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<title>Pacific Science, Volume 44, Numbers 1-4, 1990</title>
<link>http://hdl.handle.net/10125/979</link>
<description/>
<pubDate>Sun, 26 May 2013 00:01:31 GMT</pubDate>
<dc:date>2013-05-26T00:01:31Z</dc:date>
<image>
<title>Pacific Science, Volume 44, Numbers 1-4, 1990</title>
<url>http://scholarspace.manoa.hawaii.edu:80/bitstream/id/2800/PacSci.jpg</url>
<link>http://hdl.handle.net/10125/979</link>
</image>
<item>
<title>44: Index - Pacific Science</title>
<link>http://hdl.handle.net/10125/12593</link>
<pubDate>Mon, 01 Jan 1990 00:00:00 GMT</pubDate>
<guid isPermaLink="false">http://hdl.handle.net/10125/12593</guid>
<dc:date>1990-01-01T00:00:00Z</dc:date>
</item>
<item>
<title>44:4 Table of Contents - Pacific Science</title>
<link>http://hdl.handle.net/10125/1295</link>
<pubDate>Mon, 01 Oct 1990 00:00:00 GMT</pubDate>
<guid isPermaLink="false">http://hdl.handle.net/10125/1295</guid>
<dc:date>1990-10-01T00:00:00Z</dc:date>
</item>
<item>
<title>Plant Water Deficits, Osmotic Properties, and Hydraulic Resistances of Hawaiian Dubautia Species from Adjacent Bog and Wet-Forest Habitats</title>
<link>http://hdl.handle.net/10125/1294</link>
<description>Functional responses of two closely related Dubautia species from&#13;
a mosaic of Hawaiian bogs and wet forest were compared to help explain their&#13;
differential distributions. Dubautia paleata is largely restricted to saturated bogs,&#13;
while D. raillardioides is restricted to the surrounding, better-drained wet forest.&#13;
Minimum diurnal tissue water potentials of D. paleata are significantly lower&#13;
than those of D. raillardioides, despite the moister condition of bog soil. The tissue&#13;
osmotic potential at full hydration of D. paleata is significantly lower than&#13;
that of D. raillardioides. As a result, the tissue water potential at which turgor&#13;
reaches zero for D. paleata is significantly lower than that of D. raillardioides.&#13;
Dubautia paleata is thus able to maintain positive turgor to lower water potentials&#13;
than D. raillardioides. Lack of a lowered, in D. raillardioides may therefore&#13;
contribute to exclusion of that species from the bog habitat. Preliminary data&#13;
suggest a significantly greater hydraulic resistance for D. paleata than for D.&#13;
raillardioides, probably due to higher root resistance caused by the reduced&#13;
condition of the waterlogged bog substrate. The difference in hydraulic resistance&#13;
could help account for the contrasting water deficits of the two species.
</description>
<pubDate>Mon, 01 Oct 1990 00:00:00 GMT</pubDate>
<guid isPermaLink="false">http://hdl.handle.net/10125/1294</guid>
<dc:date>1990-10-01T00:00:00Z</dc:date>
<dc:creator>Canfield, Joan E</dc:creator>
</item>
<item>
<title>Revision of the Genera of Gall Crabs (Crustacea: Cryptochiridae) Occurring in the Pacific Ocean</title>
<link>http://hdl.handle.net/10125/1293</link>
<description>The coral gall crabs, Family Cryptochiridae, occurring in the&#13;
Pacific Ocean are reviewed. Fifteen genera, including four new genera, are&#13;
recognized: Cryptochirus Heller; Dacryomaia, new genus; Fizesereneia Takeda&#13;
&amp; Tamura; Fungicola Serene; Hapalocarcinus Stimpson; Hiroia Takeda &amp;&#13;
Tamura; Lithoscaptus Milne Edwards; Neotroglocarcinus Takeda &amp; Tamura;&#13;
Opecarcinus Kropp &amp; Manning; Pelycomaia, new genus; Pseudocryptochirus&#13;
Hiro; Pseudohapalocarcinus Fize &amp; Serene; Sphenomaia, new genus; Utinomiella&#13;
Kropp &amp; Takeda; and Xynomaia, new genus. Host, depth, and distribution&#13;
records are given for each genus. A key to the females of all gall crab genera is&#13;
included.
</description>
<pubDate>Mon, 01 Oct 1990 00:00:00 GMT</pubDate>
<guid isPermaLink="false">http://hdl.handle.net/10125/1293</guid>
<dc:date>1990-10-01T00:00:00Z</dc:date>
<dc:creator>Kropp, Roy K</dc:creator>
</item>
<item>
<title>Movement of Coconut Crabs, Birgus latro, in a Rainforest Habitat in Vanuatu</title>
<link>http://hdl.handle.net/10125/1292</link>
<description>Patterns of movement in the coconut crab, Birgus latro (L.), were&#13;
studied using mark-recapture and radio-tracking techniques at a number of&#13;
sites in the rainforest regions of eastern Santo, Republic of Vanuatu (South&#13;
Pacific). Movement was assessed both for crabs caught and released in one place&#13;
(indigenous) and for crabs caught and then released at a new location&#13;
(introduced). Recapture rates in eastern Santo were very small ( &lt; I%), whereas&#13;
on the small islet sites (area &lt;2 ha) the rate approached 20%. There were no&#13;
significant relationships between distance moved and either time at liberty or&#13;
size of the individuals for introduced crabs. But for indigenous crabs, size of&#13;
individual was negatively correlated with distance moved. Recapture rates of&#13;
introduced and indigenous crabs were similar , but introduced crabs moved&#13;
significantly further from their point of release. Almost all radio-tagged crabs&#13;
moved from their point of release; smaller crabs tended to move further. On&#13;
eastern Santo, only two of five radio-tagged crabs were located again ; both had&#13;
moved over 250-m away from their release point. On the islet sites, all radiotagged&#13;
crabs were found again at least once; some of these returned to a number&#13;
of different sites, indicating that B. latro seems to be able to home to particular&#13;
locations. Nonetheless, dispersal of animals from an area, at least after handling,&#13;
is a common feature.
</description>
<pubDate>Mon, 01 Oct 1990 00:00:00 GMT</pubDate>
<guid isPermaLink="false">http://hdl.handle.net/10125/1292</guid>
<dc:date>1990-10-01T00:00:00Z</dc:date>
<dc:creator>Fletcher, WJ; Brown, IW; Fielder, DR</dc:creator>
</item>
<item>
<title>Shell Exchange in Hawaiian Hermit Crabs</title>
<link>http://hdl.handle.net/10125/1291</link>
<description>Shell exchange behavior of intertidal Hawaiian hermit crabs was&#13;
observed in the laboratory. Outcomes of 255 shell-related interactions were&#13;
analyzed to test the predictive powers of two models of resource exchange. In&#13;
the case of intraspecific interactions, the negotiations model (which predicts that&#13;
exchanges should occur only when both crabs will gain in shell value) was&#13;
superior to an aggression model of resource exchange. In the case of interspecific&#13;
interactions, the negotiations model accurately predicted outcome of CalcinusCalcinus&#13;
interactions, but poorly predicted outcome of Calcinus-Clibanarius&#13;
interactions.
</description>
<pubDate>Mon, 01 Oct 1990 00:00:00 GMT</pubDate>
<guid isPermaLink="false">http://hdl.handle.net/10125/1291</guid>
<dc:date>1990-10-01T00:00:00Z</dc:date>
<dc:creator>Hazlett, Brian A</dc:creator>
</item>
<item>
<title>Morphology of the Feeding Apparatus of Cancer novaezelandiae in Relation to Diet and Predatory Behavior</title>
<link>http://hdl.handle.net/10125/1290</link>
<description>Morphology of the mouthparts, gastric mill, and chelae of the&#13;
New Zealand cancer crab, Cancer novaezelandiae Jacquinot, 1853, was investigated&#13;
in relation to dietary composition and predatory behavior. Mouthparts&#13;
and gastric mill were typical of those of other large, predatory brachyurans, with&#13;
similar structure for male and female, small (60-70 mm) and large (120-130 mm&#13;
carapace width) crabs. The third maxilliped had large crista dentata, and the&#13;
inner margin of the mandible was rounded, with a sharp, cutting edge. The large,&#13;
robust chelae were homeochelous with respect to structure and dental pattern.&#13;
A large diastema was present and both chela exhibited high mechanical advantage&#13;
(0.36 and 0.37 for left and right chela, respectively). Relative growth of the&#13;
propodus was positively allometric, which remained constant throughout crab&#13;
growth. Morphological features of the feeding apparatus suggested adaptations&#13;
for macerating coarse, particulate material. This was supported by foregut&#13;
analysis showing a predominance of sessile and slow-moving macroinvertebrates&#13;
in the diet. Bivalve and gastropod molluscs followed by crustaceans dominated&#13;
the diet; fish, sponges, coelenterates, and plant matter occurred less frequently.&#13;
Little variation in dietary composition was evident with crab sex, size, or season.&#13;
Cancer novaezelandiae adopted five distinct techniques to open bivalve shells and&#13;
three techniques to open gastropod shells. These include direct, umbone and&#13;
posterior crushing, umbone splitting, posterior chipping, and aperture breakage&#13;
and spire removal. The success of these techniques was dependent upon crab&#13;
size and prey size and shape. Large crabs were able to use direct crushing over&#13;
a wider size range of prey than smaller crabs. The structural and behavioral&#13;
adaptations permit C. novaezelandiae to specialize on mollusc prey and may&#13;
explain its migrations into areas dominated by molluscan species.
</description>
<pubDate>Mon, 01 Oct 1990 00:00:00 GMT</pubDate>
<guid isPermaLink="false">http://hdl.handle.net/10125/1290</guid>
<dc:date>1990-10-01T00:00:00Z</dc:date>
<dc:creator>Creswell, Paul D; Marsden, Islay D</dc:creator>
</item>
<item>
<title>Hawaiian Monk Seal Pupping Locations in the Northwestern Hawaiian Islands</title>
<link>http://hdl.handle.net/10125/1289</link>
<description>Most births of the endangered Hawaiian monk seal, Monachus&#13;
schauinslandi, occur in specific beach areas in the Northwestern Hawaiian&#13;
Islands. Data collected from 1981 to 1988 on the locations of monk seal births&#13;
and of the first sightings of neonatal pups were summarized to identify preferred&#13;
birth and nursery habitats. These areas are relatively short lengths of beach at&#13;
the breeding islands and have some common characteristics, of which the primary&#13;
feature is very shallow water adjacent to the shoreline. This feature, which&#13;
limits access by large sharks to the water used by mother-pup pairs during the&#13;
day, should enhance pup survival.
</description>
<pubDate>Mon, 01 Oct 1990 00:00:00 GMT</pubDate>
<guid isPermaLink="false">http://hdl.handle.net/10125/1289</guid>
<dc:date>1990-10-01T00:00:00Z</dc:date>
<dc:creator>Westlake, Robin L; Gilmartin, William G</dc:creator>
</item>
<item>
<title>Coastal Geomorphology of the Beqa and Yanuca Islands, South Pacific Ocean, and Its Significance for the Tectonic History of the Vatulele-Beqa Ridge</title>
<link>http://hdl.handle.net/10125/1288</link>
<description>Data referring to elevations of emerged shoreline indicators along&#13;
the coasts of Beqa and Yanuca islands in southern Fiji were collected and&#13;
indicate the presence of former mean sea levels at elevations (and shoreline&#13;
names) of 0.96 m (MUAI), 1.93 m (BULl), 2.63 m (MUA2), 4.32 m (MUA3),&#13;
5.94 m (MUA4), and 7.79 m (MUA5) above present mean sea level. No dates&#13;
for shoreline formation or emergence are available directly although age is&#13;
believed to increase with increasing elevation. Investigations of the Beqa lagoon&#13;
floor and comparison of shoreline levels between eastern Beqa, western Beqa,&#13;
Yanuca, and Vatulele island (at the western end of the Vatulele-Beqa Ridge)&#13;
suggest that downfaulting along faults and grabens trending a little west of north&#13;
has occurred both during and since the time of shoreline emergence. Uplift related&#13;
perhaps to either compression of the area between the Kadavu Trench (Hunter&#13;
Fracture Zone) to the south and the Fiji Fracture Zone to the north or the&#13;
renewal of northward underplating along the Kadavu Trench is believed to&#13;
be responsible for shoreline emergence, which was probably contemporary&#13;
along the whole Vatulele-Beqa Ridge and occurred during-the middle and late&#13;
Quaternary.
</description>
<pubDate>Mon, 01 Oct 1990 00:00:00 GMT</pubDate>
<guid isPermaLink="false">http://hdl.handle.net/10125/1288</guid>
<dc:date>1990-10-01T00:00:00Z</dc:date>
<dc:creator>Nunn, Patrick D</dc:creator>
</item>
<item>
<title>Review Article: Geology and Volcanology of the Hawaiian Islands</title>
<link>http://hdl.handle.net/10125/1287</link>
<description>This article summarizes the present state of knowledge of the&#13;
geology of Hawaii. It tends to concentrate on aspects not usually covered by&#13;
review articles. Current ideas on hotspots and mantle plumes are applied to the&#13;
specific example of Hawaii, the eight volcanic systems currently nourished by&#13;
the hotspot are identified, and gross differences in magma-supply rate are related&#13;
to position of these systems on the hotspot. The important role played by level&#13;
of neutral buoyancy in distributing incoming magma between magma chambers,&#13;
rift zones, intrusions, and surface flows is discussed. This is important because&#13;
volcanic edifices may expand nearly as much by growth of subsurface intrusions&#13;
as by surface lava outpourings. Recent discoveries, however, show how strongly&#13;
volcano growth is countered by subsidence and major collapses. A brief description&#13;
is given of styles of volcanism in Hawaii, and recent ideas on how formation&#13;
of aa and pahoehoe depends on eruption discharge rate are discussed . A brief&#13;
summary description pointing to highlights of each volcano is then presented.&#13;
Finally, I indulge in speculations regarding geographical distribution of the&#13;
volcanoes and show how, by postulating that a considerable strike-slip motion&#13;
has occurred on two faults, a much more orderly arrangement of volcano and&#13;
rift-zone alignments appears, leading to a dynamic model of island-chain growth&#13;
that is simpler then current models. Proceeding from Kaua'i toward the southeast,&#13;
an alternating sequence of southeast and west-southwest alignments is&#13;
revealed. These alignments may be related, respectively, to fractures propagated&#13;
against the plate motion direction (because of extensional stresses resulting from&#13;
diverging flow in the mantle plume) and along faults of the Moloka'i fracture&#13;
zone.
</description>
<pubDate>Mon, 01 Oct 1990 00:00:00 GMT</pubDate>
<guid isPermaLink="false">http://hdl.handle.net/10125/1287</guid>
<dc:date>1990-10-01T00:00:00Z</dc:date>
<dc:creator>Walker, Geprge PL</dc:creator>
</item>
<item>
<title>44:3 Table of Contents - Pacific Science</title>
<link>http://hdl.handle.net/10125/1286</link>
<pubDate>Sun, 01 Jul 1990 00:00:00 GMT</pubDate>
<guid isPermaLink="false">http://hdl.handle.net/10125/1286</guid>
<dc:date>1990-07-01T00:00:00Z</dc:date>
</item>
<item>
<title>Zooplankton of the Gulf of California after the 1982-1983 El Nino Event: Biomass Distribution and Abundance</title>
<link>http://hdl.handle.net/10125/1285</link>
<description>From 23 March to 7 April 1984, we studied the responses of&#13;
zooplankton populations to the 1982-1983 El Nino event in the Gulf of&#13;
California. Twenty six stations were sampled for zooplankton distribution and&#13;
abundance. Mean displacement volume was 388 cm3/lOOO m3&#13;
, a value higher&#13;
than biomass values reported for the California Current and the eastern tropical&#13;
Pacific. Maximum values (up to 60 mg/m3 of dry weight) were registered on the&#13;
eastern shore of the gulf. At other stations biomass values ranged from 11.2 to&#13;
39.2 mg/m3&#13;
. No significant differences were observed in the mean biomass of the&#13;
central gulf between spring 1983 and spring 1984. However, biomass increased&#13;
in the southern gulf during spring 1984. Mean total abundance of zooplankton&#13;
was 13% higher than in 1983. Coastal stations registered up to 31% of the total&#13;
abundance. Copepods and cladocerans represented over 65% of mean total&#13;
abundance and community structure differed from that in 1983: there were&#13;
more copepods, euphausiids, tunicates, and siphonophores in 1984, and fewer&#13;
cladocerans, ostracods, and red crabs (Pleuroncodes planipes). Similarity analysis&#13;
showed two main assemblages: one in the central gulf (temperate zone), the other&#13;
near the mouth (tropical zone). These two regions correspond to zones with&#13;
different physical and primary production characteristics. The different responses&#13;
seen in the central and southern gulf may reflect phytoplankton biomass&#13;
and primary productivity dynamics. The El Nino event reduced the biomass in&#13;
the southern part of the gulf, although the entire gulf in 1983 and 1984 showed&#13;
higher biomass values than other eastern Pacific systems. Year-to-year differences&#13;
may be less important than seasonal changes. The EI Nino phenomenon&#13;
mainly affected the relative abundances of different taxa.
</description>
<pubDate>Sun, 01 Jul 1990 00:00:00 GMT</pubDate>
<guid isPermaLink="false">http://hdl.handle.net/10125/1285</guid>
<dc:date>1990-07-01T00:00:00Z</dc:date>
<dc:creator>Lavaniegos-Espejo, Bertha E; Lara-Lara, J Ruben</dc:creator>
</item>
<item>
<title>Changes in the Structure and Composition of a New Zealand Lowland Forest Inhabited by Brushtail Possums</title>
<link>http://hdl.handle.net/10125/1284</link>
<description>All specimens of 19 tree and 11 shrub species greater than 10 cm&#13;
dbh (more than 3000 stems of trees and tree ferns) were labeled, measured, and&#13;
mapped in 2.25 ha of lowland forest near Wellington, New Zealand. Their fate,&#13;
growth, and additional recruitment were monitored in three surveys over 16 yr,&#13;
from 1969 to 1985. During the vegetation study, movements, diet, density, and&#13;
breeding success of the introduced Australian brushtail possum (Trichosurus&#13;
vulpecula) were studied in the same area of forest. In the study plot the number&#13;
of stems and their total basal area increased between 1969 and 1985. However,&#13;
several species that are eaten by possums have suffered substantial losses of both&#13;
stems and total basal area. These include Beilschmiedia tawa, Weinmannia racemosa,&#13;
Metrosideros robusta, and the tree fern Cyathea medullaris. Species not&#13;
eaten by possums have increased in both numbers and basal area. These include&#13;
Hedycarya arborea, Cyathea smithii, Cyathea dealbata, and Laurelia novaezelandiae.&#13;
During the study there has been a decline in basal area of emergent&#13;
trees, an increase in basal area of canopy trees (but little increase in their&#13;
numbers), and an increase in numbers and basal area of minor species and dead&#13;
trees. If present trends in structure and composition of this lowland forest&#13;
continue, the future forest will have a greater proportion of tree ferns and more&#13;
short-lived, small-diameter species. Canopy height and species diversity are also&#13;
likely to decrease.
</description>
<pubDate>Sun, 01 Jul 1990 00:00:00 GMT</pubDate>
<guid isPermaLink="false">http://hdl.handle.net/10125/1284</guid>
<dc:date>1990-07-01T00:00:00Z</dc:date>
<dc:creator>Campbell, DJ</dc:creator>
</item>
<item>
<title>Identity of Aralia bastardiana Decaisne</title>
<link>http://hdl.handle.net/10125/1283</link>
<description>Aralia bastardiana Decne., since its written description in 1864 [as&#13;
Panax bastardianus (Decne.) Decne.] thought to be from Tahiti but never recollected&#13;
there, is considered almost certainly to have been collected in the&#13;
Marquesas. It is identical to Cheirodendron marquesense F. Brown, the name by&#13;
which the Marquesanpimata, the only species of the genus outside the Hawaiian&#13;
Islands, is usually known. A new combination, Cheirodendron bastardianum, is&#13;
therefore made. Spirally arranged leaves, seemingly exceptional in Cheirodendron&#13;
but depicted on the main shoot in Decaisne's illustration of Aralia bastardiana,&#13;
also occur in juvenile plants and on reversion shoots of Hawaiian species, at&#13;
least in C. trigynum subsp. helleri and C. platyphyllum subsp. kauaiense. A list&#13;
of localities and specimens seen of C. bastardianum is given.
</description>
<pubDate>Sun, 01 Jul 1990 00:00:00 GMT</pubDate>
<guid isPermaLink="false">http://hdl.handle.net/10125/1283</guid>
<dc:date>1990-07-01T00:00:00Z</dc:date>
<dc:creator>Frodin, DG</dc:creator>
</item>
<item>
<title>Chromosome Counts from the Flora of the Juan Fernandez Islands, Chile. III.</title>
<link>http://hdl.handle.net/10125/1282</link>
<description>Thirty-four chromosome counts are reported from populations&#13;
in 20 species from Masafuera in the Juan Fernandez Islands, Chile. New species&#13;
counts are in Abrotanella crassipes (2n = 18), Carpobrotus aequilaterus (n = 9),&#13;
Coprosma pyrifolia (n = 22), Drimys confertifolia (n = ca. 43), Euphrasia Jormosissima&#13;
(n = 44), Parietaria debilis (n = 8), and UrticaJernandeziana (n = ca.&#13;
11). A new chromosomal level for Hypochoeris glabra (n = 12) also is provided.&#13;
The taxonomic implications of certain of these counts are discussed. These data&#13;
help extend chromosomal information for endemic taxa of the archipelago as&#13;
part of broad evolutionary studies on the origin of the vascular plants. This study&#13;
again emphasizes the absence of aneuploid or euploid chromosomal alterations&#13;
during speciation within the archipelago.
</description>
<pubDate>Sun, 01 Jul 1990 00:00:00 GMT</pubDate>
<guid isPermaLink="false">http://hdl.handle.net/10125/1282</guid>
<dc:date>1990-07-01T00:00:00Z</dc:date>
<dc:creator>Sun, Byung Yun; Stuessay, Tod F; Crawford, Daniel J</dc:creator>
</item>
<item>
<title>First Central Pacific Plate and Hawaiian Record of the Deep-sea Tripod Fish Bathypterois grallator (Pisces: Chlorophthalmidae)</title>
<link>http://hdl.handle.net/10125/1281</link>
<description>Two species of tripod fish, Bathypterois grallator and B. cf. atricolor,&#13;
were observed in the Hawaiian Islands at depths of &gt; 1000 m during&#13;
submersible dives in May and July 1986. This is the first record of B. grallator&#13;
in the central Pacific Ocean.
</description>
<pubDate>Sun, 01 Jul 1990 00:00:00 GMT</pubDate>
<guid isPermaLink="false">http://hdl.handle.net/10125/1281</guid>
<dc:date>1990-07-01T00:00:00Z</dc:date>
<dc:creator>Jones, Anthony T; Sulak, kenneth J</dc:creator>
</item>
<item>
<title>Polychaeta from the Vicinity of Deep-sea Hydrothermal Vents in the Eastern Pacific. II. New Species and Records from the Juan de Fuca and Explorer Ridge Systems</title>
<link>http://hdl.handle.net/10125/1280</link>
<description>A total of 15 genera and species distributed in 10 families of&#13;
Polychaeta is reported from hydrothermal vent sites on the Juan de Fuca and&#13;
Explorer ridges off British Columbia and Washington. One genus and 10 species&#13;
are new to science. New taxa include Protomystides verenae (Phyllodocidae),&#13;
Nereis piscesae (Nereididae), Hesiodeira glabra and Amphiduros axialensis&#13;
(Hesionidae), Sphaerosyllis ridgensis (Syllidae), Ophryotrocha globopalpata and&#13;
Parougia wolji (Dorvilleidae), Orbiniella hobsonae and Leitoscoloplos pachybranchiatus&#13;
(Orbiniidae), and Nicomache venticola (Maldanidae). The hesionid&#13;
Hesiospina vestimentifera and the ampharetid Amphisamytha galapagensis,&#13;
previously reported from other eastern Pacific vent sites, are newly recorded. The&#13;
scalibregmatid Axiokebuita millsi, previously known from deep-sea locations in&#13;
the North Atlantic and Antarctic, is new to the northeastern Pacific. Additional&#13;
records of the recently described alvinellid, Paralvinella pandorae, are reported.
</description>
<pubDate>Sun, 01 Jul 1990 00:00:00 GMT</pubDate>
<guid isPermaLink="false">http://hdl.handle.net/10125/1280</guid>
<dc:date>1990-07-01T00:00:00Z</dc:date>
<dc:creator>Blake, James A; Hilbig, Brigitte</dc:creator>
</item>
<item>
<title>Elevated Carbon Dioxide Levels in Bayliss Cave, Australia: Implications for the Evolution of Obligate Cave Species</title>
<link>http://hdl.handle.net/10125/1279</link>
<description>In May and June 1985, the deeper passages of Bayliss Cave,&#13;
North Queensland, Australia, contained up to 200 times the ambient atmospheric&#13;
level of carbon dioxide and a water-saturated atmosphere, yet supported&#13;
the most diverse community of highly modified, obligate, terrestrial cave species&#13;
yet known. The obligate and facultative cave species were mostly segregated&#13;
by the environment, with the 24 obligate cave-adapted species being largely&#13;
restricted to the "bad-air" zone. The discovery of this previously unknown&#13;
"bad-air," obligate cave community corroborates other behavioral and distributional&#13;
studies that suggest that cave-adapted animals are specialized to exploit&#13;
resources within the smaller underground 'voids, where fluctuating carbon&#13;
dioxide concentrations are theoretically intolerable to most surface and facultative&#13;
cave species.
</description>
<pubDate>Sun, 01 Jul 1990 00:00:00 GMT</pubDate>
<guid isPermaLink="false">http://hdl.handle.net/10125/1279</guid>
<dc:date>1990-07-01T00:00:00Z</dc:date>
<dc:creator>Howarth, Francis G; Stone, Fred D</dc:creator>
</item>
<item>
<title>Geochemical Study of Fumarolic Condensates from Kilauea Volcano, Hawaii</title>
<link>http://hdl.handle.net/10125/1278</link>
<description>Results of a geochemical study based on 20 samples of condensates&#13;
obtained between late December 1987 and early January 1989 at five&#13;
fumarole sites on or near the summit of Kilauea Volcano, island of Hawaii, are&#13;
presented. Fumarole chemistry may be explicable in terms of the currently&#13;
accepted model of Kilauea and its mechanisms of magma replenishment and&#13;
storage, degassing, and eruptive activity; it may have potential for forecasting&#13;
eruptions. Fumaroles emit magmatic and recycled gases and aerosols that enter&#13;
into Earth's exchangeable reservoirs and which have a potentially harmful&#13;
impact on health and the environment through release of toxic materials and&#13;
creation of precipitation and vog of acidic character. Condensates from&#13;
fumaroles were analyzed by neutron activation/gamma-ray spectroscopy. Concentrations&#13;
of 28 elements are tabulated and statistically analyzed. Seven&#13;
elements (As, Ba, K, Sc, Se, V, and W) were in concentrations less than their&#13;
detection limits; 10 elements (Br, Cr, Cu, Eu, Fe, Hf, Mg, Sb, Sr, and Ti) were&#13;
below their detection limits in 75% or more of the samples; and II elements (AI,&#13;
Ca, Cl, Co, I, La, Mn, Na, S, V, and Zn) exhibited significant variation.&#13;
Individual fumaroles with distinctive ratios of elements and a high degree of&#13;
correlation between element pairs are identified.
</description>
<pubDate>Sun, 01 Jul 1990 00:00:00 GMT</pubDate>
<guid isPermaLink="false">http://hdl.handle.net/10125/1278</guid>
<dc:date>1990-07-01T00:00:00Z</dc:date>
<dc:creator>Barnard, Walther M; Halbig, Joseph B; Fountain, John C</dc:creator>
</item>
<item>
<title>44:2 Table of Contents - Pacific Science</title>
<link>http://hdl.handle.net/10125/1270</link>
<pubDate>Sun, 01 Apr 1990 00:00:00 GMT</pubDate>
<guid isPermaLink="false">http://hdl.handle.net/10125/1270</guid>
<dc:date>1990-04-01T00:00:00Z</dc:date>
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