* 5,700-5,400 BC, in Italy, slowdown of the spread of Neolithic after its rapid expansion in South Italy. The change between mostly Csa (South of the Abruzzes) to Cfa (North of the Abruzzes) might be the reason. -* 5,700-5,200 BC: Cardial Filiestru-Basi-Pienza (Cardial FBP) in Tyrrhenian and Ligurian Sea. +* 5,700-5,400 BC, on both sides of the Ardriatic Sea (Italy and Croatia), linear gradient: maritime networks. +* 5,700-5,200 BC in Tyrrhenian and Ligurian Sea, development of the Cardial Filiestru-Basi-Pienza (Cardial FBP)
@@ -1603,8 +1604,8 @@ neo_dbs_info_dates_datatable(df.c14 = data, verbose = FALSE)-* *Leapfrogs*, originally from Italy, with mostly settlements in (same) Csa climates -* Fonbregoua in Cfb climate (*Temperate, no dry season, warm summer*) and Gazel in Cfa climate +* *Leapfrogs* to Southern France and the Iberian Peninsula, with mostly settlements in (same) Csa climates, among others: Pont de Roque-Haute (idf 148, Southern France), Coves del Fem (idf 101, Northeastern Spain), Cabranosa (idf 31, South Portugal). +* Fonbregoua in Cfb climate (*Temperate, no dry season, warm summer*) and Gazel in Cfa climate.
@@ -1674,10 +1675,10 @@ neo_dbs_info_dates_datatable(df.c14 = data, verbose = FALSE)-* The Southwest of the Iberian Peninsula is neolithised by ... -* Direct maritime connection between Corsica and Sardinia to the Levant Iberian coast is likely improbable. -* Catalonian Neolithic faces different climates that slow down the spread of the Neolithic (acclimatization) -* Pioneer site in Csb climate (*Temperate, dry summer, warm summer*) C8C800 between 5,600 and 5,300 BC: Balma Margineda (Andorra), Abri des Castelli (Corsica), and a cluster in the upper Ebro Basin: Tumul del Padro, etc. +* 5,900-5,300 BC, neolithisation of Southwestern Iberian Peninsula (Portugal). +* Catalonian Neolithic faces different climates that slowdown the spread of the Neolithic (acclimatization): Csa, Cfa, Cfb. +* At the opposite of Catalonia, Valencian area, with only the two main climates of Early Neolithic: Csa and BSk, favoring a faster diffusion. +* Pioneer sites in Csb climate (*Temperate, dry summer, warm summer*) between 5,600 and 5,300 BC: Balma Margineda (idf 24, Andorra), Abri des Castelli (idf 3, Corsica) and, later, a cluster in the upper Ebro Basin: Tumul del Padro (idf 168), etc.