https://ogma.newcastle.edu.au/vital/access/ /manager/Index en-au 5 https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:4333 Wed 11 Apr 2018 14:51:48 AEST ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:8812 Wed 11 Apr 2018 13:34:59 AEST ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:30645 148,000 samples to reveal huge differences in range changes associated with climate change across 35 plankton taxa. While the range of dinoflagellates and copepods tended to closely track the velocity of climate change (the rate of isotherm movement), the range of the diatoms moved much more slowly. Differences in range shifts were up to 900 km in a recent warming period, with average velocities of range movement between 7 km per decade northwards for taxa exhibiting niche plasticity and 99 km per decade for taxa exhibiting niche conservatism. The differing responses of taxa to global warming will cause spatial restructuring of the plankton ecosystem with likely consequences for grazing pressures on phytoplankton and hence for biogeochemical cycling, higher trophic levels and biodiversity.]]> Wed 11 Apr 2018 11:01:43 AEST ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:19623 Wed 11 Apr 2018 10:03:22 AEST ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:39071 Wed 04 May 2022 15:09:24 AEST ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:44316 Tue 11 Oct 2022 16:19:25 AEDT ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:9053 Sat 24 Mar 2018 08:41:06 AEDT ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:8880 Sat 24 Mar 2018 08:40:43 AEDT ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:11192 Sat 24 Mar 2018 08:13:36 AEDT ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:12313 Sat 24 Mar 2018 08:11:36 AEDT ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:10061 Sat 24 Mar 2018 08:07:22 AEDT ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:16617 Sat 24 Mar 2018 08:03:01 AEDT ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:5967 Sat 24 Mar 2018 07:47:25 AEDT ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:5968 Sat 24 Mar 2018 07:47:25 AEDT ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:29722 2282 AU, weekly-TL >2786 AU and monotony >0.78 AU) to best predict when athletes are at increased risk of self-reported illness. In addition, a reduction in overall wellbeing (<7.25 AU) in the presence of increased internal-TL as previously stated, was highlighted as a contributor to self-reported illness occurrence.These results indicate that self-report data can be successfully utilized to provide a novel understanding of the interactions between competition-associated stressors experienced by professional team-sport athletes and their susceptibility to illness. This may assist coaching staff to more effectively monitor players during the season and to potentially implement preventative measures to reduce the likelihood of illnesses occurring.]]> Sat 24 Mar 2018 07:33:25 AEDT ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:40442 n = 10 taxa) tended to show a large seasonal advancement, the timing of peak abundance for dinoflagellates as group advancing 39 days over these six decades. By contrast diatoms (n = 35) did not show any change as a group in their timing of peak abundance over the time series. Granger causality testing suggested a major driver of these phenological changes has been ocean warming in general but more specifically the rate of spring temperature rise as the most important factor. We also found differences in the timing of peak abundance of harmful algal bloom taxa, with some showing peak abundance earlier while others have moved later. Main conclusions: There has been a fundamental transformation of the classic seasonal progression from blooms of diatoms to dinoflagellates, which lies at the heart of temperate marine food chains, as the classic bimodal diatom and dinoflagellate seasonal peaks are eroded to a more continuous, single, longer-lasting phytoplankton peak. This phenological shuffling within and between major taxonomic groups is likely to have profound implications for the transfer of energy to higher trophic levels.]]> Fri 22 Jul 2022 14:37:23 AEST ]]>