New　speleothem　records　from　northeastern　Iberian　caves　provide　data　to　explore　the　climatic　patterns　during　the　Holocene.　We　present　delta　C-13　and　Mg/Ca　from　three　speleothems　from　two　different　caves　located　in　the　Iberian　Range　allowing　replication　of　the　climatic　signal　for　several　millennia.　Through　the　integration　of　those　stalagmites　covering　since　the　Holocene　onset　to　2　ka,　the　early　Holocene　(11.7-8.5　ka)　appears　as　the　wettest　interval.　A　marked　change　towards　aridity　is　observed　during　the　middle　Holocene　(8.5-4.8　ka)　and　an　increase　of　humidity　afterwards　(4.8-2　ka).　This　three-part　pattern,　contrasting　with　other　Iberian　sequences,　seems　to　be　associated　with　the　different　role　that　seasonality　has　played　in　the　response　of　different　proxies　(or　records)　to　changes　in　water　availability.　Interpreting　our　speleothem　records　as　changes　in　winter-spring　precipitation　along　the　Holocene　allows　reconciling　previous　data　on　hydrological　variability　from　the　western　Mediterranean　borderlands.