TL;DR: The temporal distribution of releases in tree ring sequences suggested a history of chronic patchy disturbance during at least the last 400 years, and the role of juvenile and adult life history differences in promoting coexistence of the four main overstory species was determined.
Abstract: We examined stand disturbance history, population structures, spatial relationships of age classes and size classes, and tree growth histories in an old-growth temperate rain forest in southern New Zealand. We aimed to determine the role of juvenile and adult life history differences in promoting coexistence of the four main overstory species (Nothofagus menziesii, Weinmannia racemosa, Dacrydium cupressinum, and Prumnopitys ferruginea). There was no evidence that major compositional shifts were occurring: N. menziesii, D. cupressinum, and P. ferruginea were represented by all-aged populations, indicating continual recruitment of all three species within the 5-ha study area during recent centuries. No age data were obtained for W. racemosa, but the diameter distribution of this species was consistent with an all-aged population structure. The temporal distribution of releases in tree ring sequences suggested a history of chronic patchy disturbance during at least the last 400 years. Ring width sequences we...
TL;DR: A model based on the extant cool temperate Valdivian rainforests is proposed and ecological reconstructions based on palaeobotanical and geological evidence suggest that changes in the palaeovegetation reflect natural dynamics following volcanic disturbances.
TL;DR: In this article, the authors used data from fossil macrofloras and microfloras in southeastern Australia are used to reconstruct vegetation and climates for the early Paleogene, showing that for much of the late Paleocene to middle Eocene, complex, species-rich forests were predominant in the southeastern Australia, under mesothermal humid climates.
Abstract: In this study, data from fossil macrofloras and microfloras in southeastern Australia are used to reconstruct vegetation and climates for the early Paleogene. Our data show that for much of the late Paleocene to middle Eocene, complex, species-rich forests were predominant in southeastern Australia, under mesothermal humid climates (mean annual temperature 16-22 °C, coldest quarter mean temperature >10 °C, mean annual precipitation >150 cm/yr). A minor cooling episode may have occurred in the mid-early Eocene. Megathermal climates may have been present in lowlands in the latest early Eocene, during the Cenozoic Global Climatic Optimum. These forests were dominated by taxa characteristic of present-day mesothermal-megathermal high-rainfall multistratal forests; e.g., Cunoniaceae, Elaeocarpaceae, Gymnostoma (Casuarinaceae), Lauraceae (e.g., Beilschmiedia, Cryptocarya and Endiandra), and Proteaceae. A prominent treefern element (Cyathea and Dicksonia types) was present in the early Eocene. A number of megathermal taxa, including Cupanieae (Sapindaceae) and Ilex (Aquifoliaceae), were present through the early and middle Eocene. Taxa characteristic of modern-day microthermal to mesothermal forests were also present, e.g., Nothofagus (Nothofagaceae), Eucryphia (Eucryphiaceae), Libocedrus (Cupressaceae) and Podocarpaceae (Acmopyle and Dacrycarpus). The relictual araucarian conifer, Wollemia, and other Araucariaceae were present through the late Paleocene to early Eocene. There is limited physiognomic evidence to suggest the late Paleocene to early Eocene forests contained some deciduous canopy trees.
TL;DR: The Oligocene vegetation at Pioneer was closed temperate rainforest dominated by Nothofagus johnstonii Hill, which probably produced N. menziesii-type pollen.
Abstract: The Oligocene vegetation at Pioneer was closed temperate rainforest dominated by Nothofagus johnstonii Hill, which probably produced N. menziesii-type pollen. However, other angiosperms (Quintinia, Cupaniae, Ilex, Cunoniaceae, Myrtaceae, Proteaceae and Winteraceae) were also present, as well as several conifers (Athrotaxis, Phyllocladus, Podocarpus, Dacrydium, Dacrycarpus and Araucariaceae). This rainforest was floristically more complex that the modern Tasmanian Nothofagus cunninghamii rainforests but contained many taxonomically related elements. One major difference was that a fern similar to extant Cyathea filled the riparian niche now largely occupied by the tree-fern Dicksonia antarctica. There is indirect evidence that species producing Nothofagus brassii-type pollen may have occurred upstream of the site of deposition, suggesting that the Nothofagus species were altitudinally zoned or edaphically restricted. The current absence of many of these Nothofagus species in Tasmania may be due to their in...
TL;DR: Parsimony cladistic analyses of chloroplast DNA sequences from two loci, trnL-trnF and rbcL, and morphology show that three genera often placed in their own families, Bauera, Davidsonia, and Eucryphia, are nested within Cunoniaceae, a circumscription of the flowering plant family with 26 genera and approximately 300 species.
Abstract: A phylogeny and revised classification of the flowering plant family Cunoniaceae and related taxa is presented. Parsimony cladistic analyses, including bootstrap and decay analyses, of chloroplast DNA sequences from two loci, trnL-trnF and rbcL, and morphology show that three genera often placed in their own families, Bauera, Davidsonia, and Eucryphia, are nested within Cunoniaceae. Brunellia may be most closely related to the Australian pitcher plant Cephalotus, and Aphanopetalum is in Saxifragales. Within Cunoniaceae, the New Guinean-South Pacific genera Acsmithia and Spiraeanthemum form a sister clade to the rest of family. Within this larger clade is a basal grade in which flowers mature centrifugally on an inflorescence axis, and a clade in which flowers mature synchronously to acropetally on an inflorescence axis. Other conspicuous morphological characters, including stipule position, inflorescence form, petal presence or absence, number of pollen colpi, carpel number, and fruit morphology,...