Ajm. Bory et Pp. Newton, Transport of airborne lithogenic material down through the water column intwo contrasting regions of the eastern subtropical North Atlantic Ocean, GLOBAL BIOG, 14(1), 2000, pp. 297-315
Downward particle fluxes were measured using deep-moored sediment traps dep
loyed in two regions of contrasting primary productivity levels (mesotrophi
c and oligotrophic) of the eastern subtropical North Atlantic Ocean. The hi
gh percentage of lithogenic material (similar to 20-30% on average) in the
particulate matter collected shows the regional significance of the atmosph
eric dust inputs originating from West Africa. The magnitudes of lithogenic
and biogenic fluxes decrease similar to 5-6 and similar to 8-9 fold, respe
ctively, from near the African margin (mesotrophic region) to the remote op
en ocean (oligotrophic region). These trophic differences seem to give rise
to differences in the characteristics of the downward transport of lithoge
nic material. At the oligotrophic site, the relatively low and slow export
of biogenic matter apparently limits and delays the removal of lithogenic p
articles delivered to surface waters from the atmosphere. In contrast, the
higher biological activity in the mesotrophic region seems to provide persi
stent conditions for an efficient and faster downward transport of the depo
sited lithogenic particles, and the temporal variability of lithogenic flux
es largely reflects that of the atmospheric dust inputs. Thus whether the t
emporal variability of the exported lithogenic flux in the water column fol
lows that of the atmospheric deposition appears to depend on the trophic st
atus. In the mesotrophic region the oft-observed linear relationship betwee
n lithogenic and particulate organic matter (hereinafter POM) fluxes breaks
down at high POM fluxes. This observation adds weight to the idea that lin
ear relationships between POM fluxes and some candidate proxies for POM tra
nsfer cannot be assumed when POM export is large. A high mesoscale variabil
ity of biogenic, but not lithogenic, fluxes in the water column of the meso
trophic region underscores the relevance of mesoscale studies for regional
estimates of export of biogenic material.