Among the most widespread seabirds in the world, shearwaters of the genus Puffinus are also some of the deepest diving members of the Procellariiformes. Maximum diving depths are known for several Puffinus species, but dive depths or diving behaviour have never been recorded for great shearwaters (P. gravis), the largest member of this genus. This study reports the first high sampling rate (2 s) of depth and diving behaviour for Puffinus shearwaters.
Time-depth recorders (TDRs) were deployed on two female great shearwaters nesting on Inaccessible Island in the South Atlantic Ocean, recording 10 consecutive days of diving activity. Remote sensing imagery and movement patterns of 8 males tracked by satellite telemetry over the same period were used to identify probable foraging areas used by TDR-equipped females. The deepest and longest dive was to 18.9 m and lasted 40 s, but most (>50%) dives were <2 m deep. Diving was most frequent near dawn and dusk, with <0.5% of dives occurring at night. The two individuals foraged in contrasting oceanographic conditions, one in cold (8 to 10°C) water of the Sub-Antarctic Front, likely 1000 km south of the breeding colony, and the other in warmer (10 to 16°C) water of the Sub-tropical Frontal Zone, at the same latitude as the colony, possibly on the Patagonian Shelf, 4000 km away. The cold water bird spent fewer days commuting, conducted four times as many dives as the warm water bird, dived deeper on average, and had a greater proportion of bottom time during dives.
General patterns of diving activity were consistent with those of other shearwaters foraging in cold and warm water habitats. Great shearwaters are likely adapted to forage in a wide range of oceanographic conditions, foraging mostly with shallow dives but capable of deep diving.
Citation: Ronconi RA, Ryan PG, Ropert-Coudert Y (2010) Diving of Great Shearwaters (Puffinus gravis) in Cold and Warm Water Regions of the South Atlantic Ocean. PLoS ONE 5(11): e15508. https://doi.org/10.1371/journal.pone.0015508
Editor: Hans-Ulrich Peter, Institute of Ecology, Germany
Received: August 16, 2010; Accepted: October 5, 2010; Published: November 30, 2010
Copyright: © 2010 Ronconi et al. This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
Funding: Financial support was provided by South African National Antarctic Programme, the European Commission's EDF-9 through the South Atlantic Invasive Species project, BirdLife International, the United States Fish and Wildlife Service, and the University of Cape Town. R.A.R. was supported by the Killam Trust, Dalhousie University. The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.
Competing interests: The authors have declared that no competing interests exist.
Shearwaters (Puffinus spp.) are among the most widespread seabirds throughout much of the world's oceans, adapted for foot and wing-propelled diving , , , with several species undertaking trans-equatorial migrations , . Although many procellariiforms perform shallow (1–5 m) dives to capture prey , , studies using depth recorders have revealed the relatively deep (>50 m) diving abilities of Puffinus shearwaters. These shearwaters exhibit maximum diving depths that are allometrically scaled and comparable in depth to those of penguins and alcids . However, maximum diving depths have been recorded for only 5 of the 20 or so species of Puffinus using capillary depth gauges , , , . More recently, dives of sooty shearwater (P. griseus) have been recorded using archival tags sampling every 24 to 32 seconds , . The use of high sampling rate time-depth-recorders (TDRs), which trace individual dives and record time spent at various depths, have been used on only one Balearic shearwater (P. mauretanicus) sampling depth every 4 seconds . Thus, very little is known about the diving ecology of this genus.
We report the first deployments of TDRs on great shearwaters (P. gravis), sampling depth and temperature during foraging trips in the early incubation period. The great shearwater is the largest Puffinus  and nests almost exclusively on islands in the Tristan da Cunha group and Gough Island in the central South Atlantic Ocean , . While breeding, they occupy a wide range of marine habitats from Polar Frontal zones to neritic waters of coastal South America and Africa . Ocean temperatures, recorded during dives, were compared to remote sensing data and movement patterns of other shearwaters tracked by satellite telemetry, in order to estimate the likely foraging ranges of the TDR-equipped birds. The high sampling rate (2 s) used in our study allowed us to investigate of maximum dive depths, dive frequency and dive profiles in relation to diel cycles while foraging in two contrasting oceanographic regions.
Access to the study colony and work on shearwaters was granted full permission by the Tristan da Cunha government. While the Tristan government does not require animal ethics approval to conduct work on animals, we adopted tagging protocols used by R.A.R. on great shearwaters in Canadian waters and approved by the Institutional Animal Use and Care Committee, University of North Carolina Wilmington (certificate #2005-003 and #2007-007). Banding permits were issued by the Canadian Wildlife Service (permit #10480 S) with special permission granted to band birds outside of North America.
Data collection and analyses
Breeding adult great shearwaters were accessed from nesting burrows on Inaccessible Island (37°18′S, 12°40′W; Fig. 1), which supports an estimated breeding population of ∼2 million pairs . Devices were deployed on four female shearwaters on 7 November 2009 within one day of egg laying to record the diving behaviour during the first post-laying foraging trip. TDRs (G5; Cefas Technology Limited, UK) were attached to the central tail feathers with waterproof Tesa tape and two plastic cable-ties. Each device weighed ∼5 g (4 g device and ∼1 g of attachment materials), roughly 0.6% of the shearwaters' body mass at the time of deployment. To maximize data collection with the data storage capacity of the device, TDRs were programmed to begin recording at 05:00 GMT (local time) on the day following attachment, and continuously recorded pressure (depth) every 2 sec and temperature every 3 sec, yielding ∼10 d of data. The resolution of the depth sensor was <0.04 m and the absolute temperature accuracy of the thermistor was ±0.1°C. Burrows were checked every second day until females returned from their foraging trip. Devices were recovered from three individuals, but files were corrupted on one, so data were only available from two birds. The final bird had not returned to relieve its partner when we left the island, 25 days after deployment. In total, 48 burrows were monitored (4 study, 44 control) of which 22 (45%) failed due to predation  or abandonment, and in 12 of the 44 control burrows (27%) females had also not returned by the final nest check, 1 Dec 2009 (17 to 23 days after laying).
A. Sea-surface temperature map (8-day averaged Modis Aqua data) during the TDR deployment period, 9–16 November, 2009. Ellipses indicate probable foraging ranges, based on TDR temperature profiles (Table 3), of birds A and B. B. Movements of 8 male Great Shearwaters tracked by satellite telemetry during the first nine days following their initial incubation shift on Inaccessible Island. Tags were deployed on 21 November, 2009, and departure dates ranged from 22 Nov to 07 Dec. Duty cycled tags transmitted every second day, and dots represents averaged daily locations for odd numbered days one through seven (•) and on day nine (○).
The TDR deployments occurred simultaneously during a larger study using satellite telemetry (PTT - Platform Terminal Transmitters) to track the movements of great shearwaters. A subset of these data was used to provide context for the likely foraging ranges of TDR-equipped birds. Eight PTTs (32 g Kiwisat 101, Sirtrack, Havelock North, NZ; ∼3–4% of shearwater body mass) were deployed on male great shearwaters, 21 Nov 2009, during their first incubation shift. Tags were duty cycled to turn on for 6 hrs at 10:00 UTC every second day. Foraging ranges were evaluated from the first 9 days once each male had departed the colony after their first incubation shift, which provides the most comparable data to the 10-d TDR recordings. Sea-surface temperature (SST) data were integrated with tracking data using Satellite Tracking and Analysis Tools (STAT ). Using positions with location class ≥0 (estimated accuracy typically within 4 km ), we calculated a single averaged location and SST for each day for each bird. Distance of each location to the colony was measured using ArcGIS 9.3 (ESRI, Redlands, CA, U.S.A.).
Downloaded TDR data were analyzed using IGOR Pro (Wavemetrics Inc., USA, 2008, Version 6.04). Data were corrected for surface drift and a number of parameters were automatically extracted for each dive: time of start and end of dives, maximum dive depth (m), total dive and post-dive duration (s), descent, bottom and ascent phases duration (s), and the number of undulations in the dive profiles (s). A dive started and ended when consecutive depth readings became greater and smaller than 0.5 m, respectively. The start and end of bottom phases were defined as the first and last time in a dive when the rate of change of depth became <0.25 m.s−1 .
Sunrise and sunset times (civil dawn/dusk) were used from two locations to evaluate diel patterns in foraging: Inaccessible Island and the Patagonia shelf region (37°S, 55°W). All breeding great shearwaters tracked by satellite tags from Inaccessible Island during the same period foraged between these two areas (Fig. 1). We estimated the likely general foraging locations by comparing temperature data recorded by the TDRs (using the minimum temperature measured within a few minutes of a dive) with sea surface temperature (SST) maps during the deployment period (Fig. 1; 8-day binned map from 9–16 Nov. 2009; Modis Aqua, http://oceancolor.gsfc.nasa.gov/ftp.html). Oceanographic zones were broadly defined focusing on surface temperatures in the central South Atlantic region : Polar Front (2–4°C), Sub-Antarctic Frontal Zone (5–9°C), and Sub-tropical Frontal Zone (10–17°C).
All statistics were analyzed with SPSS 15.0. T-tests were used to compare dive parameters between individuals and Analysis of Variance (ANOVA) was used to compare dive and temperature parameters among days for individual birds.
Tags were recovered from two birds after 17 d (bird A) and 22 d (bird B) foraging trips. Pre- and post-trip masses were 770/900 g and 810/975 g for birds A and B, respectively, averaging a daily mass gain of 7.5 and 7.6 g⋅d−1. Non-instrumented females, for which departure and return dates were recorded (n = 10), had mean trip durations of 18.8 d (range 16–22), mean post-trip mass of 929 g (845–975), and average daily mass gains of 8.7 g⋅d−1 (6.1–13.8). During the first 10 days of foraging, we recorded a total of 930 dives, with bird A performing nearly four times as many dives (n = 739) as bird B (n = 191). The deepest dive was to 18.9 m, and this was also the longest dive, lasting 40 s. It was made by bird A, which also exhibited greater average maximum dive depths (t989 = 2.53, p = 0.012) and durations (t989 = 3.01, p = 0.003) than bird B (Table 1). Most dives were shallow (>50% of dives were <2 m deep for both individuals; Table 1), but bird A performed many more dives deeper than 10 m (nearly 10%), compared to bird B (which only dived >10 m once; max. 10.9 m).
The measurement of bottom phase duration allowed for simple classification and comparison of dives which contained a bottom phase (BP) and those that did not (hereafter V-shaped dives; Table 2). Most dives (67.7% overall) were V-shaped and significantly shallower than BP dives for both bird A (2.0 vs. 5.8 m; t737 = 14.9, p<0.001) and bird B (2.4 vs. 3.3 m; t189 = 2.81, p = 0.005). During BP dives, both birds spent a similar proportion of the dive time in the bottom phase (42 and 39%), but the overall dive duration and maximum depth was greater for bird A (t301>3.69, p<0.001). This suggests that bird A spent more time pursuing prey at depth; the longest bottom phase was 24 s of a 28 s dive. During BP dives, there were no significant differences between individuals in either decent rates (t301 = 0.67, p = 0.505) or ascent rates (t301 = 1.09, p = 0.277) which averaged 1.14 and 1.35 m⋅s−1 respectively (Table 2).
Diving behaviour showed considerable variability among days. Dive frequency varied significantly among days for both individuals (X2 = 194, df = 9, p<0.001; Table 3), with both birds making few dives on day 1, suggesting that they were either resting near the colony or commuting to foraging areas. Bird B had two further days with no or few (3) dives, suggesting a longer commuting time by this individual. Mean dive depth and SST associated with each dive varied significantly among days for both birds (ANOVA: F>6.96, n = 10 days, p<0.001 for all comparisons; Table 3), suggesting that birds moved among habitats, diving differently within each. Bird A foraged primarily in the northern limits of the Sub-Antarctic Frontal Zone (8 to 10°C; hereafter “cold” water) whereas bird B exploited a wider range of warmer water temperatures (10 to 16°C) characteristic of the Sub-tropical Frontal Zone. Inspection of SST maps during this period (Fig. 1) suggests that bird A (cold water) foraged in a band of water at 42–48° S that stretched from South Africa to the Patagonian Shelf. At its closest, this region was approximately 800 km SSW of Inaccessible Island. The warmer water in which bird B foraged mainly occurred between 36–40° S, also stretching across the South Atlantic Ocean and overlapping with Inaccessible Island. Average SST within a 4 km radius of Inaccessible was 12.7±1.4°C (SD), nearly equal to that of bird B on day 1.
Male shearwaters tracked by satellite telemetry illustrate a dual foraging strategy where half of the individuals traveled south towards the Sub-Antarctic Front, and the others traveled west to the Patagonian Shelf (Fig. 1). Males departed the colony between 21 Nov and 07 Dec, which overlaps with the foraging trips of females but not with the 10-d TDR measurements. Within nine days of departing the colony, southward bound birds had traveled between 1200 and 1950 km and westward bound birds traveled ∼4000 km to within 200 km of the South American coast (Table 4; Fig. 1). Sea-surface temperatures associated with their locations (Table 4) showed that southward and westward bound birds foraged in cool (min. temp. typically <10°C) and warm waters (min. temp. >10°C) respectively, corroborating the patterns inferred from TDR data and SST maps. By day nine, two south bound individuals had reached the Polar Front (2.2°C; Table 4).
Nearly all dives occurred during daylight hours (Fig. 2), with a peak at dusk (both birds) and dawn (bird A). Assuming that bird A remained south of Inaccessible at approximately the same longitude, 35.6 and 28.3% of dives occurred within 2 h of sunrise and sunset, respectively. Assuming that bird B foraged as far away as the Patagonian Shelf, 17.3 and 16.8% of dives occurred within 2 h of sunrise and sunset, respectively, with 42.4% of all dives within 3 h of sunset. Without knowing the precise sunrise/set times at each diving location, we can only be certain that 3/930 dives (<0.5%) occurred outside of daylight hours from either region. Dive depth varied significantly among daylight hours (ANOVA bird A F15,722 = 7.56, p<0.001; bird B F17,171 = 4.25, p<0.001), but no clear diel pattern was apparent (Fig. 1).
Vertical lines reference sunrise and sunset times (civil dawn/dusk) for Inaccessible Island (dashed lines) and the Patagonia Shelf region (solid lines) from 20 November 2009. Box plots (lower graphs) indicate median dive depth and first and third quartiles (boxes presented only for hours with n>2 dives).
This study reports the first measurements of diving behaviour for great shearwaters and is only the second to use TDRs on a Puffinus shearwater. The maximum recorded depth (18.9 m) was less than has been recorded for other species: Balearic shearwater (26 m, n = 1 bird ), Audubon's shearwater P. lherminieri (35.4 m ), black-vented shearwater P. opisthomelas (52 m ), wedge-tailed shearwater P. pacificus (66.4 m ), sooty shearwater (67–70 m , ), and short-tailed shearwater P. tenurostris (70.6 m ). Although TDR data from the present study clearly demonstrate that great shearwaters frequently dive deeper than previously thought , they did not dive as deeply as might be expected by allometric relationships between mass and maximum diving depth , given that the great shearwater is the largest member of the genus . Similar sized shearwaters of the genus Calonectris typically perform comparatively shallow dives (mean 2.7 m, max 5.5 m ), though this large winged genus is adapted for gliding in tropical waters . Shallow diving was also common for great shearwaters in the Sub-tropical and Sub-Antarctic Frontal Zones (>50% of dives <2 m, this study). The maximum diving depths reported in this study are likely underestimates of their true maximum potential as we only recorded diving by two individuals. Nevertheless, the mean daily maximum dive depth of bird A (14.5 m; Table 3) is comparable to the mean maximum dive depths for several other Puffinus species , thus, the general patterns reported may be representative of the diving behaviour of great shearwaters. The fact that the birds put on weight during their foraging trips and returned after a similar period to other, control birds, indicates that the TDRs had little impact on their performance.
Although most shearwaters are well adapted for underwater swimming , , virtually nothing is know of the dive profiles for this genus. Most dives by one Balearic shearwater were V-shaped , although 4 s recording interval used in that study may have lacked the precision to detect short bottom phases. By sampling depth twice as frequently as , we were better able to examine dive profiles of great shearwaters. Although most dives were V-shaped, dives with a bottom phase by bird A had an average bottom phase lasting 6.0 s (max 24 s) which accounted for approximately 42% of the total dive time. This suggests that this shearwater was pursuing prey at depth. By comparison, bird B made fewer dives with a bottom phase. Its relatively few, short-duration dives are typical of birds scavenging for offal and discards , possibly at fishing vessels operating on the Patagonian Shelf .
The average bottom time and descent velocity were less than those of other foot and wing-propelled diving seabirds (great cormorants Phalacrocorax carbo and little penguins Eudyptula minor) that dive to similar depths , which would be expected since these birds are shaped for flight rather than underwater locomotion, and also since they dive in the upper few metres of the water column where buoyancy is greatest . However, the ability of shearwaters to descend the water column deserves further investigation, especially regarding the speed and angle adopted during dives to different depths, which will require instruments such as accelerometers sampling at even faster rates .
Several species of procellarids are thought to commonly forage at night , , but we found little evidence of nocturnal diving. Great shearwaters consume large amounts of squids , , , but where and when they obtain this prey is unknown and our data suggest little to no nocturnal diving by this species, as has been reported for other Puffinus shearwaters , . Instead, great shearwaters showed increased diving frequency around dawn and dusk - similar to patterns reported for sooty shearwaters . No clear diel patterns in dive depth were apparent, although diving depths appear to have been greatest in mid morning and again before sunset, which shows partial overlap with deeper diving periods for sooty shearwaters . Great shearwater diet during breeding periods is poorly known, with the few chicks and adults sampled containing mainly squid (flesh and beaks) and occasionally fish and crustaceans , . It is possible that these prey are obtained during shallow dives near dawn and dusk when vertically migrating prey may be closer to the ocean surface  or during surface foraging at night.
The habitats used by the two birds in this study differed with bird A foraging consistently in cool (8–10°C) and bird B in more variable, warmer (10–16°C) waters, characteristic of Sub-Antarctic and Sub-tropical Frontal Zones  respectively. Breeding short-tailed and sooty shearwaters from New Zealand and Australia are known to undertake both short (<500 km) foraging trips within warm neritic waters (13–17°C) and long (∼2000 km) trips to cold polar frontal zones (4–7°C) , , . The temperatures recorded by TDRs correspond with locations of male great shearwater tracked by satellite tags during the first 9 d after departing Inaccessible Island. Males in 8–10°C water were approximately 600–1200 km SSW of Inaccessible, whereas those in 13–16°C water ranged up to 4000 km west towards the Patagonian Shelf which was reached within 7 days by one individual. Thus it seems probable that bird B foraged as far away as the Patagonian Shelf whereas bird A foraged in pelagic waters in the northern Sub-Antarctic Frontal Zone. We observed large differences in diving behaviour between these regions, with more commuting days (due to greater distance traveled), shallower dive depths, and fewer dives in warmer waters. This may have been due to differences between individual diving abilities rather than habitat associations, but the deepest dives of bird B (10.9 m) also occurred in the coldest water (10°C) occupied by this bird. Likewise, sooty shearwaters demonstrated greater diving effort (including more trips, more dives and deeper dives) in cold water regions along the Polar Front , , mirroring patterns observed in this study. Without information on prey depth or abundance, it is not possible to speculate on the foraging efficiency of great shearwaters diving in warm and cold waters during this study. Nevertheless, both birds returned to the colony with replenished body reserves, suggesting that both long-distance trips to warm water regions and short-distance trips to Sub-Antarctic Frontal Zones, may provide profitable foraging strategies for this species.
We thank the Administrator and Island Council of Tristan for permission to visit and work on Inaccessible Island. Logistical support was supplied by the South African National Antarctic Programme (SANAP), and Tristan's Conservation Department; we especially thank Captain C. October and the crew of the Edinburgh and N. Glass. Thank you to S. Wong for her help with accessing and interpreting remote sensing data, M. Martin, D. Veit and S. Johnston for their roles in satellite tag acquisition, as well as B. Friess and M. Bruecker for the technical help with the loggers. We also wish to acknowledge use of the Maptool program (www.seaturtle.org) for graphics in this paper.
Conceived and designed the experiments: RAR PGR. Analyzed the data: RAR YR. Contributed reagents/materials/analysis tools: YR. Wrote the paper: RAR PGR YR. Conducted and supported fieldwork: RAR PGR.
- 1. Brown RGB, Bourne WRP, Wahl TR (1978) Diving by shearwaters. Condor 80: 123–125.
- 2. Burger AE (2001) Diving depths of shearwaters. Auk 118: 755–759.
- 3. Warham J (1977) Wing loadings, wing shapes, and flight capabilities of Procellariiformes. New Zealand Journal of Zoology 4: 73–83.
- 4. Gonzalez-Solis J, Felicisimo A, Fox JW, Afanasyev V, Kolbeinsson Y, et al. (2009) Influence of sea surface winds on shearwater migration detours. Marine Ecology-Progress Series 391: 221–230.
- 5. Shaffer SA, Tremblay Y, Weimerskirch H, Scott D, Thompson DR, et al. (2006) Migratory shearwaters integrate oceanic resources across the Pacific Ocean in an endless summer. Proceedings of the National Academy of Sciences 103: 12799–12802.
- 6. Mougin JL, Mougin MC (1998) Maximum diving depths of Cory's shearwater in the course of its feeding trips during incubation. Revue D Ecologie-La Terre Et La Vie 53: 69–76.
Warham J (1990) The Petrels: Their Ecology and Breeding Systems. London: Academic Press.
- 8. Peck DR, Congdon BC (2006) Sex-specific chick provisioning and diving behaviour in the wedge-tailed shearwater Puffinus pacificus. Journal of Avian Biology 37: 245–251.
- 9. Keitt BS, Croll DA, Tershy BR (2000) Dive depth and diet of the black-vented Shearwater (Puffinus opisthomelas). Auk 117: 507–510.
- 10. Weimerskirch H, Sagar PM (1996) Diving depths of Sooty Shearwaters Puffinus griseus. Ibis 138: 786–788.
- 11. Raymond B, Shaffer SA, Sokolov S, Woehler EJ, Costa DP, et al. (2010) Shearwater foraging in the Southern Ocean: the roles of prey availability and winds. Plos One 5: e10960.
- 12. Shaffer SA, Weimerskirch H, Scott D, Pinaud D, Thompson DR, et al. (2009) Spatiotemporal habitat use by breeding sooty shearwaters Puffinus griseus. Marine Ecology Progress Series 391: 209–220.
- 13. Aguilar JS, Benvenuti S, Dall'Antonia L, McMinn-Grive M, Mayol-Serra J (2003) Preliminary results on the foraging ecology of Balearic shearwaters (Puffinus mauretanicus) from bird-borne data loggers. Scientia Marina 67: Suppl. 2129–134.
- 14. Bull LS, Bell BD, Pledger S (2005) Patterns of size variation in the shearwater genus Puffinus. Marine Ornithology 33: 27–39.
- 15. Cuthbert RJ (2005) Breeding biology, chick growth and provisioning of Great Shearwaters (Puffinus gravis) at Gough Island, South Atlantic Ocean. Emu 105: 305–310.
- 16. Elliot HFI (1957) A contribution to the ornithology of the Tristan da Cunha group. Ibis 99: 545–586.
Marchant S, Higgins P, editors. (1990) Handbook of Australian, New Zealand and Antarctic Birds. Melbourne: Oxford University Press.
Ryan PG, editor. (2007) Field guide to the animals and plants of Tristan da Cunha and Gough Island. Newbury: Pisces Publications.
- 19. Ryan PG, Ronconi RA (in press) The Tristan Thrush Nesocichla eremita as seabird predator. Ardea.
- 20. Coyne MS, Godley BJ (2005) Satellite Tracking and Analysis Tool (STAT): an integrated system for archiving, analyzing and mapping animal tracking data. Marine Ecology Progress Series 301: 1–7.
- 21. Costa DP, Robinson PW, Arnould JPY, Harrison A, Simmons SE, et al. (2010) Accuracy of ARGOS locations of pinnipeds at-sea estimated using Fastloc GPS. Plos One 5: e8677.
- 22. Kato A, Ropert-Coudert Y, Gremillet D, Cannell B (2006) Locomotion and foraging strategy in foot-propelled and wing-propelled shallow-diving seabirds. Marine Ecology Progress Series 308: 293–301.
- 23. Belkin IM, Gordon AL (1996) Southern Ocean fronts from the Greenwich meridian to Tasmania. Journal of Geophysical Research - Oceans 101: 3675–3696.
- 24. Weimerskirch H, Cherel Y (1998) Feeding ecology of short-tailed shearwaters: breeding in Tasmania and foraging in the Antarctic? Marine Ecology Progress Series 167: 261–274.
- 25. Kuroda N (1954) On the classification and phylogeny of the order Tubinares, particularly the shearwaters (Puffinus). Published by the author, Tokyo.
- 26. Grémillet D, Pichegru L, Kuntz G, Woakes AG, Wilkinson S, et al. (2008) A junk-food hypothesis for gannets feeding on fishery waste. Proceedings of the Royal Society B-Biological Sciences 275: 1149–1156.
- 27. Bugoni L, Mancini PL, Monteiro DS, Nascimento L, Neves TS (2008) Seabird bycatch in the Brazilian pelagic longline fishery and a review of capture rates in the southwestern Atlantic Ocean. Endangered Species Research 5: 137–147.
- 28. Wilson RP, Hustler K, Ryan PG, Burger AE, Noldeke EC (1992) Diving birds in cold water: do Archimedes and Boyle determine energetic costs? American Naturalist 140: 179–200.
- 29. Wilson RP, Putz K, Charrassin JB, Lage J (1995) Artifacts arising from sampling interval in dive depth studies of marine endotherms. Polar Biology 15: 575–581.
- 30. Rayner MJ, Hauber ME, Clout MN, Seldon DS, Van Dijken S, et al. (2008) Foraging ecology of the Cook's petrel Pterodroma cookii during the austral breeding season: a comparison of its two populations. Marine Ecology Progress Series 370: 271–284.
Shealer DA (2002) Foraging behavior and food of seabirds. In: Schreiber EA, Burger J, editors. Biology of Marine Birds. Boca Raton, FL: CRC Press. pp. 137–177.
Hagan Y (1952) Birds of Tristan da Cunha. Results of the Norwegian Scientific Expedition to Tristan da Cunha, 1937-1938, No. 20. Oslo: Norske Videnskaps-Akademi.
- 33. Petry MV, Fonseca VSD, Krueger-Garcia L, Piuco RD, Brummelhaus J (2008) Shearwater diet during migration along the coast of Rio Grande do Sul, Brazil. Marine Biology 154: 613–621.
- 34. Rees EIS (1961) Notes on the food of the Greater Shearwater. Sea-Swallow 14: 54–55.
- 35. Rowan MK (1952) The Great Shearwater Puffinus gravis at its breeding grounds. Ibis 94: 97–121.
- 36. Williams TD, Kato A, Croxall JP, Naito Y, Briggs DR, et al. (1992) Diving pattern and performance in nonbreeding Gentoo penguins (Pygoscelis papua) during winter. Auk 109: 223–234.