On the Norfolk and Suffolk coasts artifacts have been found at Pakefield and Happisburgh 3, indicating the presence of hominid activity. These artifacts were assigned to the organic layers of the...Show moreOn the Norfolk and Suffolk coasts artifacts have been found at Pakefield and Happisburgh 3, indicating the presence of hominid activity. These artifacts were assigned to the organic layers of the Cromer Forest-bed Formation. Pakefield is dated to 700 ka and resembled a Mediterranean climate, while the Happisburgh 3 artifacts are associated with a temperate boreal climate with an age of 780 ka. Research in understanding the Palaeolandscape and climate needs to be conducted on the organic layers at the Norfolk and Suffolk coasts. In this paper the lower organic layer at Beeston has been investigated. The research in this paper identified the macrofossils of 200 cubic centimeters from the first ten centimeters of the top of the lower organic layer. The local vegetation is consistent with a Potometea community, the local environment is a flooded basin or back-swamp in a River delta with some marine influences, and the climate represents a temperate climate. Other research of the layer as a quickscan of macrofossils through the entire layer shows no significant change of vegetation in the layer. Therefore we can assume that the layer represents one distinguished type of vegetation. Pollen data in the 10-11 centimeters of the layer shows an abundance of boreal mixed forests with wetland conditions. The identified local environment, vegetation, and climate is also found in the West Runton Freshwater Bed (MIS 15-17) and Happisburgh 3 (MIS 21,25). The West Runton Freshwater Bed is part of the hypothetical “Ancaster River”. The resemblance in vegetation and climate of Happisburgh 3 and Beeston indicates a possible presence of hominid activity within the lower organic layer of Beeston. However, the presenceof hominids and age of the lower organic layer cannot yet be determined.Show less
