¶óÆæÆ®¦¢Ä«Æä¦¢ºí·Î±×¦¢´õº¸±â
¾ÆÄ«µ¥¹Ì Ȩ ¸í»çƯ°­ ´ëÇבּ¸½Ç޹æ Á¶°æ½Ç¹« µ¿¿µ»ó°­ÀÇ Çѱ¹ÀÇ ÀüÅëÁ¤¿ø ÇÐȸº° ³í¹®
ÇÐȸº° ³í¹®

Çѱ¹°Ç¼³°ü¸®ÇÐȸ
Çѱ¹°ÇÃà½Ã°øÇÐȸ
Çѱ¹µµ·ÎÇÐȸ
Çѱ¹»ý¹°È¯°æÁ¶ÀýÇÐȸ
Çѱ¹»ýÅÂÇÐȸ
Çѱ¹¼öÀÚ¿øÇÐȸ
Çѱ¹½Ä¹°ÇÐȸ
Çѱ¹½Ç³»µðÀÚÀÎÇÐȸ
Çѱ¹ÀÚ¿ø½Ä¹°ÇÐȸ
Çѱ¹ÀܵðÇÐȸ
Çѱ¹Á¶°æÇÐȸ
Çѱ¹Áö¹Ý°øÇÐȸ
Çѱ¹ÇÏõȣ¼öÇÐȸ
Çѱ¹È¯°æ»ý¹°ÇÐȸ
Çѱ¹È¯°æ»ýÅÂÇÐȸ

Çѱ¹»ýÅÂÇÐȸ / v.28, no.1, 2005³â, pp.37-43
¿µ»ê°­ À¯¿ª ¹ü¶÷¿ø ÅðÀû¹°ÀÇ È­ºÐºÐ¼® ¿¬±¸
( Vegetation History since the Mid-Lateglacial from Yeongsan River Basin, Southwestern Korea )
ÃÖ±â·æ;±è±âÇå;±èÁ¾¿ø;±èÁ¾Âù;ÀÌ±â±æ;¾çµ¿À±;³²¿íÇö; ¿ï»ê´ëÇб³ »ý¸í°úÇкÎ;¿ï»ê´ëÇб³ »ý¸í°úÇкÎ;°è¸í´ëÇб³ »ý¹°Çаú;¼­¿ï´ëÇб³ ¹°¸®ÇкÎ;Á¶¼±´ëÇб³ »çÇаú;¿ï»ê´ëÇб³ »ý¸í°úÇкÎ;Çѱ¹ÁöÁúÀÚ¿ø¿¬±¸¿ø;
 
ÃÊ ·Ï
Çѹݵµ ³²¼­ºÎ ÀúÁö´ëÀÇ ½Ä»ýº¯Ãµ»ç¸¦ ¹àÈ÷±â À§ÇÏ¿© ¿µ»ê°­À¯¿ª ¹ü¶÷¿ø ÅðÀû¹°ÀÇ È­ºÐºÐ¼®°ú AMS ÃøÁ¤À» ½Ç½ÃÇÏ¿´´Ù. ±× °á°ú BS 1. 12,222cal BC$sim$9,160cal BC: ³Ã¿Â´ë ºÏºÎ/°í»êÁö ħ¿± Ȱ¿±È¥ÇÕ¸², BS 2. 9,160cal BC$sim$4,210cal BC: ³Ã¿Â´ë ÁߺÎ/»êÁö ³«¿±È°¿±¼ö¸², BS 3. 4,210cal BC$sim$125cal BC: ³Ã¿Â´ë ³²ºÎ/Àú»êÁö ħ¿± Ȱ¿±È¥ÇÕ¸², BS 4. 125cal BC$sim$ÇöÀç: ³­¿Â´ë/³Ã¿Â´ë ³²ºÎ/Àú»êÁö ħ¿±¼ö¸²ÀÇ ½Ä»ýº¯Ãµ°úÁ¤À» ¹àÈú ¼ö ÀÖ¾ú´Ù. ¼Ò³ª¹«¸²ÀÇ Áõ°¡´Â 4,210cal BCºÎÅÍ ÀÌ¸ç º­³ó»ç °³½Ã ½Ã±â´Â 2,120cal BCºÎÅÍ Áý¾àÀûÀ¸·Î ÀÌ·ç¾îÁö±â ½ÃÀÛÇÏ¿´À½À» ¹àÇû´Ù. ¶ÇÇÑ Èĺù±â Èı⠼ҳª¹«¸²ÀÇ ±Þ°ÝÇÑ Áõ°¡´Â ³ó°æÀÇ Áý¾àÈ­¿Í °ü°è°¡ ÀÖÀ½À» ¾Ë ¼ö ÀÖ¾ú´Ù.
This study presents the Mid-Lateglacial vegetation history of southwestern Korea. From the result of AMS dating and pollen analysis, four local pollen assemblage zones(BS) were recognized. The four local pollen assemblage zones are BS 1. 12,222cal BC$sim$9,160cal BC: cool-temperate northern/altimontane mixed coniferous & deciduous broad-leaved forest, BS 2. 9,160cal BC$sim$ 4,210cal BC: cool-temperate central/montane deciduous broad-leaved forest, BS 3. 4,210cal BC$sim$125cal BC: cool-Temperate southern/submontane mixed coniferous & deciduous broad-leaved forest. BS 4. BC125cal ${sim}$present: warm-temperate/cool-temperate southern/submontane coniferous forest. Pine forest expanded since 4,210cal BC and full-scale rice cultivation might started since 2,120cal BC. A radical expansion of Pinus densiflora forest after postglacial stage might be caused by human impacts including full-scale agriculture.
 
Ű¿öµå
Lateglacial;Pollen analysis;Postglacial;Rice cultivation;Vegetation history;
 
The Korean Journal of Ecology / v.28, no.1, 2005³â, pp.37-43
Çѱ¹»ýÅÂÇÐȸ
ISSN : 1225-0317
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO200509905764885)
¾ð¾î : Çѱ¹¾î
³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø
¸ñ·Ïº¸±â
ȸ»ç¼Ò°³ ±¤°í¾È³» ÀÌ¿ë¾à°ü °³ÀÎÁ¤º¸Ãë±Þ¹æÄ§ Ã¥ÀÓÀÇ ÇѰè¿Í ¹ýÀû°íÁö À̸ÞÀÏÁÖ¼Ò ¹«´Ü¼öÁý °ÅºÎ °í°´¼¾ÅÍ
   

ÇÏÀ§¹è³ÊÀ̵¿