ATOLL RESEARCH BULLETIN NO. 455 NATURAL HISTORY OF BRAMBLE CAY, TORRES STRAIT BY JOANNA C. ELLISON ISSUED BY NATIONAL MUSEUM OF NATURAL HISTORY SMITHSONIAN INSTITUTION WASHINGTON, D.C., U.S.A. SEPTEMBER 1998 NATURAL HISTORY OF BRAMBLE CAY, TORRES STRAIT JOANNA C. ELLISON' ABSTRACT Bramble Cay, a small (3.6 ha) vegetated sand cay, is the most northern island of the Great Barrier Reef and the closest to the mouth of the Fly River. It has both volcanic rock and a reefal sand cay within its lagoon, and phosphatic rock exposures or1 the cay. The sand cay is the most important location for both seabird and turtle breeding in the Torres Strait and supports an endemic mammal, the rat Melornys ruhicola. Records indicate that numbers of birds and rats have declined over the last century, possibly due to erosiou and loss of vegetated area of the cay. The vegetation of the cay, made up of three herbs, is heavily disturbed by nesting activities. There is, however, a large and diverse drift flora, that is dominated by mangrove propagules exported from the Fly, that bas no overlap with the cay's flora. Bramble Cay has a significant human history both from European exploration of the New Guinea coast, and from being the entrance marker to the Great North East Channel through the Torres Strait. INTRODUCTION Bramble Cay is the northern extremity of the Great Banier Reef (GBR) before coral growth becomes limited by the discharge of the Fly, and is the northerly point of Queensland in the Torres Strait (9O08.6 S, 143O52.8 E, Figure 1). It is located 52.8 km SE of Kiwai Island, in the delta of the Fly River, Papua New Guinea (PNG), which carries an annual sediment load of 85 million tons year-' (Harris, et al., 1993) Bramble Cay, however, has clear water and coral reef growth owing to passage of the Fly River plume to the north, tracking directly east along the PNG coastline (Harris, et al., 1993). Of the island types found in the GBR, Bramble Cay (Plate 1) is within the category of low, vegetated sand cays modified by seabird activites described by Stoddart and Fosberg (1991) at Coombe, Michealmas, Raine, Stapleton and parts of Stainer, Morris and Magra. These are all located between 11-17"s; Bramble Cay is distinguished by its location in the wetter and biogeographically more diverse northern sector of the GBR. These types of islands feature patchy vegetation cover, with uncommon shrubs, and large bare areas resulting from seabird disturbance. LSchool of Applied Sciences, University of Tasmania, P. 0. Box 1214, Launceston, Tasmania 7250, Australia. Rlnwtzscript rcccivcd 6 April 1998; revised 26 Allgllst 1998 The closest climate station to Bramble Cay is Daru (74 km to the west), which shows a mean annual rainfall of 2063 mni, and a range of 1163-3972 mm in the period 1894 to 1970 (McAlpine et al., 1983). Most rainfall occurs in the summer period, November to April. Southeasternly trade winds prevail from March to November, tending to send westward currents through the Torres Strait; the Northwest monsoon prevails December to March, tending to send an eastward current through the Strait. Tides in the Gulf of Papua are semi-diurnal, with a mesotidal range of 2-2.5 in. Circulation in the Gulf of Papua is driven by tidal and wind-induced currents. influences the distribution of sediment load of the Fly along the coastal zone. The Fly has an annual freshwater discharge rate exceeding 235 km3 (Alongi et al., 1992), carrying 85 million tons of sediment year - 1 (Harris et al., 1993), of which 47% is discharged from the delta. This sediment is largely carried northeast from the delta and along the coast of the Gulf of Papua, except during the southeast trade wind season, when a small proportion of discharge from the Fly traverses west from the delta and along the southern coastline of PNG (Harris et al., 1993). GEOLOGY AND GEOMORPHOLOGY The island rises from water depths of 35 nl to an oval reef 1.8 x 0.9 km (Figure 2). It is of volcanic origin, demonstrated by exposures of Pleistocene Maer volcanics in the lagoon (Sardine, 1928; Willmott, et al., 1973). Similar exposures occur at several locations in the NE Torres Strait, at the Murray, Darnley and Stephens Islands, and the Black Rocks 6.5 kin to the SW of Bramble Cay. They result from subaqueous emission of basaltic lava, that subsequently was deeply eroded. The largest exposure (about 40 x 40 m) in the Bramble Cay lagoon is shown in Plates 1 and 2. The sand cay occurs at the western margin of the lagoon, 330 m NW of the large volcanic outcrop, and has a vegetated area of 175 x 76m. It is composed of foraminifera1 sand, with some coral and shell fragments (Jardine, 1928), with an exposure of phosphatic rock on the southeast shore (Figure 3, Plate 3) that rises to 1.9 111 above I-ITM. The vegetated area has several raised ridges and lower pools which collect rainwater (Plate 1). Stratigraphy was examined at two locations. Location 1, on a ridge in the southeast of the island, showed 14 cm of organic peat above hard phosphatic rock. Location 2, adjacent to a pool in the center of the island, showed 22 cm of peat above 40 cm of loosely cemented calcareous sand. This is similar to stratigraphy reported from Raine (Stoddart et al., 1981) of moist black peat above calcareous rubble. In 1862 a mining lease was granted to the Anglo-Australian Guano Company (Crowther, 1939), and occasional boats mined the low grade phosphatic rock (Sardine, 1928). The quality was poor enough to ensure that a base was not established as at Raine (Stoddart et al., 1981), and areas of rock remain today. There is an exposure at the eastern end of the cay (Figure 3, Plate 3). A sample of this rock was analysed, and compared with a surface soil sample from the interior of the cay. Samples were treated with perchloricl nitric acid and analysed by ICP-AES. Owing to their high carbonate and phosphatic content, they were diluted for verification. Results are given in Table 1. Stoddart and Scoffin (1983) reported levels of phosphate of 7.8-35.1% from rock on Raine, demonstrating the lower grade quality of the Bramble Cay rock. This is probably because Bramble Cay receives substantially more rainfall than Raine. Coal is commonly found on Bramble Cay, both inland on the surPace and cxposed in wave eroded sand cliffs. Plate 4 shows these as wave-rounded and cobble sized. Thc source is ships wrecked on the island (Table 2), the most likely being either t h ~ Windhover (1889) or the Mutluh. (1915). Both are discussed in the next section. EARLY HISTORY Thc chronology of human visits to the island is given in Table 2 Customary tenure of Bramble Cay is held by the inlrabilanls of Darnlcy Island, 45 kin to the southwest. The islanders' legend of Rebes describes how Darnley people, using soil rafted from Darnley, built Bramble Cay to provide turtle eggs and meat in season. Having deposited the soil lo form the Cay, the wind veered and strengthened, and four villagers were fixed to form the volcanic rock outcrop, and the rest formed thc (phosphatic) stone on the sand cay (Haddon, 1935). Darnley Islanders travel to Bramble Cay to collect turtle and bird eggs during the nesting season, and also grant inhahitmts of other islauds permission to collect (Johannes and MacFarlane, 1991). 'The island was uamed after the HMS Brarizhle which under the command of Lieutenant C. B. Yule, was engaged in survey work in the Torres Strait and the southern coast of Papua New Guinea in 1843 and succeeding years (Jukes, 1847). Accounts of tlicse early visits provide iuformation about the island's earlier history and ccology. The F!,) visitcd Bramble Cay on 6 May, 1844, and Jukes comments: The sand-key on one side of the reef was precisely similar in appearance and structure to Raine's Islet, except that it was much smaller. It equally abounded in "spinach" and bird's eggs, and any ship corning in from the Pacific in want of fresh provisions might get enough for some days' consumption by stopping there, taking care to break all the eggs on the island as soon as they arrive, in order to have new-laid ones to carry away with them (Jukes, 1847). When the Btznzhle returnedto Bramble Cay in April 1846, a junior officer remarked thai Mr. Yule considered it to be a good anchorage "because it was free from natives of who111 he entertained the greatest horror. Here besides a good supply of eggs and spinach we also obtained 5 turtle" (Sweatman, 1977). The anchorage was returned to on 3 June, after a survey of the south coast of New Guinea. The ship remained 5 days to obtaiu observations for ra:ing the chronometers, and took advantage of the stay to obtain a good supply of eggs (Sweatman, 1977). During the visit of the Rattlesnuke 16-19 December 1849, tern and booby eggs were smashed and gathered, and a total of 18 turtles were taken (Huxley, 1935). I-luxley comments: "The spinach to my mind is filth; others like it however." MacGillivray (1852) comments from the same visit: In the afternoon I landed for an hour, passing many t ~ ~ r t l e on the water both going and returning. As usual the island was covered with sea birds, only two species, however, of which were breeding. The Brown Booby (Sulafusca) and a large tcrn (Tlzalusseus pelecanoides) existed in about equal numbers .... As the tern eggs were within a short time of being hatched we broke all we saw in order to ensure some newly laid ones in a day or two ... The Golden Plover was plentiful on the island during our visit, and one afternoon I killed fifteen in about an hour ... The weed which in the FIJ we used to call spinach (a species of Boerlzcimio, actually B. rluJfusa) being in abundance here, was at my suggestion collected in large quantity for the use of the ships company as a vegetable., but it did not seem to be generally liked. In 1889 four ship wrecks occurred on the island (see Table 2). The Master of one requested in a letter to Nautical Mugazine that a lighthouse be located on the cay (Planck, 1889). He stated that the island is at the entrance to the N.E. channel, is difficult to see owing to its low elevation, and because strong and irregular currents occur in the area. The Wilzdlzover went ashore on the cay in August 1889 while carrying coal, and was abandoned. This wreck could have colitributed some of the coal found today on the cay. A James Nourse steamer, the Mrrtlalz, went aground at Bramble Cay on 281811915 on a voyage from Port Kembla to Colombo. It was refloated on 13/9/15 (John Foley. pers. comm), apparently after some thousands of tons of coal had been jettisoned. This coal is referred by Rev. Done, who visited the island on the Herald in 1917, and used some of the coal for fuel (Done, 1987). Done (1987) was not there in the turtle breeding season, so "On this occasion we had to be content with terns' eggs and secured a large quantity ........ They were subscquentely used boiled, fried, scrambled or in omelette form, and were not in the least fishy i n flavour." Bramble Cay was heavily exploited in its early history for bird and turtle eggs by both European and Tones Strait Islander visitors. The effects of this exploitation on breeding colonies are discussed in the fauna section below. Lighthouse History Bramble Cay, marking the northern entrance to the Great North East Channel through thc Torres Strait, is today dominated by a lighthouse (Plate 5) . From 1890 it was the boarding ground for pilots to guide sailing vessels through the channel to Thursday Island (Davenport, 1986). This followed a series of shipwrecks on the cay (Table 2), and requests for a lighthouse (see previous section). Done records in 1917 that "according to a chart there is a beacon 45 ft high. But that beacon has long been in a recumbent position, and is of no value to mariners. It is whispered that there is some talk of an unattended light being placed there ...." In 1924 (24 October) a 42 ft pyramidal steel tower was erected. Jardine (1928) showed this as located in the central eastern end of the island (Figure 6). There are no remains of this tower today. According to A.M.S.A. records it was razed in 1954 and replaced by the present lighthouse, though Limpus et al. (1983) reported that a temporaly scaffold with four wire guys was erected at the southeastern end of the cay in 1958. The remains of this structure can be found on the beach at the southeastern end (Fig. 3, Plate 6), the island having moved to the northwest. The present lighthouse, a 17 In stainless steel tower, was converted to solar power on 6 January 1987. The lighthouse was never manned, but is maintained by A.M.S.A. vessels every 3-6 months. MOVEMENT OF THE CAY Figure 4 shows changes in shape of Bramble Cay between 1978-1979 when it was mapped by Applied Ecology (Parmenter, 1980), and 1994-5 when it was mapped by the author using tape and compass techniques. Other detailed surveys of the island exist that could not be incorporated into this map. Jardine (1928) provided a map of the island from his visit in September 1924 (Figure 6), but the remains of the lighthouse shown on this map could not be located in 1994-5, hence there is no common reference. In 1924 the area of the cay within the tidal level shown by Jardine (1928) was 395 x 183 m. Limpus et al. (1983) record the dimensions of the island at spring high tide level in December 1977 and 1978 as 340 x 150 m. Parmenter (1980) mapped the island area above high tide as 281 x 128 m in October 1978, and 223 x 112 tn in March 1979. In January 1987 the dimensions of the island above high tide were 320 x 130 m (Walker, 1988); in Februa~y 1994 it was 272 x 126 m and in February 1995 it was 251 x 104 m. The area of the island in 1995 was 1.72 ha in vegetated area, and 3.62 ha above high tide mark. Limpus et al. (1983) concluded that the cay was moving towards the northwest, and losing sand over the edge of the reef flat (see Fig. 2). Parmenter (1980) showed that during the south-easterlies (winter) sand is deposited at the northwest shore of the cay, which is eroded during the north-westerlies (summer). Figure 4 shows that the shape of the cay has not substantially changed since the 1970's, the most significant change being reduction in vegetated area. In 1924 the vegetated area was 295 x 146 m at its widest dimensions (Jardine, 1928); in 1978-79 it was 170 x 97 m (Parmenter, 1980); in January 1987 it was 215 x 100 m (Walker, 1988); and in 1994-5 it was 175 x 76 m. Figure 4 shows that most of the loss has been from the south and north shores. Plate 7 shows how the vegetation margins arc limited by the activites of turtle nesting. A former control on turtle nesting would have been cliffs of phosphatic rock, the historic removal of this would make more island area accessible. The main control today is turtle access. Turtle breeding occurs in the summer period, when the island is being eroded from the northwest. Plate 8 shows the sand cliff that develops, which discourages turtles from coming ashore. Many failed attempts were witnessed at night in Februa~y 1995. The turtles would move along the shore and successfully cross the beach on the gentler graded south or north shores. The east shore is somewhat protected from turtles by the phosphatic rock outcrop cliffs. Thc reliability of Jardine's measurement techniques is demonstrated by his detailed map of the volcanic rocks in the lagoon. Therefore his map of the cay can bc used as strong evidence that the island has substantially eroded this century. The awa within high tide levels is more variable (Figure 4) with seasonal prevailing wind, but the vegctated area has consistently declined. WATER Water collects in pools on Bramble Cay after rainfall and can remain for several days. Water samples were tested in February 1995 from two locations: 1 was the large pool in the NE of the cay (Figure 5, Plate 5 ) , and 2 was the large pool SE of the lighthouse (Figure 5 , Plate 7). Results in Table 3 show that surface pools are of fresh water. VEGETATION AND FLORA The vegetation of Bramble Cay consists of low herbaceous cover (Plates I and 5), greatly disturbed by nesting activities of birds and turtles. Species present in 1994-5 and past records are summarised below. Nomenclature follows Fosberg and Stoddart (1991). AIZOACEAE Sesuvium portulacastrum (L.) L. Limpus et al. (1983) sight. AMARANTHACEAE Parmenter, s.n. (January, 1984); Queensland Herbarium s.n. (in Walker, 1988); Walker (1988); Ellison 1002, 1003, 1005. This erect or decumbent annual with weedy habit was occasional on Bramble Cay in 1994 and 1995. ARECACEAE (PALMAE) Cocos nuc