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Galapagos Islands

Fig. 6.1 Location of the Galapagos Islands in relation to the South American mainland. The darkened island is Albermerle, Isla Isabela, in the Ecuadorian system... Fig. 6.1 Location of the Galapagos Islands in relation to the South American mainland. The darkened island is Albermerle, Isla Isabela, in the Ecuadorian system...
The existence of a species of tomato on the Galapagos Islands was first noted by Charles Darwin. Despite a moderate level of variation, Lycopersicon cheesmanii Riley is considered the only tomato species on the islands. All populations examined exhibited morphological and physiological characteristics that clearly... [Pg.248]

Adersen, A., Adersen, H. and Brimer, L. 1988. Cyanogeiric constituents in plants from the Galapagos Islands. Biochem. Syst. Ecol. 16 65-77. [Pg.301]

Corkill, L. 1942. The inheritance of cyanogenesis. N. Z. J. Sci. Tech., Series B 23 178-193. Cowlishaw, M. G., Bickerstaffe, R. and Connor, H. E. 1983. Intraspecific variation in the epicu-ticular wax composition of four species of Chionochloa. Biochem. Syst. Ecol. 11 247-259. Cox, A. 1983. Ages of the Galapagos Islands. Pages 11-23 in R. I. Bowman, M. Berson and A. E. Leviton (eds.) Patterns of Evolution in Galapagos Organisms. AAAS, Pacific Division. San Francisco. [Pg.308]

Lawesson J. E. 1988. Contributions to the flora of the Galapagos Islands, Ecuador. Phytologia 65 228-230. [Pg.319]

Wendel, J. F. and Percy, R. G. 1991. Allozyme diversity and introgression in the Galapagos Islands endemic Gossypium darwinii and its relationship to continental G. barbadense. Biochem. Syst. Ecol. 18 517-528. [Pg.334]

Wessels, P. L., Holzapfel, C. W., van Wyk, B.-E. and Marais, W. 1996. Plicataloside, an 0-0-diglucosylated naphthalene derivative from Aloe plicatilis. Phytochemistry 41 1547-1551. Whittaker, R. H. 1961. Comments on the Klamath region and conifer diversity. Madrono 16 5. Wiggins, I. L. 1971. Flora of the Galapagos Islands. I. L. Wiggins and D. M. Porter (eds.) Stanford University Press, Stanford, CA. [Pg.334]

Some ridge sections are underlain by mantle melt anomalies, or hot spots, such as at the Azores and Galapagos Islands. These are marked by the stars in Figure 19.1 and data points 12 and 13 in Figure 19.5. Mantle upwelhng beneath both these ridge sections has abnormally thickened the oceanic crust to at least about 10 km. Most of the 47 known hot spots lie more than 500 km from a ridge axis. The Hawaiian islands are a notable example. [Pg.477]

Kruska, D. and Rohrs, M. (1974). Comparative-quantitative investigations on brains of feral pigs from the Galapagos Islands and of European domestic pigs. Zeitschriftfur AnatomieundEntwicklungsgeschichte 144,61-73. [Pg.479]

Report existing knowledge/facts Present-active Nitrite reductases catalyze the one-electron reduction of nitrite. (From Houser, 2001) The Galapagos Islands sit on a large volcanic platform in the Pacific Ocean. (From Harpp, 1998)... [Pg.419]

Formation mechanisms. How are the northern Galapagos Islands and seamounts related to the plume and the ridge Is the WDL a channel to the ridge from the plume. [Pg.463]

Roque-Albelo, L. (2000). The tiger moths (Arctiidae) of the Galapagos Islands, their biogeography and life history. In Proceedings of the Annual Meeting of the Lepidopterists Society, Wake Forest University, Winston-Salem, July 2000. [Pg.280]

Around deep-sea vents lives a very interesting species of animal the tubeworm. Some tubeworms can grow to be almost 8 feet (3 m) long. They were first discovered in the 1970s around some hydrothermal vents near the Galapagos Islands off the coast of South America. Since then many tubeworms have been found at deep-sea vents all over the world. [Pg.71]

Chapman, R.F., Espelie, K.E. and Peck, S.B. (2000). Cuticular hydrocarbons of grasshoppers from the Galapagos Islands, Ecuador. Biochem. Syst. Ecol., 28, 579-588. [Pg.151]

Cox, A., and G.B.Dalrymple Palaeomagnetism and Potassium-Argon Ages of Some Volcanic Rocks from the Galapagos Islands. Nature 209, 776 (1966). [Pg.71]

When Charles Darwin was climbing the rocks of the Galapagos Islands—pursuing the finches that would eventually bear his name—he must have cut his finger occasionally or scraped a knee. Young adventurer that he was, he probably paid no attention to the little stream of blood trickling out. Pain was a fact of life to the intrepid island explorer, and it had to be borne patiently if any work were to get done. [Pg.77]

An examination of Figure 6 also illustrates other problems with marine shell samples. Four samples from the environment of the Galapagos Islands ranged from a little more than —4.0% to a little less than +0.5%. This equates to an apparent variation of ca. 850 years between... [Pg.51]

Jimenez, R. (1981). Composition and distribution of phytoplankton in the upweUing system of the Galapagos Islands. In Coastal UpweUing. (Richards, F. A., ed.). American Geophysical Union, pp. 327-338. [Pg.802]

Koutavas A., Lynch-Stieglitz J., Marchitto T. M. J., and Sachs J. P. (2002) Deglacial and Holocene climate record from the Galapagos Islands El Nino linked to Ice Age climate. Science 297(5579), 226-230. [Pg.3234]

Propylene has the same general characteristics found for the other hydrocarbons. Leg I concentrations vary from 3.43 0.49 X 10 ml/l near the Galapagos Islands to 0.59 0.07 X 10" ml/l for an area located s 1500 miles southeast of Hawaii. Leg II exhibits what appears to be a... [Pg.168]

Ethane concentrations exhibit the same type of relative constancy as methane. The only variable and high concentrations (relative to open ocean values) of 0.50 X 10 ml/1 are found near the Galapagos Islands and Ecuador. There is good agreement between the average concentration found in 1972 ( 0.20 X 10" ml/1.) and 1974 (0.28 X 10 ml/L). [Pg.170]


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See also in sourсe #XX -- [ Pg.196 , Pg.214 , Pg.259 ]

See also in sourсe #XX -- [ Pg.30 ]




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The Galapagos Islands

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