1 1 Diversity and spatial patterns of foraminiferal assemblages in the eastern Clarion– 2 Clipperton Zone (abyssal eastern equatorial Pacific) 3 4 5 6 7 Aurélie Goineaua, Andrew J Gooday* 8 9 10 11 National Oceanography Centre, Southampton, University of Southampton Waterfront Campus, 12 European Way, Southampton SO14 3ZH, UK 13 14 15 16 17 18 a Present address: 1, Rue du Champ de Foire, 44530 Guenrouët, France 19 20 *Corresponding author. E-mail address:
[email protected] (A.J. Gooday) 21 22 2 24 Abstract 25 Foraminifera are a major component of the abyssal meiofauna in parts of the eastern Pacific 26 Clarion-Clipperton Zone (CCZ) licensed by the International Seabed Authority for polymetallic 27 nodule exploration. We analysed the diversity and distribution of stained (‘live’) and unstained 28 (dead) assemblages (0-1 cm layer, >150-µm sieve fraction) in megacorer samples from 11 sites 29 (water depths 4051 - 4235 m) within three 30 x 30 km ‘strata’ in the United Kingdom 1 (UK1 30 Strata A and B; 5 and 3 samples, respectively) and Ocean Minerals Singapore (3 samples) 31 license areas and separated by distances of up to 28 km within a stratum and 224 km between 32 strata. Foraminiferal assemblage density, diversity and composition at the higher 33 taxon/morphogroup level were largely consistent between samples. Stained assemblages were 34 dominated (>86%) by single-chambered monothalamids, mainly spheres, tubes, komokiaceans 35 and forms that are difficult to categorise morphologically. Hormosinaceans were the most 36 common multichambered group (~10%), while calcareous taxa (mainly rotaliids) represented 37 only ~3.5% of stained tests.