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<title>Pacific Science Volume 46, Number 3, 1992</title>
<link>http://hdl.handle.net/10125/627</link>
<description/>
<pubDate>Thu, 23 May 2013 15:52:48 GMT</pubDate>
<dc:date>2013-05-23T15:52:48Z</dc:date>
<item>
<title>46:3 Table of Contents - Pacific Science</title>
<link>http://hdl.handle.net/10125/1417</link>
<pubDate>Wed, 01 Jul 1992 00:00:00 GMT</pubDate>
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<dc:date>1992-07-01T00:00:00Z</dc:date>
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<item>
<title>The Impact of Alien Species on Island Ecosystems: Extended Abstracts of a Symposium, 30 May 1991, Honolulu, Hawaii, XVII Pacific Science Congress</title>
<link>http://hdl.handle.net/10125/1416</link>
<pubDate>Wed, 01 Jul 1992 00:00:00 GMT</pubDate>
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<dc:date>1992-07-01T00:00:00Z</dc:date>
<dc:creator>Cowie, Robert H</dc:creator>
</item>
<item>
<title>Coral Reefs and Environmental Change-The Next 100 Years: A Synopsis and Abstracts of Papers Presented at a Symposium of the XVII Pacific Science Congress</title>
<link>http://hdl.handle.net/10125/1415</link>
<pubDate>Wed, 01 Jul 1992 00:00:00 GMT</pubDate>
<guid isPermaLink="false">http://hdl.handle.net/10125/1415</guid>
<dc:date>1992-07-01T00:00:00Z</dc:date>
<dc:creator>Grigg, Richard W</dc:creator>
</item>
<item>
<title>Simulation of Organic Chemical Movement in Hawaii Soils with PRZM: 3. Calibration</title>
<link>http://hdl.handle.net/10125/1414</link>
<description>his is the third and final part of a multipart paper reporting&#13;
testing of the EPA's Pesticide Root Zone Model (PRZM) using data from&#13;
Hawaii. PRZM is a dynamic-conceptual pesticide leaching model. In the first&#13;
and second parts of the paper results were reported for predicted pesticide&#13;
movement based upon preliminary PRZM simulations. In this part of the paper&#13;
a trial-and-error calibration of PRZM is reported for a site in Hawaii.&#13;
Performance results from the model calibration exercise are quite poor, illustrating&#13;
the need for multicriteria evaluation procedures.
</description>
<pubDate>Wed, 01 Jul 1992 00:00:00 GMT</pubDate>
<guid isPermaLink="false">http://hdl.handle.net/10125/1414</guid>
<dc:date>1992-07-01T00:00:00Z</dc:date>
<dc:creator>Loague, Keith</dc:creator>
</item>
<item>
<title>Naso caesius, a New Acanthurid Fish from the Central Pacific</title>
<link>http://hdl.handle.net/10125/1413</link>
<description>Naso caesius, a new unicornfish (Perciformes: Acanthuridae:&#13;
Nasinae) is described from specimens from the Marshall Island s, Mariana&#13;
Island s, Hawaiian Islands, and Pitcairn Group. Its occurrence in the Society&#13;
Island s, New Caledonia, Fiji, and the Coral Sea is confirmed by underwater&#13;
photographs. It is very similar to and has been confused with Naso hexacanthus,&#13;
differing in having sma11er bladelike caudal spines that do not become sharply&#13;
pointed and antrorse as on large male N. hexacanthus, a pale instead of black&#13;
tongue, entirely pale lower-limb gill rakers (base of rakers blackish in N.&#13;
hexacanthus), and in life color. It is bluish gray overa11 (not yellowish ventra11y&#13;
as on N. hexacanthus) and lacks the black borders on the opercle and preopercle&#13;
and the white lower lip usua11y seen on N. hexacanthus ;one common color phase,&#13;
which can be rapidly assumed, has vertically elongate spots on the body that&#13;
vary from paler to darker than the ground color. Naso thorpei Smith, known&#13;
from one 314-mm specimen from Durban, South Africa, is questionably distinct&#13;
from N. hexacanthus. Naso tapeinosoma (Bleeker) and N. vomer (Klunzinger)&#13;
are probable junior synonyms of N. hexacanthus.
</description>
<pubDate>Wed, 01 Jul 1992 00:00:00 GMT</pubDate>
<guid isPermaLink="false">http://hdl.handle.net/10125/1413</guid>
<dc:date>1992-07-01T00:00:00Z</dc:date>
<dc:creator>Randall, John E; Bell, Lori J</dc:creator>
</item>
<item>
<title>Egg Abundance and Spawning Biomass of the Hawaiian Anchovy or Nehu, Encrasicholinapurpurea, during 1984-1988 in Kaneohe Bay, Hawaii</title>
<link>http://hdl.handle.net/10125/1412</link>
<description>In Kaneohe Bay, Hawaii, nehu (Hawaiian anchovy, Encrasicholina&#13;
purpurea) eggs were found primarily in areas where water depth was&#13;
&gt; 10-12 m and were infrequently encountered near reefs, shorelines, or other&#13;
shallow areas. Eggs were usually most abundant near the centers of one or both&#13;
of the two large basins; the more enclosed southern basin usually accounted for&#13;
the majority of the total eggs present. Nehu eggs were present throughout the&#13;
year, but abundance was usually higher between July and February or March.&#13;
There was considerable shorter time-scale variation in egg abundance, but there&#13;
was no apparent underlying periodicity other than the annual cycle. Egg&#13;
abundance was poorly correlated with measured environmental factors; the only&#13;
potential relationship was that abundance tended to be low during the season&#13;
of strong northeast trade winds. Egg abundance in Kaneohe Bay was poorly&#13;
correlated with abundance in Pearl Harbor, Hawaii, the other major area where&#13;
nehu are found. Total numbers of eggs present in Kaneohe Bay reached about&#13;
109 during peaks. Based on available knowledge of nehu fecundity, spawning&#13;
frequency, and sex ratio, the biomass of spawning females was about 2 t and&#13;
that of all adults about 8 t during peaks of egg abundance. Catches of nehu by&#13;
the skipjack tuna baitfishery were poorly correlated with estimates of adult&#13;
standing crop, and most variation in catch was attributed to variation in effort.&#13;
Annual catches, however, were about five times the highest estimates of adult&#13;
biomass, and several monthly catches exceeded 8 t. The results indicate that&#13;
postmetamorphic nehu move into and out of and perhaps between spawning&#13;
and nursery areas such as Kaneohe Bay and that the total population is much&#13;
larger than that present in enclosed areas at any given time. Consequently,&#13;
further studies of the population dynamics of nehu and their interaction with&#13;
the fishery should be conducted on an island-wide and probably archipelagowide&#13;
basis.
</description>
<pubDate>Wed, 01 Jul 1992 00:00:00 GMT</pubDate>
<guid isPermaLink="false">http://hdl.handle.net/10125/1412</guid>
<dc:date>1992-07-01T00:00:00Z</dc:date>
<dc:creator>Clarke, Thomas A</dc:creator>
</item>
<item>
<title>Changing Photosynthetic Capacity during Leaf Ontogeny in Juvenile and Mature Metrosideros polymorpha Trees</title>
<link>http://hdl.handle.net/10125/1411</link>
<description>Net CO2 uptake at light saturation (Pmax) was measured (both&#13;
area and weight basis) for leaves of four categories based on leaf age and branch&#13;
position in juvenile and mature trees of Metrosideros polymorpha, a tropical,&#13;
dicot evergreen species. Conductance, weight /area, and Nand P concentrations&#13;
were also measured. In both juvenile and mature trees, Pmax was higher in&#13;
terminal leaves 6-14 months old than in younger or older leaves. Low Pmax of&#13;
leaves less than 6 months old was related to factors of immaturity, including low&#13;
weight /area and low N concentration. Low Pmax of older and subterminal leaves&#13;
was correlated with low N concentration related to withdrawal during leaf aging.&#13;
This correlation was stronger in mature than in juvenile trees. Pmax was&#13;
significantly lower, and nitrogen concentration and specific leaf weight were&#13;
higher, in the sample of mature trees than in the juvenile tree sample (Pmax&#13;
5.89 and 4.99 molm- 2 S- 1 in juvenile and mature trees, respectively).
</description>
<pubDate>Wed, 01 Jul 1992 00:00:00 GMT</pubDate>
<guid isPermaLink="false">http://hdl.handle.net/10125/1411</guid>
<dc:date>1992-07-01T00:00:00Z</dc:date>
<dc:creator>Gerrish, Grant</dc:creator>
</item>
<item>
<title>Population Size and Frequency of Branching in the Eke Silversword, Argyrox iphium caliginis (Asteraceae), on Eke Crater, West Maui, Hawaii.</title>
<link>http://hdl.handle.net/10125/1410</link>
<description>The Eke silversword, Argyroxiphium caliginis, is a rosette plant&#13;
endemic to the summit bogs of Eke Crater and Puu Kukui, West Maui, Hawaii.&#13;
On 2 November 1985, a belt transect across Eke Crater was used to estimate the&#13;
population of silverswords on the summit bog. Total population of the Eke&#13;
silversword on Eke Crater was estimated to be about 76,000 plants. Although the&#13;
plant has been described as a branching shrub that reproduces vegetatively, the&#13;
majority of the individuals in the sampled population of the Eke silversword on&#13;
Eke Crater were unbranched, monocarpic plants that appeared to reproduce by&#13;
seed.
</description>
<pubDate>Wed, 01 Jul 1992 00:00:00 GMT</pubDate>
<guid isPermaLink="false">http://hdl.handle.net/10125/1410</guid>
<dc:date>1992-07-01T00:00:00Z</dc:date>
<dc:creator>Powell, Elizabeth Ann</dc:creator>
</item>
<item>
<title>Hawaiian Quaternary Paleoenvironments: A Review of Geological, Pedological, and Botanical Evidence.</title>
<link>http://hdl.handle.net/10125/1409</link>
<description>Climates in Hawaii during glacial periods were relatively wetter&#13;
and cooler than interglacial climates. Eolian deposits indicate that northeasterly&#13;
trade winds predominated during glacial periods. Orographic rainfall patterns&#13;
were probably similar to those of today except that they were shifted downward&#13;
in response to lowered sea levels and a depressed inversion level. Botanical&#13;
evidence indicates that some areas probably received more than double their&#13;
current annual rainfall. Greater rainfall during glacial periods was probably&#13;
responsible for the formation of highly weathered soils that are now in semiarid&#13;
climates. More intense periglacial processes may have operated during glacial&#13;
periods. Snowline on Mauna Kea was depressed about 900 m and glaciation&#13;
may have occurred because of lower air temperature and greater cloudiness.&#13;
Ocean temperature was probably also slightly cooler. At low elevations,&#13;
interglacial climates were drier than glacial climates because of the influence&#13;
higher sea levels had on orographic rainfall distribution. Trade winds still&#13;
predominated but the inversion level was higher, which may have caused greater&#13;
rainfall at high elevations. Pedological evidence indicates a highly erosive&#13;
environment before the formation of the Kaena shoreline at about 650,000 yr&#13;
ago. Climatic conditions at that time are not known. Subsequent environmental&#13;
conditions have not been as conducive to erosion, and the past several hundred&#13;
thousand years have witnessed relative landscape stability.
</description>
<pubDate>Wed, 01 Jul 1992 00:00:00 GMT</pubDate>
<guid isPermaLink="false">http://hdl.handle.net/10125/1409</guid>
<dc:date>1992-07-01T00:00:00Z</dc:date>
<dc:creator>Gavenda, Robert T</dc:creator>
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