“…R s is generally accepted to be largely controlled by soil temperature (Bond-Lamberty and Thomson, 2010) with the consequence that many studies consider it sufficient to use a single simultaneous daily measurement of R s to test for differences between different land uses or vegetation types and to extrapolate long-term budgets, (e.g. Barrena et al, 2013;Finocchiaro et al, 2014;Gauder et al, 2012;Johnson et al, 2010;Shvaleva et al, 2014;von Arnold et al, 2005;Zhang et al, 2013). Whilst the importance of selecting appropriate and synchronous sampling times is commonly recognised, measurement "windows" often vary across two hours (Kessavalou et al, 1998;Zhang et al, 2013) to as much as seven (Finocchiaro et al, 2014) or even eight hours (Gao et al, 2014), generally between 09:00-16:00; however, none of these cited studies provided any data to support these windows which are largely based on minimising time delays between comparisons and assumptions that minimised temperature changes are the key to measurement parity.…”