varia

doc/talks/2024-asd/index.qmd

@@ -1237,7 +1237,7 @@ neo_dbs_info_dates_datatable(df.c14 = data, verbose = FALSE)
 
 <small>
 
-* Greece mainland turns colder (*8.2 ky BP event*), for example: <span style="color:#FF00FF;">Dsa</span> → <span style="color:#37C8FF;">Dfb</span> 
+* Greece mainland turns colder (*8.2 ky BP event*), for example: <span style="color:#FF00FF;">Dsa</span> → <span style="color:#37C8FF;">Dfb</span> (*Cold, no dry season, warm summer*)
 * In South Balkans, concentration of dates in <span style="color:#FFDC64;">BSk</span> climates (<span style="color:#FFDC64;">Sesklo</span>, idf <b>52</b>; <span style="color:#FFDC64;">Paliambela</span>, idf <b>41</b>); <span style="color:#FFDC64;">Anzabegovo</span>, idf <b>41</b>; etc. )
 * First Neolithic in Northern East Mediterranean (Ugurlu, idf <b>57</b>, no climatic data) related to first Neolithic in Northwestern Anatolia: <span style="color:#FFFF00;">Barcin</span> (idf <b>9</b>), <span style="color:#FFFF00;">Aktopraklik</span> (idf <b>2</b>)
 * New <span style="color:#C8FF50;">Cfa</span> climate (*Temperate, no dry season, hot summer*) with  <span style="color:#C8FF50;">Mavropigi</span> (idf <b>36</b>), <span style="color:#C8FF50;">Lefkopetra</span> (idf <b>33</b>), <span style="color:#C8FF50;">Orfeas</span> (idf <b>40</b>)
@@ -1318,6 +1318,7 @@ neo_dbs_info_dates_datatable(df.c14 = data, verbose = FALSE)
 <p><small>
 
 * Rapid expansion in the Southern Balkans (<span style="color:#FFFF00;">Csa</span> and <span style="color:#FFDC64;">BSk</span>). And slowdown of Neolithic expansion in Northern Balkans' expansion required adapting agriculture and stockbreeding systems to colder climates (<span style="color:#00FFFF;">Dfa</span>, <span style="color:#37C8FF;">Dfb</span>, ex: <span style="color:#37C8FF;">Porodin</span>, idf <b>46</b>). Confirms: Krauß et al. 2018[^81], Ivanova et al. 2018[^82].
+* Pioneer site in <span style="color:#00FFFF;">Dfa</span> climate (*Cold, no dry season, hot summer*).
 * South of Italy (off the map) is reached, probably from Corfu: <span style="color:#FFFF00;">Sidari</span> (idf <b>53</b>)
 
 </small></p>
@@ -1691,7 +1692,7 @@ neo_dbs_info_dates_datatable(df.c14 = data, verbose = FALSE)
 ## End of the Mediterranean Neolithisation
 
 <center>
-![](https://raw.githubusercontent.com/zoometh/neonet/master/doc/talks/2024-asd/img/isochr-5200-BC-MedCompleted-koppen_7k.png){width="900" style="horizontal-align: middle;"}
+![](https://raw.githubusercontent.com/zoometh/neonet/master/doc/talks/2024-asd/img/isochr-5200-BC-MedCompleted-koppen_7k.png){height="550" style="horizontal-align: middle;"}
 </center>
 
 
@@ -1811,6 +1812,10 @@ minimizing regional climate contrasts: Similarity between local landscapes of ea
 
 ## Climates occupied by the Early Farmers 
 
+::: {.panel-tabset}
+
+### Overview
+
 ::: columns
 
 ::: {.column width="50%"}
@@ -1823,20 +1828,38 @@ minimizing regional climate contrasts: Similarity between local landscapes of ea
 
 :::
 
+### Pioneer Neolithic sites
+
 ![](https://raw.githubusercontent.com/zoometh/neonet/master/doc/talks/2024-asd/img/Slide2.PNG){width="1000" style="horizontal-align: middle;"}
 
+ca 10,000-9,500 BC, Near East <span style="color:#FFDC64;">BSk</span> (*Temperate, dry summer, warm summer*), <span style="color:#FFFF00;">Csa</span> (*Temperate, dry summer, hot summer*) and, more rarely, <span style="color:#FF00FF;">Dsa</span> (*Cold, dry summer, hot summer*) climates.
+
 ![](https://raw.githubusercontent.com/zoometh/neonet/master/doc/talks/2024-asd/img/Slide3.PNG){width="1000" style="horizontal-align: middle;"}
 
+ca 9,000-7,500 BC, Near East <span style="color:#FF0000;">BWh</span> climate (*Arid, desert, hot*), ie: arid margins
+
 ![](https://raw.githubusercontent.com/zoometh/neonet/master/doc/talks/2024-asd/img/Slide4.PNG){width="1000" style="horizontal-align: middle;"}
 
+ca 8,000-7,500 BC, Near East (South Levant), <span style="color:#F5A500;">BSh</span> (*Arid, steppe, hot*), and <span style="color:#FF9696;">BWk</span> (*Arid, desert, cold*).
+
 ![](https://raw.githubusercontent.com/zoometh/neonet/master/doc/talks/2024-asd/img/Slide5.PNG){width="1000" style="horizontal-align: middle;"}
 
+ca 6,500-6,000 BC, Balkans (between North and South), <span style="color:#C8FF50;">Cfa</span> climate (*Temperate, no dry season, hot summer*)
+
 ![](https://raw.githubusercontent.com/zoometh/neonet/master/doc/talks/2024-asd/img/Slide6.PNG){width="1000" style="horizontal-align: middle;"}
 
+ca 6,100-6,000 BC, Balkans, <span style="color:#37C8FF;">Dfb</span> (*Cold, no dry season, warm summer*) = Proto-Sesklo Culture.
+
 ![](https://raw.githubusercontent.com/zoometh/neonet/master/doc/talks/2024-asd/img/Slide7.PNG){width="1000" style="horizontal-align: middle;"}
 
+ca 6,100-6,000 BC, Northern Balkans and Central Europe, <span style="color:#00FFFF;">Dfa</span> (*Cold, no dry season, hot summer*), outside the studied area.
+
 ![](https://raw.githubusercontent.com/zoometh/neonet/master/doc/talks/2024-asd/img/Slide8.PNG){width="1000" style="horizontal-align: middle;"}
 
+ca 5,500-5,300 BC, Western Mediterranean, <span style="color:#C8C800;">Csb</span> climate (*Temperate, dry summer, warm summer*)
+
+:::
+
 
 ## <img src='https://raw.githubusercontent.com/zoometh/thomashuet/master/img/app-prg-r.png' style='height: 50px;vertical-align: middle;'/> productible methods {data-visibility=hidden}
 

doc/talks/2024-asd/run_asd.R

@@ -127,7 +127,7 @@ isochr <- neo_isochr(df.c14 = df_filtered,
                      lbl.time.interv = TRUE)
 isochr$map
 # ggplot2::ggsave(paste0(obj.case.out, ".png"), isochr$map, width = 7, height = 6)
-ggplot2::ggsave(paste0(obj.case.out, ".png"), isochr$map, width = 16, height = 8)
+ggplot2::ggsave(paste0(obj.case.out, ".png"), isochr$map, width = 10, height = 8)
 ggplot2::ggsave(paste0(obj.case.out, "-legend.png"), isochr$legend, width = 5)
 write.table(isochr$data, paste0(obj.case.out, ".tsv"), sep = "\t", row.names = FALSE)
 # subset(isochr$data[order(isochr$data$median),], code == 'Csb')