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发表于 2025-3-21 18:53:52
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粗糙
发表于 2025-3-21 20:28:51
2523-7489 frica’s mountain regions.Features hundreds of color photograResearch in recent years has increasingly shifted away from purely academic research, and into applied aspects of the discipline, including climate change research, conservation, and sustainable development. It has by now widely been recogn
象形文字
发表于 2025-3-22 01:45:40
Der lange Schatten des Contrat socialhumic Nitisols and Acrisols in case of the basement formations and the lower volcanic areas, and deep humic Andosols above about 2700 m (Mäckel 1986; Mäckel and Schultka 1988; Mäckel and Walter 1983, Schmitt 1991, Speck 1983).
Vsd168
发表于 2025-3-22 07:34:22
Ethnobotany of Mountain Regions: Eastern Africahumic Nitisols and Acrisols in case of the basement formations and the lower volcanic areas, and deep humic Andosols above about 2700 m (Mäckel 1986; Mäckel and Schultka 1988; Mäckel and Walter 1983, Schmitt 1991, Speck 1983).
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发表于 2025-3-22 10:35:28
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entail
发表于 2025-3-22 16:17:11
Ethnobotany of Mountain Regions: Africay leached soils are more widespread in Africa than on any other continent, and the huge relatively flat Savannahs are well known. Inselbergs are very characteristic remnants of the older surfaces in these plains, but far too low to merit treatment here.
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发表于 2025-3-22 17:54:33
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sorbitol
发表于 2025-3-23 01:14:21
Reference work 2021e, attendance at professional conferences has grown steadily, and the n.umber of professionals calling themselves ethnobotanists has increased significantly (the various societies (Society for Economic Botany, International Society of Ethnopharmacology, Society of Ethnobiology, International Society
解冻
发表于 2025-3-23 02:27:43
Ethnobotany of Mountain Regions: Africahe geology of pre-cambrian material (Petters 1991). Large areas, so-called cratons, have remained essentially unchanged since the early Proterozoic (~2000 MYA). The mobile belts, i.e., the huge basins and swells between these cratons, are composed of equally old rocks, but have been subject to defor
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发表于 2025-3-23 07:28:15
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