http://hdl.handle.net/10125/3330 Mon, 20 May 2013 07:00:16 GMT 2013-05-20T07:00:16Z http://scholarspace.manoa.hawaii.edu:80/bitstream/id/13488/PacSci.jpg http://hdl.handle.net/10125/3330 http://hdl.handle.net/10125/7826 Sat, 01 Oct 1966 00:00:00 GMT http://hdl.handle.net/10125/7826 1966-10-01T00:00:00Z http://hdl.handle.net/10125/7825 Display racks built in 1909 to exhibit various woods grown in Hawaii provided some unique observations on dry-wood termite infections. Of 79 wood samples, including 76 species, 54 samples were not attacked. It is quite likely that this may be the only record of dry-wood termite resistance for many of these species. Sat, 01 Oct 1966 00:00:00 GMT http://hdl.handle.net/10125/7825 1966-10-01T00:00:00Z Boone, RS http://hdl.handle.net/10125/7824 The pattern noted for the various families was simple, showing one major protein band and, in most cases, at least one minor one. Serum from crabs from the open coast always showed two bands, while those from the mud flats showed but one. Th is held even in Pachygrapsus, which is found in both habitats. Sat, 01 Oct 1966 00:00:00 GMT http://hdl.handle.net/10125/7824 1966-10-01T00:00:00Z Hughes, Lawrence D; Winkler, Lindsay R http://hdl.handle.net/10125/7823 Sat, 01 Oct 1966 00:00:00 GMT http://hdl.handle.net/10125/7823 1966-10-01T00:00:00Z Higgins, Robert P http://hdl.handle.net/10125/7822 Sat, 01 Oct 1966 00:00:00 GMT http://hdl.handle.net/10125/7822 1966-10-01T00:00:00Z Murchison, AE; Magnuson, John J http://hdl.handle.net/10125/7821 Sat, 01 Oct 1966 00:00:00 GMT http://hdl.handle.net/10125/7821 1966-10-01T00:00:00Z Houng, KH; Uehara, G; Sherman, GD http://hdl.handle.net/10125/7820 The mineral taranakite was obtained in reactions between samples of an Akaka soil and monopotassium phosphate solutions ranging from 0.2 to 0.6 molar, at pH values of the reacting system ranging from 2.3 to 2.9. Characteristics of the reaction products were compared with those of pure synthetic taranakite, using X-ray, chemical, optical, infrared absorption, and differential thermal techniques. The taranakite was essentially a potassium-aluminum-phosphate complex. There was no indication of isomorphous substitution of iron for aluminum. The molar ratios of K/P04 and Al/P04 of the reaction product were found to be 0.37 and 0.72 respectively. The taranakite was thought to be formed by precipitation of a soluble phospho-alumino complex anion together with potassium ions. The possibility is suggested of the formation of taranakite when soluble potassium and phosphate react with Hydrol Humic and Humic Latosols in the field. During the early stages of reaction, the reaction product is believed to be cryptocrystalline, but the size of crystals increases with time. Sat, 01 Oct 1966 00:00:00 GMT http://hdl.handle.net/10125/7820 1966-10-01T00:00:00Z Liu, Po L; Sherman, GD; Swindale, LD http://hdl.handle.net/10125/7819 Sat, 01 Oct 1966 00:00:00 GMT http://hdl.handle.net/10125/7819 1966-10-01T00:00:00Z Arnold, BC http://hdl.handle.net/10125/7818 Sat, 01 Oct 1966 00:00:00 GMT http://hdl.handle.net/10125/7818 1966-10-01T00:00:00Z Heyligers, PC http://hdl.handle.net/10125/7812 Rectal temperatures of 23 species of Malaysian mammals were recorded during the course of an intensive mark-recapture program in rain forest. Repeated capture allowed repetitive readings for many individuals over several months. Individual variations and group comparisons are tabulated and discussed. Comparisons are made with body temperatures of arctic and temperate mammals. It was concluded that mean temperature for all tropical mammals described in this study was lower than in higher latitude forms, but that comparisons, to be meaningful, should be restricted to equivalent taxonomic groups. Sat, 01 Oct 1966 00:00:00 GMT http://hdl.handle.net/10125/7812 1966-10-01T00:00:00Z Rudd, Robert L http://hdl.handle.net/10125/7811 Sat, 01 Oct 1966 00:00:00 GMT http://hdl.handle.net/10125/7811 1966-10-01T00:00:00Z Tester, Albert L; Kato, Susumu http://hdl.handle.net/10125/7810 Sat, 01 Oct 1966 00:00:00 GMT http://hdl.handle.net/10125/7810 1966-10-01T00:00:00Z Russell, Eleanor http://hdl.handle.net/10125/7809 Young of Scomberomorus sierra are briefly described and compared with young of other scombroids and some other related families. At sizes of 30-50 mm of total length young S. sierra can be distinguished from S. concolor on the basis of gill raker counts. From this study, based on the collection of larvae and juveniles of S. sierra, it is evident that this species spawns near the coast over most of its distributional limits. Spawning off Mexico takes place in July through September and in lower latitudes from perhaps December through April. Sat, 01 Oct 1966 00:00:00 GMT http://hdl.handle.net/10125/7809 1966-10-01T00:00:00Z Klawe, WL http://hdl.handle.net/10125/7808 Sat, 01 Oct 1966 00:00:00 GMT http://hdl.handle.net/10125/7808 1966-10-01T00:00:00Z Wilson, Mildred S http://hdl.handle.net/10125/7807 Sat, 01 Oct 1966 00:00:00 GMT http://hdl.handle.net/10125/7807 1966-10-01T00:00:00Z Yamaguti, Satyu http://hdl.handle.net/10125/7806 Sat, 01 Oct 1966 00:00:00 GMT http://hdl.handle.net/10125/7806 1966-10-01T00:00:00Z Gosline, William A http://hdl.handle.net/10125/7805 Sat, 01 Oct 1966 00:00:00 GMT http://hdl.handle.net/10125/7805 1966-10-01T00:00:00Z Nelson, Gareth J http://hdl.handle.net/10125/7804 Sat, 01 Oct 1966 00:00:00 GMT http://hdl.handle.net/10125/7804 1966-10-01T00:00:00Z http://hdl.handle.net/10125/7770 Fri, 01 Jul 1966 00:00:00 GMT http://hdl.handle.net/10125/7770 1966-07-01T00:00:00Z Edmonds, SJ http://hdl.handle.net/10125/7769 Fri, 01 Jul 1966 00:00:00 GMT http://hdl.handle.net/10125/7769 1966-07-01T00:00:00Z Yaldwyn, John C