Review of the Australian endemic genus Tasmosalpingus Lea, 1919 (Coleoptera, Cucujoidea, Tasmosalpingidae).

The sole genus of the Australian endemic family Tasmosalpingidae, Tasmosalpingus Lea, 1919, is revised and T. promiscuus Lea, 1919 is proposed as a junior synonym of T. quadrispilotus Lea, 1919. T. magnus sp. nov. is described from New South Wales and Victoria, representing the northernmost distribution of this family. A predicted distribution of the genus is given, and the relationships between Tasmosalpingidae, Cyclaxyridae and Lamingtoniidae are discussed.

Extinct before discovered? Epactoidesgiganteus sp. nov. (Coleoptera, Scarabaeidae, Scarabaeinae), the first native dung beetle to Réunion island.

We describe a new species of dung beetle, Epactoidesgiganteus sp. nov., from a single female specimen allegedly collected in the 19th century on Réunion island and recently found at the Muséum national d'Histoire naturelle, Paris. This species differs from other species of Epactoides by larger size and a set of other distinctive morphological characters. Epactoidesgiganteus sp. nov. is the first native dung beetle (Scarabaeinae) of Réunion, and its discovery expands the known area of distribution of the genus Epactoides, which was hitherto believed to be endemic to Madagascar. Like other taxa from Madagascar and peripheral islands (e.g., Comoro, Seychelles, Mascarenes), E.giganteus sp. nov. may have reached Réunion by over-water dispersal. Given the rapid loss of biodiversity on Réunion island and the fact that no additional specimens were re-collected over the last two centuries, it is very likely that E.giganteus sp. nov. has gone extinct. However, we have unconfirmed evidence that the holotype of E.giganteus sp. nov. might be a mislabeled specimen from Madagascar, which would refute the presence of native dung beetles on Réunion. We discuss both hypotheses about the specimen origin and assess the systematic position of E.giganteus sp. nov. by examining most of the described species of Madagascan Epactoides. Additionally, we provide a brief overview of the dung beetle fauna of Mascarene Archipelago.

Early tropical crop production in marginal subtropical and temperate Polynesia.

Polynesians introduced the tropical crop taro (Colocasia esculenta) to temperate New Zealand after 1280 CE, but evidence for its cultivation is limited. This contrasts with the abundant evidence for big game hunting, raising longstanding questions of the initial economic and ecological importance of crop production. Here we compare fossil data from wetland sedimentary deposits indicative of taro and leaf vegetable (including Sonchus and Rorippa spp.) cultivation from Ahuahu, a northern New Zealand offshore island, with Raivavae and Rapa, both subtropical islands in French Polynesia. Preservation of taro pollen on all islands between 1300 CE and 1550 CE indicates perennial cultivation over multiple growing seasons, as plants rarely flower when frequently harvested. The pollen cooccurs with previously undetected fossil remains of extinct trees, as well as many weeds and commensal invertebrates common to tropical Polynesian gardens. Sedimentary charcoal and charred plant remains show that fire use rapidly reduced forest cover, particularly on Ahuahu. Fires were less frequent by 1500 CE on all islands as forest cover diminished, and short-lived plants increased, indicating higher-intensity production. The northern offshore islands of New Zealand were likely preferred sites for early gardens where taro production was briefly attempted, before being supplanted by sweet potato (Ipomoea batatas), a more temperate climate-adapted crop, which was later established in large-scale cultivation systems on the mainland after 1500 CE.

Phylogeny of the beetle supertribe Trechitae (Coleoptera: Carabidae): Unexpected clades, isolated lineages, and morphological convergence.

Using data from two nuclear ribosomal genes and four nuclear protein-coding genes, we infer a well-resolved phylogeny of major lineages of the carabid beetle supertribe Trechitae, based upon a sampling of 259 species. Patrobini is the sister group of Trechitae, but the genus Lissopogonus appears to be outside of the Patrobini + Trechitae clade. We find that four enigmatic trechite genera from the Southern Hemisphere, Bembidarenas, Argentinatachoides, Andinodontis, and Tasmanitachoides, form a clade that is the sister group of Trechini; we describe this clade as a new tribe, Bembidarenini. Bembidarenini + Trechini form the sister group of remaining trechites. Within Trechini, subtribe Trechodina is not monophyletic, as three trechodine genera from Australia (Trechobembix, Paratrechodes, Cyphotrechodes) are the sister group of subtribe Trechina. Trechini appears to have originated in the continents of the Southern Hemisphere, with almost all Northern Hemisphere lineages representing a single radiation within the subtribe Trechina. We present moderate evidence that the geographically and phylogenetically isolated genera Sinozolus (six species in the mountains of China), Chaltenia (one species in Argentina and Chile), and Phrypeus (one species in western North America) also form a clade, the tribe Sinozolini. The traditionally recognized tribe Bembidiini sens. lat., diagnosed by the presence of a subulate terminal palpomere, is shown to be polyphyletic; subulate palpomeres have arisen five times within Trechitae. Anillini is monophyletic, and the sister group of Tachyini + Pogonini + Bembidiini + Zolini + Sinozolini; within anillines, we confirm earlier results indicating the eyed New Zealand genus Nesamblyops as the sister to the rest. Sampled New World Pogonini are monophyletic, rendering the genus Pogonus non-monophyletic. Tachyina and Xystosomina are sister groups. Within Xystosomina, the New World members are monophyletic, and are sister to an Australia-New Zealand clade. The latter consists of the genus Philipis as well as taxa not previously recognized as xystosomines: Kiwitachys, the "Tachys" ectromioides group, and "Tachys" mulwalensis. Within Tachyina, the subgenus Elaphropus is not closely related to other subgenera previously placed in the genus Elaphropus; we move the other subgenera into the genus Tachyura. Tachyina with a bifoveate mentum do not form a clade; in fact, a bifoveate mentum is found in Xystosomina, Sinozolini, Trechini, Trechitae and its sister group, Patrobini. Extensive homoplasy in the morphological characters previously used as key indicators of relationship is supported by our results: in addition to multiple origins of subulate palpomeres and bifoveate menta, a concave protibial notch has arisen independently in Anillina, Xystosomina, and Tachyina. Phylogenetically and geographically isolated, species-poor lineages in Trechini, Bembidarenini, and Sinozolini may be relicts of more widespread faunas; many of these are found today on gravel or sand shores of creeks and rivers, which may be an ancestral habitat for portions of Trechitae. In addition to the description of Bembidarenini, we present a diagnosis of the newly delimited Sinozolini, and keys to the tribes of Trechitae.

The Early Shorebird Will Catch Fewer Invertebrates on Trampled Sandy Beaches.

Many species of birds breeding on ocean beaches and in coastal dunes are of global conservation concern. Most of these species rely on invertebrates (e.g. insects, small crustaceans) as an irreplaceable food source, foraging primarily around the strandline on the upper beach near the dunes. Sandy beaches are also prime sites for human recreation, which impacts these food resources via negative trampling effects. We quantified acute trampling impacts on assemblages of upper shore invertebrates in a controlled experiment over a range of foot traffic intensities (up to 56 steps per square metre) on a temperate beach in Victoria, Australia. Trampling significantly altered assemblage structure (species composition and density) and was correlated with significant declines in invertebrate abundance and species richness. Trampling effects were strongest for rare species. In heavily trafficked plots the abundance of sand hoppers (Amphipoda), a principal prey item of threatened Hooded Plovers breeding on this beach, was halved. In contrast to the consistently strong effects of trampling, natural habitat attributes (e.g. sediment grain size, compactness) were much less influential predictors. If acute suppression of invertebrates caused by trampling, as demonstrated here, is more widespread on beaches it may constitute a significant threat to endangered vertebrates reliant on these invertebrates. This calls for a re-thinking of conservation actions by considering active management of food resources, possibly through enhancement of wrack or direct augmentation of prey items to breeding territories.

Pliocene reversal of late Neogene aridification.

The Pliocene epoch (5.3-2.6 Ma) represents the most recent geological interval in which global temperatures were several degrees warmer than today and is therefore considered our best analog for a future anthropogenic greenhouse world. However, our understanding of Pliocene climates is limited by poor age control on existing terrestrial climate archives, especially in the Southern Hemisphere, and by persistent disagreement between paleo-data and models concerning the magnitude of regional warming and/or wetting that occurred in response to increased greenhouse forcing. To address these problems, here we document the evolution of Southern Hemisphere hydroclimate from the latest Miocene to the middle Pliocene using radiometrically-dated fossil pollen records preserved in speleothems from semiarid southern Australia. These data reveal an abrupt onset of warm and wet climates early within the Pliocene, driving complete biome turnover. Pliocene warmth thus clearly represents a discrete interval which reversed a long-term trend of late Neogene cooling and aridification, rather than being simply the most recent period of greater-than-modern warmth within a continuously cooling trajectory. These findings demonstrate the importance of high-resolution chronologies to accompany paleoclimate data and also highlight the question of what initiated the sustained interval of Pliocene warmth.