Wolfteich, C. M.: Sattelite-derived sea surface temperature, mesoscale variability, and foraminiferal production in the North Atlantic, M.Sc., MIT and WHOI, Cambridge, MS, 91 pp., 1994.

Jonkers, L., Brummer, G.-J. A., Peeters, F. J. C., van Aken, H. M., and De Jong, M. F.: Seasonal stratification, shell flux, and oxygen isotope dynamics of left-coiling N. pachyderma and T. quinqueloba in the western subpolar North Atlantic, Paleoceanography, 25, PA2204; 2210.1029/2009PA001849, 2010.
Jonkers, L., van Heuven, S., Zahn, R., and Peeters, F. J. C.: Seasonal patterns of shell flux, δ18O and δ13C of small and large N. pachyderma (s) and G. bulloides in the subpolar North Atlantic, Paleoceanography, 28, 164-174, 10.1002/palo.20018, 2013.

Mohtadi, M., Steinke, S., Groeneveld, J., Fink, H. G., Rixen, T., Hebbeln, D., Donner, B., and Herunadi, B.: Low-latitude control on seasonal and interannual changes in planktonic foraminiferal flux and shell geochemistry off south Java: A sediment trap study, Paleoceanography, 24, PA1201, doi:10.1029/2008PA001636, 2009.

G. digitata changed to B. digitata, N. pachyderma sin changed to N. pachyderma, N. pachyderma dex changed to N. incompta, N. conglomerata changed to G. conglomerata

depth change, on average 97 % species counted

Rigual-Hernández, A. S., Sierro, F. J., Bárcena, M. A., Flores, J. A., and Heussner, S.: Seasonal and interannual changes of planktic foraminiferal fluxes in the Gulf of Lions (NW Mediterranean) and their implications for paleoceanographic studies: Two 12-year sediment trap records, Deep Sea Research Part I: Oceanographic Research Papers, 66, 26-40, http://dx.doi.org/10.1016/j.dsr.2012.03.011, 2012.

From 01/06/2000 clsoing day + 1 to bring in agreement with reported collecting period

Donner, B., Wefer, G., 1994. Flux and stable isotope composition of Neogloboquadrina pachyderma and other planktonic foraminifers in the Southern Ocean (Atlantic sector). Deep Sea Research Part I: Oceanographic Research Papers 41, 1733-1743.

depth change (only first year is from deep trap). absence of species other than pachyderma due to presence of polyna, water depth from ETOPO1