Herbivory patterns in mature sugar maple: variation with vertical canopy strata and tree ontogeny

1. Although leaf morphology and chemistry show profound changes as trees age, the consequences of such changes to herbivory have received little attention, particularly late in the ontogeny of canopy trees. 2. Using a mobile aerial lift for canopy access, patterns of leaf damage were evaluated in canopy‐dominant mature sugar maple (Acer saccharum Marsh) trees ranging from ～20 to 70 cm in diameter, corresponding to an age range of ～40–180 years. 3. Herbivore damage patterns varied in relation to both vertical canopy position (among upper‐, mid‐, and lower‐canopy positions) and with tree size. Damage types attributable to herbivores active on leaf surfaces, including leaf skeletonizers and leaf cutters (both principally Lepidoptera), and leaf stippling inducers (Hemiptera) showed decreases with tree size, and with increasing height in the canopy. In contrast, leaf damage from the most abundant gall‐forming arthropod in the system, the eriophyid mite Vasates aceriscrumena, increased markedly with tree size. 4. The results indicate that herbivory patterns vary with both canopy stratum and with tree size in sugar maple, and that the relative strength of vertical stratification and tree ontogeny effects are similar in magnitude. The predominant patterns are of a decrease in herbivory with increasing height in the canopy and with tree size, but certain galling arthropods exhibit the reverse trends.     

The Indomitable Miss Pink: A Life in Anthropology

The Indomitable Miss Pink:. Life in Anthropology. Julie Marcus. Sydney: University of New South Wales Press, 2001. 340 pp.     

Biogeographic mirages? Molecular evidence for dispersal‐driven evolution in Hydrobiusini water scavenger beetles

Water beetles of the tribe Hydrobiusini are globally distributed in the northern hemisphere and all austral continents except Antarctica. A remarkable clade also occurs in the Hawaiian Islands. The phylogenetic relationships among genera were recently investigated using a combination of molecules and morphology. Here, we use this phylogenetic framework to address the biogeographic evolution of this group using Bayesian fossil‐based divergence times, and model‐based maximum likelihood ancestral range estimations. We recover an origin of the tribe in the Cretaceous ca. 100 Ma. Our biogeographic analyses support an origin of the tribe in Laurasia followed by the colonization of Australia. However, a Gondwanan origin of the group cannot be ruled out when considering the fossil record. The timeframe of the tribe's evolution as well as the model‐based approach of ancestral range estimation favour a scenario invoking multiple transoceanic dispersal events over a Gondwana vicariance hypothesis. The Hawaiian radiation originated from long‐distance dispersal to now‐submerged islands, paired with dispersal to new islands as they formed.     

Climate and CO2 controls on global vegetation distribution at the last glacial maximum: analysis based on palaeovegetation data, biome modelling and palaeoclimate simulations

The global vegetation response to climate and atmospheric CO₂ changes between the last glacial maximum and recent times is examined using an equilibrium vegetation model (BIOME4), driven by output from 17 climate simulations from the Palaeoclimate Modelling Intercomparison Project. Features common to all of the simulations include expansion of treeless vegetation in high northern latitudes; southward displacement and fragmentation of boreal and temperate forests; and expansion of drought‐tolerant biomes in the tropics. These features are broadly consistent with pollen‐based reconstructions of vegetation distribution at the last glacial maximum. Glacial vegetation in high latitudes reflects cold and dry conditions due to the low CO₂ concentration and the presence of large continental ice sheets. The extent of drought‐tolerant vegetation in tropical and subtropical latitudes reflects a generally drier low‐latitude climate. Comparisons of the observations with BIOME4 simulations, with and without consideration of the direct physiological effect of CO₂ concentration on C₃ photosynthesis, suggest an important additional role of low CO₂ concentration in restricting the extent of forests, especially in the tropics. Global forest cover was overestimated by all models when climate change alone was used to drive BIOME4, and estimated more accurately when physiological effects of CO₂ concentration were included. This result suggests that both CO₂ effects and climate effects were important in determining glacial‐interglacial changes in vegetation. More realistic simulations of glacial vegetation and climate will need to take into account the feedback effects of these structural and physiological changes on the climate.     

People Out of Place: Unquiet Immigrants

Legalizing Moves: Salvadoran Immigrants' Struggle for U.S. Residency . Susan Bibler Coutin. Ann Arbor: University of Michigan Press, 2003. 228 pp.
The Maya of Morganton: Work and Community in the Nuevo New South . Leon Fink. Chapel Hill: University of North Carolina Press, 2003. 254 pp.
The Children of NAFTA: Labor Wars on the U.S./Mexico Border . David Bacon. Berkeley: University of California Press, 2004. 348 pp.