Pacific Science Volume 46, Number 2, 1992

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Pacific Science is a quarterly publication devoted to the biological and physical sciences of the Pacific Region.


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    Altitudinal Change in Plant Endemism, Species Turnover, and Diversity on Isla Santa Cruz, the Galapagos Islands
    (University of Hawai'i Press, 1992-04) Itow, Syuzo
    Vegetation zones of Isla Santa Cruz in the Galapagos Islands range from the lowland dry zone, through transition and moist zones, to the highland zone, reflecting the precipitation pattern. The zones are deflected upward on the leeward north side, as compared with the windward south side. The brown subzone and Miconia robinsoniana scrub of the moist zone are absent on the north side. Zonation and species distribution patterns are also related to altitude and substrate. Floristic and phytosociological endemisms for woody species increase with higher altitude, while those of herbaceous species are low in high elevations because of low endemism in pteridophytes. Species turnover rate along the altitudinal gradient is three times higher on the windward south side than on the leeward north side. Species diversity is low in Scalesia pedunculata forest, where stand-level dieback has occurred as a consequence of the species-poor constitution.
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    Biogeography of the Tropical Pacific
    (University of Hawai'i Press, 1992-04) Stoddart, D.R.
    Many previous biogeographic regionalizations of the islands and reefs of the tropical Pacific are unsatisfactory: the regions as defined are heterogeneous, localities with unlike biotas are grouped together, and those with similar characteristics are placed in separate categories. Often distinctions appear to be based on cultural or political rather than biogeographic considerations. Criteria are defined for the establishment of biogeographic boundaries. Instead of the hierarchical schemes often utilized, it is proposed that the basis of biogeographic regionalization be typological. A distinction is made between the biogeographic characteristics of atolls and other reef islands, elevated limestone (makatea) islands, and high (often volcanic) islands. It is concluded that if the first two categories are filtered out, the treatment of the biogeography of the third group and hence the regionalization of the Pacific becomes relatively unproblematical.
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    Vegetation of the Society Islands
    (University of Hawai'i Press, 1992-04) Fosberg, F Raymond
    The vegetation of the Society Islands, 16°-18° south of the equator, in the wet SE trade wind belt, is described. The flora is primarily of Indo-Malayan derivation with a few New Zealand, Australian, American, and Hawaiian elements. There is little doubt that the volcanic islands at the time of human arrival, perhaps 4000 yr ago, were forested from mountaintop to seashore. The original vegetation consisted of broad-leaved, usually hygrophilous, montane rainforest. There was an abundance of shrub and small tree species, and terrestrial ferns dominated the ground layer. The sequence of vegetation from forest on the coastal zone and in deep valley bottoms through montane rainforest, mossy or cloud forest, and mossy scrub-covered crests and peaks is distinguished. With the arrival of the Polynesians, nonindigenous plant species were introduced for food, medicine, and fiber,and "camp followers" arrived accidentally. Native species, especially in the lowland coastal zone, were replaced with coconut groves; taro marshes; and valley-bottom forests of mape, breadfruit, and bamboo. The advent of Europeans brought further, often disastrous, change as newly introduced goats and pigs and logging and clearing opened up originally closed formations. Exotic species such as mango and guava came to dominate the vegetation in some places. The flora of the five atolls and the barrier-reef islets is essentially that of strand habitats throughout the Indo-Pacific and is impoverished. There was a mixed broad-leaved forest of several common widespread strand species such as Pisonia, Guettarda, Pandanus, etc., and the halophytic Tournefortia and Scaevola toward the seaward periphery. The original vegetation has also been changed by human activity, replaced by coconut and breadfruit groves and, in wet places, by taro pits. The vegetation patterns of the individual islands are also described.
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    Disjunction of Tree Species in Mountain Forests, Southern North Island, New Zealand: A Review of Paleobotanical Evidence
    (University of Hawai'i Press, 1992-04) McQueen, D.R.
    Dominant trees of New Zealand forests, particularly Nothofagus, which has low seed mobility, show major distribution gaps, associated with past glacial and volcanic destruction of forest. In the southern North Island there are forest tree discontinuities distant from volcanic destruction and subject only to periglacial activity in the Pleistocene. Here there is absence of one taxon of Nothofagus and of some mountain coniferous trees, including podocarps, with bird-carried seeds, and Libocedrus, with winged seeds. The southern North Island, from 40° S to 41 ° 30' S, shows a progressive southward loss in montane and subalpine tree species. These species are common, often dominant, to the north of the area described, and in the northern South Island. In order of increasingly southern limits in the North Island they are Halocarpus bidwillii, Nothofagus solandri var. cliffortioides, Libocedrus bidwillii, Halocarpus biformis, and Phyllocladus alpinus. Their pollen and macrofossil history is reviewed. Libocedrus bidwillii was present in the southern North Island 80,000 yr ago, and Halocarpus and P. alpinus until ca. 10,000 yr ago. Various glacial episodes since 80,000 yr ago have severely limited their distribution. The postglacial reoccupation by forest of southern North Island sites was influenced by rapid climatic warming. This warming not only flooded the Cook Strait landbridge, cutting off tree migration from the south, but also allowed lowlands around the gorge bisecting the axial mountains to be occupied by temperate forest, effectively blocking access southward by L. bidwillii and N. solandri var. cliffortioides. The mountain podocarps, H. biformis and P. alpinus, now abundant just south of the gorge, are in a particularly cloudy climate, which lacks Nothofagus. Farther south, under less cloudy conditions, the rapid expansion of N. menziesii forest from lowland refugia could have excluded the two small podocarps, which were present in pollen records in the early postglacial.
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    Distributional Dynamics in the Hawaiian Vegetation
    (University of Hawai'i Press, 1992-04) Mueller-Dombois, Dieter
    Vegetation ecology is usually divided into two broad research areas, floristic/environmental gradient analysis and studies of vegetation dynamics. The early influential American ecologist Clements combined the two areas into a dynamic system for classifying vegetation. His succession and climax theory, however, was later severely criticized. A new approach to the study of distributional dynamics, called "landscape ecology," focuses on the dynamics of spatial vegetation patterns. There is a spatial hierarchy rule, which implies greater stability of species and community patterns when one considers larger area units versus smaller ones. It is argued that this rule is frequently transgressed in biotically impoverished areas, like the Hawaiian Islands, where certain dominant plant species have become established over unusually broad areas and habitat spectra. A further point made is that with "species packing" successional patterns change from auto-succession, where the dominant species retains dominance by in situ generation turnover (termed chronosequential monoculture), via "normal" succession (i.e., displacement of dominants by other dominants over time [termed chronosequential polyculture]), to small-area patch or gap dynamics (termed chronosequential gap rotation). Examples of the three spatially different succession paradigms are given for Hawaii, and the point is made that chronosequential monocultures cannot be expected to last, but change to chronosequential gap rotation with the invasion of alien dominants. Before the invasion of alien dominants, certain native dominants seem to have segregated into races or varieties by evolutionary adaptation to successional habitats. Finally, the concept of climax is discussed as having two meanings: (I) permanency of community type, which can only be observed for the aggregate assemblage of smaller communities in a larger space, such as occupied by a biome; (2) the mode of organic production in ecosystem development. The mode seems to occur between 1000 and 3000 yr in the Hawaiian rainforest biome on volcanic soils. Thereafter, productivity declines with acidification and soil nutrient impoverishment over a million years and more. This amounts to a retrogression in the course of primary succession.
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