Depositional Sequences of Madagascar during the breakup of Gondwana
Markus Geiger, Jochen Kuss
DFG Project KU 642/18
Crustal extension and eventual separation of the eastern and western
part of the Gondwana supercontinent left imprints in the Jurassic sedimentary
record in the Morondava Basin of western Madagascar. The sedimentary successions
were studied with an interdisciplinary approach, based on interpretations
of sedimentary textures (outcrop) as well as microfacies interpretations
(outcrop and thin sections), stratigraphic studies (ammonites), palaeoecological
interpretations (macro- and microfossil), interpretations of the stratal
architectures (seismic images), provenance studies and resedimentation
studies (detrital apatite fission track analyses). Sedimentological and
stratigraphical analyses elucidate local and regional palaeo-environmental
perturbations and relative sea-level changes. Seismic images allow the
nature and temporal order of tectonic events to be interpreted. The combination
of sedimentological and seismic concepts results in a tectono-sedimentary
model of the breakup of Gondwana.
During the Late Carboniferous-Late Triassic extensional basins formed
all across Gondwana. In contrast to earlier concepts, in which Gondwana
breakup was seen as a multiphase, long-lasting process during Late Carboniferous-Late
Triassic times, the present study infers that the breakup episode can
be constrained to the Toarcian-Aalenian interval (late Early Jurassic).
Seismic images from the northern Morondava Basin illustrate that the Late
Carboniferous-Late Triassic Karoo succession is involved in breakup faulting
with fault block rotation and therefore is by definition a pre-breakup
strata. The typical syn-breakup strata are formed by the Andafia Formation
(Toarcian) and the Aalenian Sandstones, when they form divergent strata
of shales, limestones, and sandstones, deposited in half-grabens above
tilted blocks. Observations from outcrop also suggest a basinward repeating,
eastward-tilting of the strata and an eastward pinching out of the Andafia
Formation. The Andafia Formation in the Morondava Basin correlates with
strata of the Beronono Formation in the Majunga Basin. There, the oldest
syn-breakup deposits in Madagascar are classified to the Bouleiceras nitescens
Zone (Early Toarcian). A major unconformity, which is overlain by Early
Bajocian sediments, marks the end of this early syn-breakup phase, and
is followed by post-breakup deposits of the drift phase. The post-rift
phase is characterised by the initial formation of a coastal carbonate
platform (Bajocian), which extends along the entire continental margin
followed by a siliciclastic ramp system (Bathonian) and subsequently by
basinal shales and intercalating shallow water limestones (Callovian-Kimmeridgian).
During breakup rifting and drifting four major transgressive events, each
followed by a regression, were recognised to mainly follow eustatic sea-level
changes and to be only minor affected by regional tectonism:
- Early Toarcian
- Early Bajocian
- Early Callovian
- Early Oxfordian
The first transgressive-regressive (T-R) cycle coincided with the Toarcian
syn-breakup rifting. Apart from this three T-R cycles are documented in
the passive margin succession. An Early Bajocian transgression overstepped
the rift flank of the breakup eastwards far inland and covered Toarcian-Aalenian
syn-breakup rift strata and extensive parts of the pre-breakup Karoo strata.
At the same time a coastal carbonate platform attached to the newly formed
continental margin. Previous studies have failed to recognize the basin-wide
extent of the carbonate platform (mudstones, limestones, and oolites Bemaraha
Formation), because only the coastal equivalents (mudstones, limestones,
siltstones, and sandstones of the Sakaraha Formation) are exposed in the
southern Morondava Basin.
A major regressive event in the Early-Middle Bathonian resulted in a partial
exposure of basinal strata in the northern part of the Morondava Basin
(Stoakes and Ramanampisoa, 1988). There palaeokarstification and incised
valleys on top of the carbonate platform are known from seismic lines
in the north. At the same time shallow water siliciclastics were deposited
in the south to form the sandstone-dominated Ankazoabo and Sakanavaka
formations. The combination of basin exposure, incised valleys, and localised
siliciclastic wedges are interpreted as typical forced regression features.
A widespread transgressive unconformity introduces deeper marine conditions
again in the Early Callovian (Bullatus Zone) with mudstones, siltstones,
limestones, and a few iron-oolites at the base. Deeper basinal conditions
prevail, with the exception of prominent shallow water sandstones which
post-date the Athleta Zone (Late Callovian) and predate the Plicatilis
Zone (Middle Oxfordian). This “Oxfordian sandstone” documents
a short regression forcing the siliciclastic shoreline to prograde into
the basin. The base of the youngest Jurassic transgression of the southern
Morondava Basin (Plicatilis Zone) is characterised by the occurrence of
iron-oolitic limestones. Stratigraphically upwards mudstones and shales
are intercalated with bioclastic and iron-oolitic limestones.
The three post-rift T-R cycles are basically comparable with the second-order
cycles of the Tethys. Biostratigraphic bias of the Ankazoabo Formation
and of the “Oxfordian sandstone” hampers a precise comparison.
However, the Jurassic sea-level curves of both the Morondava Basin and
of the Tethys show strong similarities and suggest that the eustatic signal
is superimposed on the local sea-level curve.
The depositional concepts derived from studies at outcrop and subsurface
are complemented by the compilation of facies maps and isopach maps for
the Morondava Basin. Facies maps suggest a basinwide occurrence of the
Bajocian carbonate platform, whereas in contrast a pure siliciclastic
environment is present during the Oxfordian. Isopach maps of Bajocian-Bathonian
and Callovian-Tithonian intervals outline a strong difference in sediment
thickness in the southern part of the basin compared to the north. Both
time intervals imply two depocentres in the south-central part of the
basin, whereas in the north strata are thinner for a large area.
Palaeo-current indicators from the south Morondava Basin suggest a general
westward sediment transportation and a N-S trending shoreline during the
Middle and Late Jurassic. During the Bajocian-Bathonian a northward directed
transport is inferred at the very southern end of the Morondava Basin,
where local uplift is probable. During Oxfordian times, at the northern
edge of the southern central part of the basin, southward-directed palaeo-currents
may indicate an elevated basin margin. Evidence for slightly uplifted
marginal areas can also be found at the southern basin margin by the comparison
of stratigraphic ages of Bajocian-Callovian sediments with apatite fission
track (AFT) ages of detrital apatite grains. The stratigraphic order of
detrital AFT ages can only has been formed by a stratigraphic reversal,
possibly due to reworking of former Karoo deposits. The erosion of Karoo
sediments may refer to uplift of the margin of the breakup basin, which
is lined by Karoo deposits.
Considerations of biogeographical vicariance based on new ostracod data
indicate high endemism in Madagascar compared to East Africa and other
Jurassic findings. Spreading ridge formation and dysoxic basinal conditions
in the Proto-Indian Ocean formed a possible migration barrier between
Madagascar and the African coast.
Reappraisal of published regional ocean floor ages and consideration of
Middle Jurassic volcanism in the region suggests that the maximum age
of the Proto-Indian Ocean floor is approximately 180 Ma. This age corresponds
to the Toarcian time, which is considered to be the syn-breakup period.
Finally, the new perceptions of basin structure and stratal architecture,
as well as their development during the Jurassic can be compared to numerical
models of basin formation (Burov and Cloetingh, 1997; Cloetingh et al.,
1997; van Balen et al., 1995). Such comparisons indicate that during the
Jurassic the Morondava Basin of Madagascar was part of a non-volcanic,
fast spreading, narrow, passive rift which rift shoulder experienced no
considerable uplift.