<![CDATA[Telah dilakukan penelitian untuk mempelajariperubahan iklim dan vegetasi menggunakan isotop alam 13C, 14C dan 18O yang berasal darisampel stalaktit. Sampel stalaktit diambil dari goa Seropan yang terletak di KecamatanSemanu, Gunung Kidul, Yogyakarta. Penelitian ini bertujuan mengetahui perubahan iklim,vegetasi, temperatur atmosfer, umur dan pertumbuhan stalaktit. Kandungan CaCO3 dalamstalaktit digunakan untuk mendapatkan data dari ke tiga jenis isotop alam tersebut. Dataisotop 13C digunakan untuk mengetahui fluktuasi iklim dan vegetasi. Data isotop 18O, baikyang berasal dari stalaktit maupun dari air tanah yang menetes dalam stalaktit digunakanuntuk mengetahui perubahan temperatur atmosfer, sedangkan isotop 14C digunakan untukmengetahui umur dan pertumbuhan stalaktit. Hasil analisis isotop alam 13C menunjukkanbahwa iklim daerah Gunung Kidul didominasi iklim kering. Hampir 87,5 % menunjukkanvegetasi kering C4, di mana kandungan 13C-nya lebih kaya (-6 o/oo hingga +2 o/oo Pee DeeBelemnite, PDB) dan hanya 12,5 % saja kadang-kadang vegetasinya basah C3, di manakandungan 13C-nya lebih miskin (-14 o/oo hingga -6 o/oo PDB). Dari hasil analisis 18O (stalaktit,PDB) dan 18O (tetesan air, Standard Mean Ocean Water, SMOW) menghasilkan data temperaturantara 12,2 oC hingga 32,1 oC dalam kurun waktu dari tahun 1621 hingga 2011 dengantemperatur rata-rata 19,5 oC, sedangkan dari hasil analisis 14C menunjukkan bahwapertumbuhan stalaktit sekitar 0,1 mm/tahun atau dalam sepuluh tahun hanya tumbuh sekitar1 mm saja. Pertumbuhan ini tergolong lambat dan hal ini lazim untuk daerah tropis denganiklim/vegetasi kering seperti Gunung Kidul.Climate and vegetation study usingenvironmental isotopes (i.e., 13C, 14C and 18O) variations of stalactite has been conducted atSeropan cave, Gunung Kidul Karst area. The stalactite samples were collected from SeropanCave at Semanu, Gunung Kidul, Yogyakarta. The objective of study is to understand theclimate change, and vegetation types, temperature of atmosphere, age and stalactite growthrate through the interpretation of environmental isotopes (i.e., 13C, 14C and 18O) of stalactitesamples. The environmental isotope content of stalactite samples were analysed throughCaCO3 compound that was found at the stalactite samples. The 13C content of samples isimportant to understand climate undulation and also vegetation variation. On the other hand,the variation of 18O and 14C contents is important to predict past temperature of atmosphere,and the age as well as stalactite growth rate, respectively. The result of environmental 13Cisotope analysis showed that Gunung Kidul area in general can be classified as dry climate. Itis also indicated that almost 87.5 % of local vegetation can be classified as dry vegetation C4as can be seen from the variation of 13C content that is -6 o/oo to +2 o/oo vs PDB. This can alsomean that only 12.5 % of the time that the vegetation in the area is wet in which the variationof 13C content is in the range -14 o/oo to -6 o/oo vs PDB. The variations of 18O contents of thesamples (carbonate stalactite, or drip water) showed that the average temperature since 1621to 2011 was around 19.5 oC. On the other hand, the variations of 14C contents of the samplesshowed that stalactite growth rate was around 0.1 mm/year or one mm in ten years. Theresult shows that the stalactite growth is very slow as generally expected in tropical area suchas Gunung Kidul.]]>
