Recommended Citation

Marks, J. S., T. L. Tibbitts, R. E. Gill, and B. J. McCaffery (2020). Bristle-thighed Curlew (Numenius tahitiensis), version 1.0. In Birds of the World (A. F. Poole and F. B. Gill, Editors). Cornell Lab of Ornithology, Ithaca, NY, USA. https://doi.org/10.2173/bow.brtcur.01
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