LINGKUNGAN PENGENDAPAN DI SITUS NEGERI BARU, KALIMANTAN BARAT
Abstract
Situs Negeri Baru terletak di tepi aliran Sungai Pawan yang bermuara di Selat Karimata. Satuan batuandi Situs Negeri Baru adalah aluvium dan endapan rawa, yang terdiri atas lingkungan pengendapan aluvium resen,
aluvium tua, dan endapan rawa dataran pantai. Tulisan ini membahas lebih jauh karakteristik lingkungan pengendapan
di kawasan Situs Negeri Baru. Studi ini dilakukan dengan analisis sedimentologi dan stratigrafi berdasarkan data
dari delapan belas kotak ekskavasi. Hasil kajian menunjukkan bahwa korelasi perubahan lingkungan pengendapan
secara lateral dan vertikal pada rangkaian endapan kuarter di Situs Negeri Baru diindikasikan merupakan perubahan
dari lingkungan permukaan pantai atas (upper shoreface) menjadi sol. Lingkungan pengendapan ini terletak pada
estuari dan permukaan pantai (shoreface) dan sangat dipengaruhi oleh pasang surutnya air laut.
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