TY - JOUR
T1 - Biosedimentary disturbances in shallow-water carbonate environments: An example from the Upper Hauterivian in the Lusitanian Basin
AU - Sá Caetano, Paulo do Carmo de
AU - Rocha, Rogério Eduardo Bordalo da
PY - 2012/1/1
Y1 - 2012/1/1
N2 - Highlights.► Paleoenvironmental significance of biological, chemical, magnetic markers in a lagoon.► Detrital input modifies benthic foraminifera associations and mode of life.► Activity of boring and micritizing organisms varies according to detrital input.► δ13C variations are explained by variation of photosynthesis activity and turbidity.► Detrital input is controlled by variations of rainfall on the continent.
AB - Highlights.► Paleoenvironmental significance of biological, chemical, magnetic markers in a lagoon.► Detrital input modifies benthic foraminifera associations and mode of life.► Activity of boring and micritizing organisms varies according to detrital input.► δ13C variations are explained by variation of photosynthesis activity and turbidity.► Detrital input is controlled by variations of rainfall on the continent.
KW - Hauterivian
KW - Facies
KW - Benthic foraminifera
KW - Paleoenvironments
KW - Shallow-marine carbonates
KW - Magnetic susceptibility
KW - Geochemistry
U2 - 10.1016/j.palaeo.2011.11.005
DO - 10.1016/j.palaeo.2011.11.005
M3 - Article
SN - 0031-0182
VL - 315
SP - 24
EP - 37
JO - Palaeogeography, Palaeoclimatology, Palaeoecology
JF - Palaeogeography, Palaeoclimatology, Palaeoecology
IS - NA
ER -