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Study region Western Tasmania, southeastern Australia.Study focus We present two new tree-ring based inflow reconstructions from western Tasmania in southeastern Australia.The warm season reconstruction (Dec–Feb) extends from 1030–2007 CE and explains up to 42% of the variance in instrumental flow, while the cool season (JA) extends from 1550–2007 CE and explains 27% of instrumental flow variance. Key features include an extended pluvial period in the 11th Century and a protracted dry period in ∼1500CE, neither of which are represented in the DJF instrumental record. Decreasing JA flow since the 19th Century is consistent with a local sediment-based hydroclimate record.New hydrological insights for the region The reconstructions confirm that the instrumental data do not capture how protracted past low or high flow periods have been. It is therefore important to consider pre-instrumental flow data when planning for the future. The reconstructions provide new insights into regional variability through their association with the Subtropical Ridge (STR) and the Southern Annular Mode (SAM). Differing spatial signatures of the seasonal reconstructions, and their associations with season-specific impacts of STR and SAM, highlight the need for caution when considering the use of remote hydroclimate proxy records with strong seasonal signatures. The reconstructions suggest that extrapolation of seasonally defined reconstructions to represent annual flow for regions beyond the extent of their spatial footprint may be problematic.

This paper presents the spatial and temporal characteristics of petroleum hydrocarbons (PH) in surficial sediments from the Songhuajiang River using the method of petroleum chemical fingerprinting. Twenty-four surface sediment samples were collected at 17 sites along the river from upstream to downstream in flood season (August 2005) and icebound season (December 2005) and were analyzed for PH including n-alkanes (C-C), isoprenoid alkanes (pristane and phytane), and unresolved complex mixture (UCM). The concentration of PH varied from 22.64 to 91.45 μg g dry sediment. n-alkanes with a carbon number from 16 to 33 were detected in all samples, and the UCM was the dominant composition for PH. The variability of the PH concentration was mostly influenced by external conditions, such as seasonal change and industrial area position, as well as internal sediment physicochemical properties, such as organic carbon and grain size. The concentration of hydrocarbons is higher in flood season than in icebound season and is higher upstream than downstream. The diagnostic ratios of specific hydrocarbons showed that the PH pollution comes from a combination of biogenic and petrogenic sources, and petrogenic input is dominant in icebound season relative to flood season. It also indicates that there is a clear terrigenous input of n-alkanes in flood season. Principal components analysis was used to study the composition and characteristics of PH in Songhuajiang River sediments and to assess the spatial and temporal distribution of their natural and anthropogenic sources. [ABSTRACT FROM AUTHOR]