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C.R. Long 1964 Enderbury Island July 15, 1964 - A landing was made about 1:30 pm. Camp was set up in shed and shack. I walked the west shore of the island - very rocky and the vegetation is not as lush as at Phoenix - at least on this southwest end. Tropic birds observed nesting under slanting stone slabs. rocky with patches of sand and gravel sand *Transect I Digitaria -> Portulaca -> Sida -> Sida -> Triumfetta Triumfeta Portulaca Boerhaavia Boerhaavia Digitaria Digitaria sand and gravel slope darker soil Boerhaavia Digitaria Lepturus Boerhaavia Sida Portulaca -> Lepturus -> Boerhaavia -> Portulaca -> Lepturus Lepturus Portulaca Triumfeta Sesuvium Boerhaavia Portulaca Sesuvium -> -> Sesuvium Eragrostis edge of lagoon raised islet salt crust guano soil with much shell material Observed Boerhaavia sp. with white flowers and little or no anthocyanin in the exposed stems. Messerschmidtia argentea (L.f.) Johnston comprises the brush area as on the chart. This shrub sprouts on the bottom branches and has flowers, the upper parts appear dead possibly as a result of the high concentration of nesting lesser frigatebirds (guano concentration on live stems and leaves, and physical damage as a result of nest building and other avain activities) and/or the high insolation and continuous drying wind. Red footed boobies are also found nesting in this "brush". On the east side of the lagoon - along the edge - were observed several dead patches of Sesuvium sp. indicating perhaps an earlier high water in the lagoon. Evaporation must be rapid but not always so rapid as to insure that even Sesuvium (which has been observed living submerged in salty water) will not be killed back. Sesuvium forms an uneven cover over guano or gravel surfaces associated with Lepturus, Portulaca and Sida - at the periphery of the lagoon, on raised dry heads covered with guano and in the areas just above or in back of the lagoon edge. On this island the Sesuvium forms no solid mat (uninterrupted). Counted twenty-four golden plovers. July 16, 1964 - Plant presses taken out to ship. Dry plants taken from the presses. Drying conditions in the engine room are not ideal. The humidity is too high. The best action is to take smaller samples and segregate the succulent material. On next trip will either have a portable drier or saturate the material with paraformaldehyde solution and defer drying until we reach Honolulu. This latter method might also make for a more organized procedure on shipboard - avoiding the mess and heat of the engine room. Into the field at 3:30 pm walking north toward the lagoon and then on to the north end of the island - mapping vegetation and placing permanent markers (steel poles). North of the old guano ruins a large colony of nesting Greater Frigates - in dead or weakly sprouting Messerschmidtia (some Cordia sp. also present). At the edges of the colony some of the birds make their nest on
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C.R. Long 1964 shrubby Sida bushes. The nests are constructed of Sida twigs with Boerhaavia stems and leaves placed in the center. The nests in the dead or weakly sprouting Cordia and Messerschmidtia are composed of Sida twigs piled high. The twigs on the bottom are weathered a gray color while those on top are lighter and appear to have been added at a later time. The Digitaria sp. is much shorter and less vigorous in appearance than that observed on Starbuck. Much of the Sida is prostrate - only at the protected edges of the lagoon or around the outside edge of the brush patches is the Sida upright. Both seedling and adult plants of Sida seem to be frequent in the Sesuvium patches rimming the lagoon (on the north end the Sesuvium has filled in the old lagoon area). The wind seems to be out of the east at this season and almost constant. The brush piles, located toward the rim of the islands must also penetrate deeper for moisture to the fresh water lens below. This lens is subject to greater depletion in the dry lagoon areas and perhaps the lens is contracted during periods of extreme evaporation and dryness. The guano soils and underlying hardpan, and, the salty crusts formed in the lagoon beds may be responsible for the existence of any vegetation available water supplies on these dry islands. The Lesser Frigates nesting in the brush patch "spill over" into open areas on the west side (bare surfaces or some small Sida and Lepturus). Further along this side of the island is a guano mound, guano operation ruins and another brush area with Cordia and Messerschmidtia spp. supporting the nests of Greater Frigatebirds and redfooted boobies. Transect II (starting on the west near old guano diggings - from the shore). sand Triumfetta -> gravel and sand, bare disturbed site Digitaria Sida -> Boerhaavia -> Lepturus dead Cordia Portulaca Cassytha on Sida larger gravel, rocks -> former house sites mid-point of island Lepturus gravel and sand Sida Digitaria Portulaca Sida Portulaca Boerhaavia In the rubble of the old guano operations on the north end of the island the Sida - Portulaca - Boerhaavia association was observed. A few clumps of Lepturus are also present but very sparsely distributed in this area. The distribution of plant species on the north end is non-uniform. On the rocky flats and rolling mounds Boerhaavia is found - suggesting, perhaps, a pioneer species in rocky or heavily gravelled areas. In some of these same areas one finds Portulaca associated with the Boerhaavia. It may be that the perennial Boerhaavia with its seasonal addition of dead leaves and stems and, finally, a dead rootstock of considerable size may contri- bute significantly to the windblown sand (which accumulates between and down below the rocks) - and windblown organic matter to form the necessary soil pockets for the successful sprouting and growing of other species. The Portulaca is shallow rooted and needs a soil which will hold some water content and at the same time be near the sunlit surfaces. In semi-protected areas behind the hillocks you find patches of Lepturus, usually on the east face slopes. In the depressions between the hillocks - in coral gravel and guano soil Sesuvium seems to thrive, but not forming a continuous mat over the
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C.R. Long 1964 surface. Sida and Portulaca are scattered about in mixed clumps or alone. The vegetation here reflects the disturbance of the past. The loss of cover and the making of new substrates shows vividly the time required for the vegetation associations of low, dry islands to become established. On the west face of one guano mound Fleurya ruderalis was collected - stems very succulent. The plants are shallow rooted. Perhaps during heavy rain the guano soils absorb a large amount of the rainfall and/or the depressions are filled. This latter source of water would supply moisture to the sides of the guano piles. Permanent markers - No. 1 - placed in coral gravel ridge north of the larger guano pit. The cover in this area is approx. fifty percent with Sida, Portulaca and Boerhaavia associated. The site is nnw of the Enderbury light. In the areas between the rubble piles on the west end there are good stands of the Portulaca - Boerhaavia association. These areas have gravel on top with a mixture of sand and guano below forming a fine soil. The best stands are in spots with some protection from the prevailing wind. Permanent marker - No. 2 - placed in fine coral gravel between small rubble mounds - about one-half mile due north and slightly east of the large guano mound on the west side of the island. Here is found a Port- ulaca-Boerhaavia association. Four golden plovers observed on the ground in this area. On the north' side near the beach are a series of deep gouges - approx. ten to twenty-five feet deep. Guano is found on the bottom with small plants of Sesuvium and some Sida seedlings. At the north raised end of the deepest gouge are Portulaca and Sida with trailing Triumfetta on the rocky (with sand pockets) sides of the gouge. On the top of the slope on the north end are found Portulaca, Boerhaavia, Sida and some scattered clumps of Lepturus. On top near the beach one finds Triumfetta alone. This area particularly in the distribution of Portulaca and Lepturus reflects the importance of substrate and topography in the distribution of species on low dry islands. I walked along the north beach to the east end and found Triumfetta, Boerhaavia, Lepturus and Sida- cover is very sparse. I suspect Portulaca also present but there was little light left. * see vegetation map of Enderbury Island constructed by C.R.Long from observations and field notes taken between July 15-17, 1964.
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sand. The stems of Triumfetta are to 10 m. in length with upright sprouts. Not common, probably a wave carried adventive. Found along the west side with Lepturus and Digitaria, less apparent elsewhere At the edge of hardpan just above the lagoon flat on the midwest side. Also occurs at the bottom of a shallow depression N of the guano workings. Not common on Enderbury but commonly distributed in the Phoenix and Line islands. Small trees occur in restricted groves on the S and W sides often with Tournefortia. Used as nesting sites by the redfooted booby and greater frigatebird. Small trees found on the W and S sides with Cordia used as nest sites by the species cited above. Much of the groves on the We side are composed of dead wood. Heavy concentrations of nesting birds combined with salt spray (especially with Cordia) restricts growth. Green sprouts in the area of nest platforms were torn and guano covered. Accumulations of guano found at the surface under these groves but no evidence of phosphatization such as occurs on wet islands under Pisonia was observed. Fifteen species of vascular plants have been recorded from Enderbury Island. Ten of these are considered native, two are problematical introductions and three are known introductions since the European discovery of the island. Only Digitaria of the introduced plants appears to have naturalized to any extent. Collections of vascular plants from Enderbury Island have been made by the following: E. H. Bryan, Jr., March 1924 and July 1938; S. H. Lamb, 1938 March 1938; C. R. Long, November 1964; P. Woodward, February 1965. July and
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we found a quantity of driftwood, lying just on the edge of the bank of coral slabs. Some of the trunks were very large, being fifty or sixty feet in length, and from two to three feet in diameter. — The locality in which these large trees are found, would show that there is at times a very great rise of the waters, which must submerge the islands altogether.” This account was botanically accurate and gives much valuable data with which to make comparisons. In 1964 the channel mentioned by Wilkes was no longer evident represented by a narrow area on the NE side behind which there occurs a low lagoon flat covered with Sesuvium, Portulaca and Eragrostis. In the latter half of the nineteenth century guano mining was carried out on Enderbury Island. According to Hutchinson (1950) about 100,000 tons were removed chiefly from the northern portion. Much of the low flat area around the lagoon and covered with stands of Sesuvium – Eragrostis were also mined probably lowering the soil level to hardpan. During the 1930's colonists were established on the island by the U.S. Department of the Interior. Attempted plant introductions were not successful. The estimated amount of guano taken from Enderbury Island does not seem compatible with the present numbers of nesting sea birds. The guano areas of the island are at the edge of a lagoon which has probably dried up, or, at least been closed off in the recent times. The discovery of recently deposited marine mollusks supports this contention. The bluefaced booby is the chief nester along the lagoon rim but the present population would need a very long period with maximum populations in order to deposit 30 cm. of guano (Hutchinson, 1950). It seems necessary to suppose a possible shift in waters of high productivity near Enderbury and a drop in the population of guano depositing bird populations. The other alternative is to suggest a shift in rainfall patterns and a subsequent dying out of a Pisonia type vegetation under which guano deposition seems to occur on many of the wet islands (Fosberg, 1957). No remnant population of Pisonia occurs on Enderbury Island but a comparably dry island (Malden) does have a few Pisonia which are adjacent to the large guano works on that island. Oceanographic research in the Phoenix Islands may help favor one or the other of the above suppositions. It seems highly probable that the genera Sula and Fregata were and are responsible for the deposition of guano soils on dry central Pacific atolls. The Tournefortia grove on the west side of the island supports nesting populations of Sula sula and Fregata minor. There was no evidence of a phosphatized layer forming underneath the thin litter layer. It is these species with Sula dactylatra and Fregata ariel which deposits layers of guano in open sites where accumulation is apparent on the basis of the individual organism. The influence of man has been relatively slight on Enderbury Island as regards the vegetation. The thick guano layers, however, point to a period in the natural development of the island when the vegetation may have been of a differing composition or to a change in the numbers of nesting seabirds on Enderbury Island. (Digitaria pacifica has naturalized over the sandy inner slopes of the island and appears to be colonizing such areas.) The guano layers originally mined on Enderbury may have been laid down under climatic and/or vegetation regimes which are no longer extant.
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The vegetation of Enderbury Island is typical of the very dry atoll flora found in the central Pacific. Among the native plants are found Eragrostis whitneyi and Sesuvium portulacastrum var. griseum both of which are taxa endemic to low island atolls of the Pacific. Both of these species and Lepturus repens, the common bunchgrass, cover large areas on the inner flats or slopes and beach crest. The Lepturus is found commonly in the sandy peripheral regions and inner slopes while the Eragrostis is confined to low guano emptied areas on the NE, S and on the drier portions or elevated "islets" of the large central lagoon. Many such sites support tall clumps of this small grass but more often the clumps are very short. This probably results from periodic inundation of low areas in the central portion of the island during occasional heavy rain or high tides. Eragrostis apparently cannot stand inundation as can Sesuvium with which it is often associated. The introduced Digitaria pacifica is scattered along the inner slopes along the west side. First collected by Marshall in days of guano mining. 1964 it may have been introduced as early as the mining of guano Other native herbs such as Portulaca lutea, Boerhavia repens, Triumfetta procumbens, Cordia subcordata, Tournefortia argentea, Cassytha filiformis and Sida fallax are common although only the first two are abundant and found over most of the area of the island. The Triumfetta is restricted to sandy slopes on the NW side. The shrubby Tournefortia and Cordia form small groves, mixed and pure on the W and S sides. Sesuvium is common along the edges of the lagoon and in open flats, areas where guano soils have been removed and the elevation of the soils decreased so that the under subsurface soils are constantly moist - often with Eragrostis. This succulent plant is apparently one of the few known endemic plants found on coral atolls. Cassytha was found on the west side of the island parasitizing Sida and Portulaca lutea. Among the introduced plants Euphorbia hirta was found near the wooden structure on the SW side; Fleurya ruderalis and Ipomea tuba are rare. The former was growing on a pile of guano soil near the old guano workings and the latter at the edge of the lagoon on coralline hardpan. The climate or restricted holding capacity of the fresh water lense probably accounts for the failure of Cocos, the remains of a number of which were found in three depressions on the N and S sides of the island, areas left apparently between deposition of coral rubble by high wave action.
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The major demarcation in the vegetation zones of the dry islands occur along the elevation of the lagoon and proceeds to the top of the inner slopes. Under natural conditions the lagoon basin is at sea level or just above - thus some of the lagoons of the dry islands have more seepage than others due to the tidal fluctuations and fill found in the lagoon. Some of the islands have lagoons which were filled in above the level of the sea. Normally around the edges of the lagoon is a low flat, often submerged area on which the halophytic Sesuvium forms luxuriant mats. Not more than a half meter above this area one finds a transition to a Portulaca - Lepturus association found in some cases on guano soils adjacent to the lagoon. On the slopes above with more depth of soil other herbaceous plants such as Boerhavia and Sida form an association. Lepturus is usually found in thick often pure stands on the outermost beaches and not uncommonly on the inner most edge of the lagoon near seeps. In the case of Enderbury Island this concentric ring of species and species associations seems to hold true except in areas where the substrate becomes a limiting factor. Sesuvium, for example, is not found on sand beaches except in areas where the sand is underlain by a watered hardpan. An area a few m2 exists on the NE side of Enderbury in the area where an opening to the sea was reported by Wilkes (?). On Enderbury the importance of sandy areas left in the midst of high wavewrows of coral rubble is evident. The groves of Cordia and Tournefortia on the south end and the former Cocos pits on both the north and south ends are such areas. Such areas apparently marked an area of seepage connected with the lens and were surrounded with piles of coral rubble. In such sites are also found vigorous Sida, Ipomoea tba and, in such areas with sandy sides, Triumfetta.
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A number of surface soil samples were taken and will be reported on elsewhere. The soils found on the island are typically sand based with additions of varying amounts of organic material of two types, bird guano and decayed vegetable material much of which is processed by the hermit crabs. Much of the inner slopes - the wider found on the west side - are covered to a depth of several dm. with a sandy soil overlaying which overlays wave deposited coral rubble. Many areas on the N and S sides which are more recent deposits judging from the lack of soil cover have pockets of sand but these are often too far from the surface to provide a habitat for plants. In other areas coral waverows have been filled with wind and wave deposited sand and on which pioneer plant species such as Boerhavia and Portulaca find a niche. Often these waverows become obscured by the deposition of sand and the formation of soil subsequent to the formation of plant communities. The soils range from almost pure sand to those which contain a low degree of organic material. In some small sites such as thick stands of Lepturus, under Tournefortia and Cordia groves and in locally more mesic sites with lusher vegetation one will finds[illegible] correspondingly higher amounts of organic material mixed with the sand. A second type of soil is found in the low, former lagoon flats and present lagoon with its numerous islets. On the flats one finds a reddish brown, friable soil derived from guano accumulations of nesting seabirds. At the dry edges of the present lagoon a highly saline soil also with admix- tures of guano is found. On the dry islets a lighter powdery guane soil with an admixture of salts and calcium-carbonates derived from exposed fossil layers of mollusks which inhabited the old lagoon, is found. On this soil type are found Sesuvium and Eragrostis and sparingly Portulaca lutea, Sida fallax and Lepturus. At perhaps a half m. elevation above these low guano soil area one finds Portulaca as a common component of partially guano filled soils. It may be that with the lowering of the flats due to the guano mining that the areas for optimal growth of the Sesuvium - Eragrostis association were increased to the detriment of that area on which was found at an elevation only perhaps a half meter higher the Portulaca - Lepturus association which may have characterised much of the guano filled areas of the dry central Pacific atolls. The concentric pattern of atoll vegetation can be seen on Enderbury
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Island. This has been reported to be mainly a result of salinity of the ground water (Fosberg, 1949). One seep at the edge of the present lagoon contained 75.2 ppm of salts almost double that of sea water. In the case of some of the drier islands [illegible] this interior may be affected lay. with enclosed lagoons, the of the island results in an increase in the salinity due to the closed nature of the lagoon and the evaportaion of standing sea water seepage from shallow surfaces. [illegible] may accentuate the importance of salinity and One possible factor of importance its effect in the salinity gradients of dry islands would be the increase on the of salinity in the lagoon which goes hand in hand with the closing off vegetation of channels. One interesting case is that of Sydney Island a small atoll which has been an enclosed lagoon cut off within historic time much like the one at Enderbury. A sample of water taken from the lagoon water in the vicinity of islets along the NW shore evidenced a slainity of 166.0 ppm, nearly five times that of seawater. This increase in salinity may control to a great extent the species found considering the species found in at present on the dry islands working from the lagoon to the outer beach. There is a suggestion that the dying Pisonia on Gardner and Sydney may be due to a combination of [illegible] the lack of rainfall and an increase in salinity of normally tolerable levels of salinity associated with the lense of freshwater. One of the village wells 2.2 m. deep on Sydney contained brackish water in October 1964. If rainfall two bore pits were tested, both were brackish but a reed was growing in one. is negligible and evaporation continues over a long period the fresh water lens may be exhausted in some areas particularly in narrow sides of islets and enclosed islands. Saline waters [illegible] tend to be replacing these at levels where the roots of shrubs and trees penetrate. An unusually high salinity in waters underlying the islets would raise the salinity of the groundwater and may contribute to the irregular pattern of vegetation associations or distribution of species on dry atolls. The Pisonia groves of both Gardner and Sydney Islands are dying or in a state of extreme drought. This is a species usually identified with the more mesic sites of a coral atoll. It is suggested that the increased salinity of lagoon waters due to the enclosure of a once open lagoon may be partly responsible due to the raising of the salinity of the groundwater. This with the prevailing drought may be responsible for the apparent dying back of potential Pisonia groves on these islands.
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Digitaria pacifica much shorter less level than our Starbucks. Much of Sida procumbent - only in protect- ed edges of dragon or arena bowl is Sida upright. Sida, small seedlings and young plants seem to be fre- quent in Sesuvium patches rimming dragon (a white sand desert) hoe field in old dragon area). Londia - Meroechinoidic genera are a top-dend looking / a combination of a. low racipell or low ground water; b. small wind (cost to weed) across island; c. guano dropping or stem can leave from nesting lesser frigate and red-footed boobies. Frigate colony formed about bowl patch and into open area (on west side). Only a few frigate and red-foots near guano rice brush pile. Red-foot nests of Sida in old Londia links. Truncate at old guano digging wet site for scale bend Garcini -> Sida -> Borlaugue -> orchis (gourd) Cassine heptura helenium Digitaria Potulaca Cordiellum Sida capzithan (Sida) Potulaca -> Digitaria -> Sida to mid point in form Potulaca of scale brink side Borlaugue Sida - Borlaugae - Potulaca - in middle of old guano digging well end of island. Some heptura but very sparse. Distribution non-uniform - on rocky flats can find nothing but Borlaugae in other Borlaugae-Potulaca. Sida patches are occasional along rim of old guano works, as is a few scattered clumps of hepturaz. In protected area (behind shield) patch of heptura or low coral bottom Sesuvium (not this) Sida-Potulaca scattered about myself and poor other Corrolo veg- atation pattern of disturbed area.)
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C.R. Long 1964 Soil Samples - June-July 1964 Enderbury July 11, 1964 Phoenix Island (5) I199-I203 I199 - 1 1/2-2 In. Lepturus, Portulaca I200 - 2 Sesuvium 1/2-2 in. I201 - 3 Lepturus, Portulaca Nesting Sooty Terns I202 - 4 1/2-2 in. I203 - 5 1/2 - 2 in. Sida patch - mid north part of island July 12, 1964 Phoenix Island (3) I204-I206 I204 - 1 Algal layer 1/2 in. deep lagoon. Lepturus stand at edge of lagoon (with a narrow strip of Sesuvium at edge between the grass and the bare surface of the lagoon. I205 - 2 1/2-2 in. windblown soil around slab rocks. I206 - 3 1/2-2 in. Lepturus South end. July 13, 1964 Phoenix Island (3) I207-I209 I207 - I Sesuvium mat - dry, open area (0.5-2 in. layer), many roots present; soil dark brown. I208 - II Soil accumulation under coral rock slab. Windblown mineral matter; dried organic (Lepturus, Portulaca) - crab burrows along edge of rock. I209 - III Bare soil surrounded by Portulaca and Lepturus. Gravel at surface 0.5 in. (0.5-2 in. layer) July 15, 1964 Enderbury Island (1) I210 I210 Eragrostis, Sesuvium 1/2-2 in. July 16, 1964 Enderbury Island (4) I211-I214 I211 - 1 1/2-2 in. Portulaca, Boerhaavia, Lepturus west side of lagoon. I212 - 2 Portulaca, Boerhaavia gravel top, fine beneath, northwest end. I213 - 3 top 1/2 in. Cordia grove west end. I214 - 4 1/2-2 in. Cordia grove west side July 17, 1964 Enderbury Island (2) I215-I216 I215 - 1 South end Eragrostis sp., Sesuvium sp. soil 6 in. deep 1/2-2 in. I216 - 2 Cement floored storage house - hermit crab accumulation. July 18, 1964 McKean Island (7) I217-I223 I217 - 1 Under Sida, Sesuvium 1/2-2 inches I218 - 2 1/2-2 in. under dead Sesuvium nest of masked booby I219 - 3 1/2-2 in. bare lagoon dry on top I220 - 4 Boerhaavia, Digitaria near beach, 1/2-2 in. I221 - 5 1/2-1 in. rock area gravel on top south end Boerhaavia, Sesuvium I222 - 6 1/2-2 inches: Digitaria, Portulaca, Boerhaavia I223 - 7 Sida, near old guano ruins 1/2-2 in. nesting sooty terns
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C.R. Long 1964 Addenda to the Report of C. D. Hackman, February - March ATF, 1964. Plants. Enderbury Island February 27, 1964, Sida sp. - Sida fallax Walp. or close. The Sida specimens collected from the Phoenix Islands are partially indistinguishable from Sida cordifolia L. and Sida fallax Walp. A nomenclatorial change or a new taxa may be indicated. Cordia sp. - probably Cordia subsordata Lam. but possible Cordia sebestena L. Dodder sp. - Cassytha filiformis L. February 28, 1964 - "grass is quite small and easily overlooked" - Eragrostis whitneyi Fosb. var. Canton Island March 2, 1964 - Scaevola taccada or Scaevola frutescens (Mill.) Krause for Scaevola sp. The former name is the oldest which may be applied to material commonly called frutescens by most authors. However, the Scaevola in the Phoenix and Line Islands varies from the Scaevola found to the north and new taxa are indicated with the proper nomenclatorial changes.- "several clumps of the species of grass we had discovered near the lagoon on Enderbury"- Eragrostis whitneyi Fosb. var. There are two varieties of this species. Jarvis Island March 14, 1964 Sida sp.-Sida fallax Walp: - see above February 27 note Boerhaavia sp. -B . diffusa L. var. tetrandra Heimerl. - but the status of these color variations also noted on Hull Islnad indicate new taxa. Portulaca sp. - Portulaca lutea Sol. March 15, 1964 "The small bunchgrass-" - Eragrostis whitneyi Fosb. var. "ragweed plant-" - Chenopodium ambrosioides L. Illustrations: -7. Cordia subcordata Lam.; 6. Portulaca lutea Sol.; 5. Lepturus repens (Forst.)R.Br.; 4. Digitaria pacifica Stapf.; 3. Sida fallax Walp.; 2. Tribulus cistoides L.; 10. Euphorbia prostrata L.; 11. Cenchrus echinatus L.; 12. Cynodon dactylon (L.) Pers.; 13. Setaria verticellata (L.) Beauv.; 14. Triumfetta procumbens L.; 15. Sesuvium portulacastrum L. 16. Messerschmidtia argentea (L.f.) Johnston; 17. Cassytha filiformis L.; 18. Ipomoea indica (Burm. f.) Merr.; 19. Eragrostis whitneyi Fosb. var.; 20. Chenopodium ambrosioides L.; 22. Eragrostis whitneyi Fosb. var.; 24. Suriana maritima L.; 25. Heliotropium anomalum H. and A.; 26. Scaevola taccada 27. Acanthaceae (we are having difficulty keying this to genus and species level- it is not grown in Hawaii and may have been introduced from the southwest Pacific area); 28. Polypodium scolopendrim Burm. f. C. R. Long Research Curator