https://nova.newcastle.edu.au/vital/access/ /manager/Index en-au 5 https://nova.newcastle.edu.au/vital/access/ /manager/Repository/uon:17139 p) rather than the thermodynamic partition coefficient (K_p) to account for the presence of crystalline phosphate inclusions. SK_p describes P enrichment in speleothems regardless of the process, as similar mechanisms of phosphate co-precipitation may be in operation in biotic and abiotic conditions. The most important implication of our study is that variability in P concentration may be related to diverse processes which can be recognized through petrographic observations and chemical mapping. In particular, there may not be a direct relation between an increase in P concentration and seasonal infiltration as has been found in some previous studies, especially if the source of this element is not the labile phosphate released through leaching during seasonal vegetation dieback in temperate climates.]]> Wed 11 Apr 2018 10:30:22 AEST ]]> https://nova.newcastle.edu.au/vital/access/ /manager/Repository/uon:6875 Tue 19 May 2020 10:48:38 AEST ]]> https://nova.newcastle.edu.au/vital/access/ /manager/Repository/uon:7742 Sat 24 Mar 2018 08:41:55 AEDT ]]> https://nova.newcastle.edu.au/vital/access/ /manager/Repository/uon:5267 Sat 24 Mar 2018 07:46:33 AEDT ]]> https://nova.newcastle.edu.au/vital/access/ /manager/Repository/uon:3319 Sat 24 Mar 2018 07:23:19 AEDT ]]> https://nova.newcastle.edu.au/vital/access/ /manager/Repository/uon:3320 Sat 24 Mar 2018 07:23:18 AEDT ]]> https://nova.newcastle.edu.au/vital/access/ /manager/Repository/uon:3317 Sat 24 Mar 2018 07:23:18 AEDT ]]>