13 research outputs found
Relationships between Antarctic cyclones and surface conditions as derived from high-resolution numerical weather prediction data
Insolation and cross-hemispheric controls on Australian monsoon variability over the past 180 ka: new evidence from offshore southeastern Papua New Guinea
The impact of European occupation on terrestrial and aquatic ecosystem dynamics in an Australian tropical rain forest
1 The long-term impact of changes in land use, fire and climate on species diversity in Australia are only just beginning to be understood. We combined fine-resolution palaeoecological proxies for terrestrial and aquatic ecosystems to investigate the responses of a tropical rain forest catchment over the last 700 years. 2 Sediment cores were sampled at 1-cm intervals to a depth of 100 cm from Lake Euramoo on the Atherton Tableland of north-east Queensland, dated and analysed for pollen, charcoal, diatom, chironomid and inorganic content. 3 The pollen and charcoal record shows a rapid loss of forest diversity (particularly the long-lived taxa Agathis and Podocarpus) and increased burning coinciding with the arrival of European settlers. The aquatic environment is also subject to rapid changes at this time, with a possible increase in pH and subsequent shifts in local algal and insect communities. This event was outside the historic range of variability in both rain forest and aquatic communities. 4 The present mosaic of vegetation types is a complex function of environmental changes operating across a range of spatial and temporal scales: millennial climate change, short-term climatic variations associated with El Niño events and, most significantly, a shift from indigenous to 'European' land-use practices, including clearance and burning activities associated with the timber and farming industry between about ad 1880 and 1920. 5 The establishment of a World Heritage reserve around the lake catchment and the suppression of fire over the last 50 years have not yet restored the terrestrial or aquatic ecosystem to its pre-European state and are unlikely to, given the current predictions of future climate change. This supports the notion that ecological and climate thresholds are not necessarily the same, and that the effects of crossing them are not necessarily reversible. Retrospective studies of the historic range of variability within small catchments can provide an understanding of the limits of natural and human-induced variability that can inform management decisions and resource planning.Simon G. Haberle, John Tibby, Sophia Dimitriadis, and Henk Heijni
Recommended from our members
Millennial and orbital variations of El Nino/Southern Oscillation and high-latitude climate in the last glacial period
The El Nino/Southern Oscillation (ENSO) phenomenon is believed to have operated continuously over the last glacial interglacial cycle(1). ENSO variability has been suggested to be linked to millennial-scale oscillations in North Atlantic climate during that time(2,3), but the proposals disagree on whether increased frequency of El Nino events, the warm phase of ENSO, was linked to North Atlantic warm or cold periods. Here we present a high-resolution record of surface moisture, based on the degree of peat humification and the ratio of sedges to grass, from northern Queensland, Australia, covering the past 45,000 yr. We observe millennial-scale dry periods, indicating periods of frequent El Nino events ( summer precipitation declines in El Nino years in northeastern Australia). We find that these dry periods are correlated to the Dansgaard - Oeschger events - millennial-scale warm events in the North Atlantic climate record - although no direct atmospheric connection from the North Atlantic to our site can be invoked. Additionally, we find climatic cycles at a semiprecessional timescale (, 11,900 yr). We suggest that climate variations in the tropical Pacific Ocean on millennial as well as orbital timescales, which determined precipitation in northeastern Australia, also exerted an influence on North Atlantic climate through atmospheric and oceanic teleconnections