Abstract It remains unclear whether waning of the volcanic degassing CO2 source or enhancement mafic (Ca, Mg-silicate) weathering sink, both, caused global cooling leading to Ordovician greenhouse–icehouse transition. We present a uniquely age-constrained and integrated Middle–Late (470–450 Ma) continental isotopic proxy data set (87Sr/86Sr ?Nd(t)) from carbonate rocks Antelope Range central Ne...