Glaucony in ocean-margin sequence stratigraphy (Oligocene-Pliocene, offshore New Jersey, USA; ODP Leg 174A) by Hesselbo, S, Huggett, J

“…Glaucony occurs in abundance in clinoform-top and clinoform-toe positions within Atlantic-margin depositional sequences (offshore New Jersey, U.S.A.; Oligocène to Pliocene). Thin section and backscatter scanning electron microscope (BSEM) analyses indicate that grains of glaucony commonly formed in situ within burrows in deep-water (600-1000 m), clinoform-toe settings; fragmentation of glaucony grains in the matrix is most likely to have occurred through animal disturbance (e.g., ingestion and displacement by burrowers). …”

Lentivector producer cell lines with stably expressed vesiculovirus envelopes by Tijani, M, Munis, AM, Perry, C, Sanber, K, Ferraresso, M, Mukhopadhyay, T, Themis, M, Nisoli, I, Mattiuzzo, G, Collins, MK, Takeuchi, Y

“…Interestingly, we showed that VSVind.G and other vesiculovirus G from the VSV New Jersey strain (VSVnj), Cocal virus (COCV), and Piry virus (PIRYV) could be constitutively expressed and supported lentivector production for up to 10 weeks. …”