In 1950 a pilot borehole was put down for exploratory water supply purposes at the Smallburgh Rural District Council waterworks at Wateringpiece Lane, Catfield, near Ludham. Investigation of sediment samples was carried out for fossil foraminiferan content by Brian Funnell and for pollen by Colin Forbes. In 1959 the Royal Society of London financed a research borehole located 80 m to the east. It penetrated Pliocene and Pleistocene deposits of the Crag Group to a depth of 50 m, and found them resting on deposits of the EoceneLondon Clay Formation. Sediment samples were analysed for their fossil pollen, foraminiferan and molluscan content by Richard West, Brian Funnell and Peter Norton, and later by Martin Head and others for dinoflagellates This research has confirmed the value of the Ludham Borehole for understanding the Pliocene and Pleistocene geology of East Anglia, and for correlation with strata of equivalent age in the North Sea basin and north-west Europe. The findings have since been supplemented by the results from the Ormesby Borehole. The Ludham Borehole is the type site for the Ludhamian Stage which has been correlated with part of the Praetiglian Stage on the continent, and tentatively correlated with the transition of Marine Isotope Stages 97 to 96.
Stratigraphy
The borehole log has been given by West. It was considered that the sedimentary sequence between – 7.6 and –49.7 m depth clearly belonged to the Crag Group. The sequence above this was considered to resemble the uppermost division of Norwich Crag as described by Woodward, attributed to the Bure Valley Beds.
Fauna and flora
Molluscs
Work by Norton investigated the molluscan fossils from the Ludham Borehole. A sequence of six biostratigraphic assemblage zones was identified, and the results correlated with palaeontological research at this and other sites. It was noted by Norton that the molluscan fauna gave no indication of the clearly cyclical temperature changes evident from pollen and foraminiferal fossils in the Ludham sequence, and hence it was unreliable for palaeoclimatic interpretation.
Plants
A sequence of pollen assemblage zones was identified by West, which permitted the designation of five biostratigraphic stages. 1. Ludhamian, with temperate mixed coniferous/deciduous forest including Tsuga and Pterocarya; 2. Thurnian, a glacial stage with an oceanic heath type of vegetation; 3. Antian, with temperate mixed coniferous/deciduous forest including Tsuga and Pterocarya; 4. Baventian, a glacial stage more severe than the Thurnian, with the return of oceanic heaths; 5. An unnamed stage with temperate mixed coniferous/deciduous forest lacking Pterocarya and with only a few traces of Tsuga. These stages were provisionally correlated with Early Pleistocene stages in the Netherlands: the Ludhamian with the Tiglian, the Thurnian with Eburonian, the Antian with Waalian, and the Baventian with Menapian. The unnamed stage was later tentatively correlated with the Pastonian. Further work was later conducted on Ludham pollen samples, yielding evidence for input by British rivers into the Crag sedimentary sequence in the southern North Sea basin.
Dinoflagellates
assemblages were analysed by Wall & Dale, and were found to correspond with five facies associations in the sequence identified by West. More detailed work was later conducted by Head, permitting the identification of over 29 species.
Foraminifers
A sequence of seven foraminiferal assemblage zones were identified by Funnell on the basis of research into the Ludham Pilot Boring. Those from the lower part of the sequence were correlated with the Red Crag Formation and from the upper part with the Norwich Crag Formation. The uppermost zone had an arctic-type fauna correlated with the Weybourne Crag.
