Tái cấu trúc cổ sinh thái của thời kỳ Pleistocen muộn, dựa trên hệ động vật hai mãnh tại Hungary

GeoJournal - Tập 36 - Trang 213-222 - 1995
Endre Krolopp1, Pál Sümegi2
1Hungarian Geological Survey, Budapest, Hungary
2Dept. of Geology, Kossuth University, Debrecen, Hungary

Tóm tắt

Các loài nhuyễn thể được thu thập từ các lớp đất loess và các lớp tương tự ở Hungary bằng phương pháp phát triển cho các nghiên cứu địa tầng phân giải cao, đã được đánh giá thống kê để tái cấu trúc môi trường cổ. Các loài được phân loại theo 4 yếu tố sinh thái quan trọng, cụ thể là: loại đất, độ ẩm không khí, nhiệt độ và thảm thực vật. Dựa trên sự thay đổi theo thời gian trong tính ưu thế, các thời kỳ cổ sinh thái đã được phân biệt. Trong thời kỳ băng hà Würm, 5 sự thay đổi lớn đã được phát hiện qua phương pháp này. Giữa khoảng thời gian thứ tư và thứ năm được phân định (cuối Würm và các thời kỳ băng hà muộn) đã có thể xác định được 9 sự kiện có thời gian ngắn và ý nghĩa sinh thái của chúng đã được tái cấu trúc.

Từ khóa

#nhuyễn thể #tầng lớp đất loess #tái cấu trúc môi trường cổ #đặc điểm sinh thái #thời kỳ Pleistocen

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