Site U1385 | Site U1386 | Site U1387 | Site U1388 | Site U1389 | Site U1391
IODP Expedition 339:
Site U1390 Summary
PDF file is available for download.
Background and objectives
Site U1390 (proposed site GC-02B)
is located on the southern Iberian Margin (36°19.110'
N and 7°43.077' W) about 130 km W of the Spanish city of Cadiz, in a
water depth of 992 m. This is the second of two sites drilled in the "channels
and ridges" sector of the larger Cadiz Contourite
Depositional System (CDS). It is located near the western end of a sheeted
drift adjacent to the Guadalquivir Contourite Channel
~300 m above the channel floor, and approximately 20 km NW of the of the
Guadalquivir diapiric ridge.
This sheeted drift is known as the Guadalquivir drift, which is part
of a much larger middle-slope sheeted drift system that has been dissected by
several contourite channels. Site U1389 lies on the
Huelva drift, which is another dissected portion of this same system also under
the influence of Lower Core MOW (see "Summary" for U1389). On seismic profiles
it shows a well-layered internal acoustic structure with laterally extensive, mainly aggradational seismic depositional units. It lies unconformably above two earlier buried drifts that have been differentially tilted up towards the N adjacent to the tectonically elevated Guadalquivir Bank.
Our primary objective at this site was to recover the Pliocene-Quaternary sedimentary
succession close to and affected by tectonic uplift of the Guadalquivir Bank.
By penetrating the unconformities between the surface and buried drifts we have
been able to evaluate the timing of this tectonic activity and its effects on
drift sedimentation. The secondary objective was to further assess drift
sedimentation under the influence of the MOW Lower Core.
Site U1390 was occupied on 2 January 2012. Three holes were drilled and
cored using the advanced piston corer (APC) and the extended core barrel (XCB)
system, achieving the target depth of 350 mbsf in the first hole, U1390A. The
second and third holes were piston-cored to refusal. Downhole logging was
carried out at Hole U1390A using the Triple Combo and FMS-Sonic tool strings. Overall recovery for Site U1390 was 438 m (98%) with the APC and 248 m (91%) with the XCB. The total cored interval for Site U1390 was 719.5 m and total recovery was 686.3 m (95%).
our pre-drilling interpretation had assumed a relatively low rate of
sedimentation above base-Quaternary and mid-Pliocene unconformities, instead we
found very high rates of sedimentation under the influence of an active Lower
Core of the MOW. The unconformities
noted on seismic records, therefore, are much younger than expected. The basal unconformity of Guadalquivir drift is from 0.9-1.2 Ma, and the bottom of the hole reached to about 1.3 Ma.
sedimentary succession at Site U1390 extends for 350 m from the mid Pleistocene
to Holocene. It is represented by a very rapidly accumulated and uniform series
of contouritic sediment, which has been assigned to a
single lithostratigraphic unit that is divided into two
sub-units (Sub-Units IA and IB). Unit I is dominated by classic contourite deposition, including calcareous mud, silty mud, sandy mud and silty bioclastic sand lithologies. These are generally organized as bi-gradational sequences and partial sequences, of which base-cut-out normally-graded sequences are more common than top-cut-out inversely-graded sequences. Carbonate content ranges from 21-35%, and total organic carbon from 0.4-1.1%. The
division of Unit I into two subunits is based on a marked change at 290 mbsf in
the relative abundance and thickness of the silt/sand intervals. These are more
prominent in Sub-Unit IB, with the sandy facies
making up around 50% of the total.
Calcareous microfossils (nannofossils, planktonic and benthic
foraminifera, and ostracods) are mostly common to
abundant, with moderate to good preservation throughout. Pteropod
fragments are present sporadically. There
are two relatively short hiatuses from 0.3 to 0.6 Ma and 0.9 to 1.2 Ma, separating intervals with rapid rates of sedimentation: averaging 75 cm/ky above the upper hiatus and 85 cm/ky below. Holocene sedimentation rates are also very high – around 80 cm/ky. Although age constraints are not yet refined, it
appears that the rate below the lower hiatus exceeds 100 cm/ky.
This is the highest rate we know of for any contourite drift site.
There is a distinctive variability in benthic foraminifer assemblages, which reveals significant long-term trends as well as short-term cycles of environmental change. Comparable with other sites, the upper 0.9 My of the Quaternary shows typical upper bathyal assemblages indicative of increased organic matter
input and reduced ventilation. The remainder of the Pleistocene shows lower
nutrient supply and greater ventilation. The direct role and influence of the
MOW at this site requires further study. The shipboard palynological
study was carried out at a very coarse resolution but, as for other sites
drilled, shows dominance of the four main plant ecological groups that
characterize this region – Pinus, Mediterranean forest, semi-desert and grasslands.
Magnetostratigraphy proved difficult to resolve closely, in
part due to coring disturbance and in part due to presence of hiatuses at or
near critical polarity transitions. The upper 230 m of section is within the Brunhes chron, but the deeper
section requires more detailed shore-based study to resolve. Strong peaks in
magnetic susceptibility in these cores appear to correlate with large amounts
of diagenetic iron sulfides (presumably including greigite and pyrrhotite).
As has been observed at the other sites drilled during Expedition 339, physical property data show relatively
close tracking of magnetic susceptibility and bulk density in much but not all
of the section. These may correlate or anti-correlate with NGR values, and with
color reflectance (L* and a* values). Both larger-scale trends and smaller-scale cycles are evident, with some correlation at the small-scale with lithology.
The pore water profiles at Site U1390 show significantly higher concentrations of many elements (including Na, Cl, Ca, Mg, Sr
and NH3) than at any of the other sites drilled thus far, including
Site U1389 where the values reached a distinct maximum at around 530 mbsf. However, the high
chloride and sodium concentrations are associated with low δD values,
which indicates that high salinity may not be the result of in situ salt
dissolution. Instead, we suggest that salts were dissolved at depth by pore
waters that had been altered by clay mineral dehydration reactions, which can
also affect water sodium concentration.
measurements were made in Hole U1390A to a depth of 350 mbsf,
with good quality data obtained due to good hole conditions especially in the
upper 270 m. There is a distinct change in log characteristics at around 290
mbsf, which correlates closely with the lithostratigraphic
boundary between sub-units and with the change downhole to a more sand-rich
lithology. Distinct cyclicity is apparent in some
parts of the section, corresponding with both lithological and physical
properties data. Nine downhole temperature measurements were made in the top 110
m of section, yielding a geothermal gradient of 32.0 °C/km.
At Site U1390 we penetrated a 350 m section that extends from the mid
Pleistocene to Holocene. The site lies under the influence of Lower Core
MOW close to the Guadalquivir contourite channel, and
shows very high rates of sedimentation, both for the sand-rich and mud-rich
sections. With maximum rates of 85 cm/ky (and perhaps
in excess of 100 cm/ky), these are the highest known
for contourite drifts anywhere. As a result, some of
the contourite muds retain a distinctive lamination
(albeit discontinuous in character), while the thicker sands are especially
clean and well sorted. There are two important hiatuses, at around 0.4 and 0.9
Ma, which reflect episodes of enhanced bottom current flow, in part related to
tectonic adjustment of the local topography. Significantly, these hiatuses are
correlative across the Cadiz Contourite Depositional System on the basis of seismic stratigraphy, and are recognized as more minor
events at our other sites.