Lineage 发表于 2025-3-23 10:08:13
http://reply.papertrans.cn/59/5807/580634/580634_11.png大量杀死 发表于 2025-3-23 14:08:30
http://reply.papertrans.cn/59/5807/580634/580634_12.pngExpurgate 发表于 2025-3-23 19:07:38
http://reply.papertrans.cn/59/5807/580634/580634_13.pngMitigate 发表于 2025-3-23 22:32:45
http://reply.papertrans.cn/59/5807/580634/580634_14.pnghabile 发表于 2025-3-24 05:40:02
http://reply.papertrans.cn/59/5807/580634/580634_15.png酷热 发表于 2025-3-24 08:29:56
The Evolution of Vegetation from the Last Glacial Maximum Until the Presentgh-resolution palaeoecological records (pollen, plant macrofossil and charcoal) from Romania and provides an overview of broad-scale vegetation dynamics and diversity from the Last Glacial Maximum (LGM) to the present. Specifically, we discuss: (i) temporal and spatial variations in the magnitude of改变 发表于 2025-3-24 14:10:44
http://reply.papertrans.cn/59/5807/580634/580634_17.png揉杂 发表于 2025-3-24 15:40:42
http://reply.papertrans.cn/59/5807/580634/580634_18.png愤怒历史 发表于 2025-3-24 21:51:59
Present-Day Periglacial Processes in the Alpine Zoneost has a patchy distribution and occurs in marginal conditions only in few massifs from the Romanian Carpathians, the key periglacial processes are those associated with seasonal frost, which are widespread above the tree line. The present-day amplitude of solifluction, frost heaving or frost creep证实 发表于 2025-3-25 00:56:50
Thermal Weathering and Distribution of Mountain Rockwallsans most studies rely on air temperature when estimating the intensity of freeze-thaw cycles, comparative analysis of in situ ground thermal measurements shows that important differences occur in the thermal behaviour of mountain sectors and landforms. Specifically, air temperature fails to account