MARINE AND FISHERY SCIENCES 37 (1): 233-240 (2024)
https://doi.org/10.47193/mafis.3712024010102
ABSTRACT. Radar images are commonly applied to recognize and monitor oil seeps on surface
waters over continental shelves. In San Jorge Gulf, Patagonia, between 46° S and 48° S, oil slicks
have been surveyed performing ellipse patterns in response to mesotidal dynamics. These effects
were assigned to recent episodic increments of summer bottom temperatures at depths between 100
and 120 m, which are 2 °C warmer than those recorded during the 20th century. Slicks are assumed
to have their origin from faults already known by the oil industry onshore. The effects here
described should be envisaged in a climate-change scenario leading to temperature increases of the
oceans’ shallow waters, together with other effects such as the human-induced global sea level rise.
Under such warmer conditions seeps from continental shelf floors will become more frequent, and
their contribution to the atmospheric C budget should be globally assessed.
Key words: SAR images, continental shelf, Argentina.
Filtraciones de petróleo desde la plataforma patagónica: su destino termoestérico
RESUMEN. Las imágenes de radar se aplican comúnmente para reconocer y monitorear las fil-
traciones de petróleo en las aguas superficiales sobre las plataformas continentales. En el Golfo San
Jorge, Patagonia, entre los 46° S y 48° S, se han relevado manchas de petróleo que presentan patro-
nes de elipse en respuesta a la dinámica mesotidal. Estos efectos fueron asignados a incrementos
episódicos recientes de las temperaturas del fondo del verano a profundidades entre 100 y 120 m,
que son 2 °C más cálidas que las registradas durante el siglo XX. Se supone que las manchas tienen
su origen en fallas ya conocidas por la industria petrolera en tierra. Los efectos aquí descritos deben
contemplarse en un escenario de cambio climático que provoque un aumento de la temperatura de
las aguas poco profundas de los océanos, junto con otros efectos como el aumento global del nivel
del mar inducido por el hombre. Bajo tales condiciones más cálidas, las filtraciones de los suelos de
la plataforma continental serán más frecuentes y su contribución al balance de C atmosférico debe
evaluarse globalmente.
Palabras clave: Imágenes SAR, plataforma continental, Argentina.
Natural oil seeps have been surveyed at different locations worldwide. The
most accurate figure was about 6 ´105t y-1, although it could vary from 2 ´
105to 2 ´106t y-1 (Kvenvolden and Cooper 2003), while estimates of CH4
contributions to the atmosphere from geological sources indicated 45 Tg y-1
(Kvenvolden and Rogers 2005). Synthetic Aperture Radar (SAR) images are
233
*Correspondence:
fisla@mdp.edu.ar
Received: 7 June 2023
Accepted: 26 July 2023
ISSN 2683-7595 (print)
ISSN 2683-7951 (online)
https://ojs.inidep.edu.ar
Journal of the Instituto Nacional de
Investigación y Desarrollo Pesquero
(INIDEP)
This work is licensed under a Creative
Commons Attribution-
NonCommercial-ShareAlike 4.0
International License
Marine and
Fishery Sciences
MAFIS
NOTE
Oil seeps from the Patagonian shelf: their thermosteric fate
FEDERICO I. ISLA1, 2,* and LUIS C. CORTIZO1, 3
1Instituto de Geología de Costas y del Cuaternario (IGCC), Universidad Nacional de Mar del Plata (UNMDP), Comisión de Investigaciones
Científicas (CIC), Funes 3350, B7602AYL - Mar del Plata, Argentina. 2Instituto de Investigaciones Marinas y Costeras (IIMyC), Universidad
Nacional de Mar del Plata (UNMDP), Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET), Mar del Plata, Argentina.
3Comisión de Investigaciones Científicas (CIC), Buenos Aires, Argentina. ORCID Federico I. Isla https://orcid.org/0000-0002-4930-0907
progressively applied to detect and monitor oil
spills. Wavelengths of C-band are preferentially
applied to L and X-bands for detecting oil slicks
(Marghany 2014; Nunziata and Miglioaccio
2015; Asl et al. 2017; Jafarzadeh et al. 2021).
San Jorge Gulf has been reported as the most
polluted area of the Argentine coast. Highest
hydrocarbon concentrations are associated with
sandy sediments and gravel. This was primarily
attributed to the extraction and transportation of
oil through two loading buoys in Caleta Córdova
and Caleta Olivia (Commendatore et al. 2000)
(Figure 1). During the summer months of the
Southern Hemisphere (January), three oil spills
were detected close to San Jorge Gulf (Argentina)
between 2017 and 2023. They were not related to
known anthropogenic-triggered activities (spills);
instead, they were related to oil seeping from the
bottom of this productive basin. This paper
described and analysed the occurrence and possi-
ble causes of these oil slicks.
San Jorge Gulf is located in the eastern Patago-
nia between 44° S and 47° S. Provinces of Chubut
and Santa Cruz share the gulf. Tidal ranges
increase from 3.5 m at the outer edge to more than
5 m at the interior (Isla et al. 2002). The sedimen-
tary basin below the gulf has been producing oil
and gas since 1910, covering an area of 170,000
km2. San Jorge basin is known for its normal
faults, which are common for the Salamanca For-
mation (Foix et al. 2008). Oil extraction is related
to normal faults deepening 60°-65° prevailing E-
W and ESE-WNW alignments (Sylwan 2001;
Foix et al. 2008). The gulf was originated during
the Holocene sea-level transgression (Desiage et
al. 2023). Today, the sediment is supplied by cliffs
subjected to coastal erosion, and occasionally by
the wind (including ashfalls) and southerly
coastal currents (Desiage et al. 2018). The gulf
circulation is dominated by westerly winds and
tidal currents (Isla et al. 2002). Temporal variabil-
ity of the atmospheric heat flux increases from
spring to summer (Palma et al. 2020).
In order to map these slicks, Sentinel 1-A radar
images (C-band, 5.6 cm wavelength) were
processed from different areas of the outer shelf
of San Jorge Gulf during summer months. The
VV polarization procedure gave better results for
234 MARINE AND FISHERY SCIENCES 37 (1): 233-240 (2024)
Figure 1. Location of seeps and dates recorded by Sentinel radar images.
60°
42° 30'
47° 30'
S
W65°
those purposes than the HH polarization. The
WV-GRD acquisition mode was preferred for
scenes of 20 ´20 km, spatial resolution of 5 ´
20 m, and vertical angle between 23° and 36.5°.
The Copernicus Open Access Hub (European
Space Agency, ESA) and the Alaska Satellite
Facility of the National Aeronautics and Space
Administration (NASA) were accessed for this
research. Images from the interval 2015-2023
were analysed for different meteorological condi-
tions. Radiometric, geometric and speckle noise
(Lee Sigma and Frost) were performed with con-
version to decibels and geolocalization through a
Shuttle Radar Topography Mission (SRTM)
masking the land territories. The SNAP 8.0 (SeN-
tinel Applications Platform; ESA) program was
applied to get areas, perimeters and axis lengths
of darks stains (Marzialetti 2012). False positives
were assigned to surfactants liquids or biological
detritus. In order to analyse the occurrence of
these seeps during recent summers, the BARDO
statistical database (Baldoni et al. 2008) of the
Instituto Nacional de Investigación y Desarrollo
Pesquero (INIDEP, Argentina) was consulted
(https://www.inidep.edu.ar/datos-oceanograficos).
Oil seeps were registered out of San Jorge Gulf
during summer months of the southern hemi-
sphere (January 2018, January 2019 and January
2023). Seeps of 2018 were reported by CGG
Geoconsulting (2019). As the area is subjected to
tidal ranges between 2 and 4 m, seeps configure
ellipses with longer axis between 3 and 5 km
(Figure 2). A careful examination denoted that
some of these ellipses were oriented into lines.
Episodic temperatures three degrees warmer
were recorded since the year 2000 at 120 m depth
(Figure 3).
As slicks were distributed along lines or in
clusters, they were assigned to faults that are evi-
dent at cliffs (Figure 4) and that have been detect-
ed by reflective seismic (Fígari et al. 1999). Com-
paring beach samplings performed between 1989
and 1995, highest values were recognised at Cale-
ta Córdova and Comodoro Rivadavia, although
no spills were related to these anomalous values
(Commendatore et al. 2000). However, episodic
natural spills at the outer gulf could explain these
higher values.
Although oil seeps have been surveyed at the
Argentine Exclusive Economic Zone (EEZ)
(CGG Geoconsulting 2019), no prospection was
carried out offshore San Jorge Gulf. Biological
impacts of oil pollution in San Jorge Gulf were
already analysed considering them of anthro-
pogenic origin (Klotz et al. 2018).
Significant changes in the deep water tempera-
ture of oceans have been reported worldwide
(Abraham et al. 2013). It was also postulated that
235
ISLA AND CORTIZO: SAN JORGE GULF OIL SEEPS
Figure 2. Partial ellipses from the outer area of San Jorge Gulf captured by radar Sentinel 1A, band C, image taken at 9.10 AM
local time. A) January 29, 2018 (major axis 3.4 km). B) January 11, 2019 (major axis 5 km). C) January 13, 2023.
2018 2019 2023
AB
C
increments of intermediate water temperatures
could release hydrocarbon gas along the Gulf
Stream current to the uppermost planet cycle
(Phrampus and Horbach 2012). The Argentine
shelf is assumed to be warming in the last years
with a possible migration of the convergence of
Brazil and Malvinas currents due to a southwards
displacement of Brazil current (Risaro et al. 2022;
Chidichimo et al. 2022).
Increase in the tidal ranges could lead to an
increase in the buoyancy of shallow-shelf oil
accumulations (Idier et al. 2017; Pickering et al.
2017). Some models have been proposed to
explain the behaviour of seeps in the Gulf of
Mexico (Asl et al. 2017).
The upward velocity of droplets produced at
the bottom depends on temperature, salinity (both
as function of depths) and the diameter size of
droplets (Najoui et al. 2018). Considering the sea-
level rise trends expected for the next century
(Oppenheimer et al. 2019), it is concluded that
the buoyancy will increase and seeps will there-
fore be more frequent.
In the case of San Jorge Gulf, faults are con-
duits for hydrocarbons to reach the bottom (Figure
5). In Punta Peligro, sediment-filled fissures filled
with friable, fine-grained sandstone strata, suitable
for liquefaction/fluidization processes (Rio Chico
Formation) (Foix et al. 2008) gave idea of the
seepage probability of recurrence. According to
the hook-shaped of the spills in January 29, 2018
and January 11, 2019, it would take at least 3 h the
reversal of tides to produce those shapes. Faults
were also reported to cause natural oil seeps mon-
itored from Lower Congo Basin (Jatiault et al.
2017). According to a collection of SAR images,
these spills lasted 3.25 h in relation to the wind
speed. Considering wind statistics along the year
it was estimated that this site was supplying
4,380 m3y-1 to the ocean surface and therefore
considered the third biggest supply province from
natural leakage (Jatiault et al. 2017). Applying
ENVISAT-ASAR images from the South China
Sea, it is rather difficult to know whether spills
have been generated by gas hydrates or petroleum
seeps (Wang et al. 2013). Although anthropogenic
oil spills have been drastically diminishing world-
wide in the last years (ITOPF 2022), oil tankers
activities (Kluser 2006) along the trip from
Buenos Aires to Tierra del Fuego are suspected of
illegally cleaning of their deposits.
CONCLUSIONS
1) Natural oil seeps were repeatedly detected
close to San Jorge Gulf during the summer
months.
236 MARINE AND FISHERY SCIENCES 37 (1): 233-240 (2024)
Figure 3. Water temperature records at different depths in
San Jorge Gulf. The circle highlights the anomalous
measurements (courtesy of INIDEP).
18
16
14
12
10
8
6
4
2
00 20 40 60 80 100 120 140
Z (m)
1960-1989 1990-1999
2000-2009 2010-2019
Temperature (°C)
237
ISLA AND CORTIZO: SAN JORGE GULF OIL SEEPS
Figure 4. Fault at the coast of San Jorge Gulf (modified after Foix et al. 2008).
Figure 5. Seepage explanation of San Jorge Gulf seepage processes (modified from Najoui et al. 2018).
Sea surface
Oil seep
Wind
Sea surface outbreak (SSO)
Water column
Deflection
Seafloor source (SFS)
Seafloor
Fault lineation
Tidal current
2) Anomalous bottom temperature increments in
the gulf have been detected since 2000.
3) C-band and VV polarization radar images were
the most useful to discriminate hydrocarbon
stains related to seeps.
4) The SNAP software permitted to approximate
the direction of these slicks and the wind
velocity at the moment of the image captures.
5) L-band images (Alos Palsar) were compared to
the C images showing less details due to the
longer wavelengths.
ACKNOWLEDGEMENTS
Authors are indebted to researchers from the
Physical Oceanography Lab of the INIDEP (Mar
del Plata, Argentina). CONAE kindly provided
the radar images. Two anonymous reviewers and
the editor made useful comments and sugges-
tions.
Author contributions
Federico I. Isla: conceptualization, investiga-
tion, supervision, validation, writing-original
draft, writing-review and editing. Luis C. Corti-
zo: image processing, formal analysis, investiga-
tion, methodology.
REFERENCES
ABRAHAM JP, BARINGER, M, BINDOFF, NL,
BOYER, T, CHENG, LJ, CHURCH, JA, CONROY,
JL, DOMINGUEZ, CM, FASULLO, JT, GILSON, J,
et al. 2013. A review of global ocean tempera-
ture observations: implications for ocean heat
content estimates and climate change. Rev
Geophys. 51: 450-483. DOI: https://doi.org/10.
1002/rog.20022
ASL SD, DUKHOOVSKOY DS, BOURASSA M, MAC-
DONALD IR. 2017. Hindcast modeling of oil
slick persistence from natural seeps. Remote
Sens Environ. 189: 96-107.
BALDONI A, MOLINARI G, GUERRERO RA, KRUK
M. 2008. Base regional de datos oceanográfi-
cos (BaRDO) INIDEP. Inf Invest INIDEP
13/2008. 25 p.
CHIDICHIMO MP, MARTOS P, ALLEGA L, BERGHOFF
C, BIANCHI AA, COZZOLINO E, DOGLIOTTI AI,
DRAGANI WC, FENCO H, FIORE M, et al. 2022.
Cambios físicos y geoquímicos en el Océano
Atlántico Sudoccidental. In: BURATTI CC,
CHIDICHIMO MP, CORTÉS F, GAVIOLA S, MAR-
TOS P, PROSDOCIMI L, SEITUNE D, VERÓN E,
editors. Estado del conocimiento de los efec-
tos del cambio climático en el Océano Atlánti-
co Sudoccidental sobre los recursos pesqueros
y sus implicancias para el manejo sostenible.
Buenos Aires: Ministerio de Agricultura,
Ganadería y Pesca. p. 27-81.
CGG GEOCONSULTING. 2019. NPA satellite map-
ping-oil exploration; Argentina 2018 seepage
study. [accessed 2023 Apr]. https://satellite
blog.cgg.com/seeps-confirm-potential-for-
offshore-argentina/.
COMMENDATORE MG, ESTEVES JL, COLOMBO JC.
2000. Hydrocarbons in coastal sediments of
Patagonia, Argentina: levels and probable
sources. Mar Pollut Bull. (40) 11: 989-998.
DESIAGE PA, MONTERO-SERRANO JC, ST-ONGE G,
CRESPI-ABRIL AC, GIARRATANO E, GIL MN,
HALLER MJ. 2018. Quantifying sources and
transport pathways of surface sediments in the
Gulf of San Jorge, central Patagonia (Argenti-
na). Oceanography. 31 (4): 92-103. DOI:
https://doi.org/10.5670/oceanog.2018.401
DESIAGE PA, ST-ONGE G, DUCHESNE MJ, MON-
TERO-SERRANO JC, HALLER MJ. 2023. Late
Pleistocene and Holocene transgression
inferred from the sediments of the Gulf of San
Jorge, central Patagonia, Argentina. J Quat
Sci. 38 (5): 629-646. DOI: https://doi.org/10.
1002/jqs.3511
238 MARINE AND FISHERY SCIENCES 37 (1): 233-240 (2024)
FIGARI E, STRELKOV E, LAFFITTE G, CID DE LA
PAZ MS, COURTADE S, CELAYA J, VOTTERO A,
LAFOURCADE P, MARTÍNEZ R, VILLAR H. 1999.
Los sistemas petroleros de la Cuenca del
Golfo San Jorge: síntesis estructural, estrati-
gráfica y geoquímica. IV Congreso de Explo-
ración y desarrollo de hidrocarburos. Actas IV
Congreso de Exploración y Desarrollo de
Hidrocarburos: Mar del Plata, Argentina, 18 al
21 de abril de 1999. Buenos Aires: Instituto
Argentino del Petróleo y del Gas. p. 197-237.
FOIX N, PAREDES JM, GIACOSA RE. 2008. Paleo-
earthquakes in passive-margin settings, an
example from the Paleocene of the Golfo San
Jorge Basin, Argentina. Sediment Geol. 205:
67-78.
IDIER D, PARIS F, LECOZANNET G, BOULAHYA F,
DUMAS F. 2017. Sea-level rise impacts on the
tides of the European Shelf. Cont Shelf Res.
137: 56-71.
ISLA, FI, IANTANOS N, ESTRADA, E. 2002. Playas
reflectivas y disipativas macromareales del
Golfo San Jorge. AAS Revista. 9 (2): 155-164.
[ITOPF] THE INTERNATIONAL TANKER OWNERS
POLLUTION FEDERATION LIMITED. 2022. Oil
tanker spill statistics 2021. London: ITOPF. 18
p. [accessed 2023 Apr]. https://www.itopf.org/
knowledge-resources/data-statistics/statistics/.
JAFARZADEH H, MAHDIANPARI M, HOMAYOUNI S,
MOHAMMADIMANESH F, DABBOOR M. 2021.
Oil spill detection from synthetic aperture
radar earth observations: a meta-analysis and
comprehensive review. GISci Remote Sens.
58 (7): 1022-1051. DOI: https://doi.org/10.10
80/15481603.2021.1952542
JATIAULT R, DHONT D, LONCKE L, DUBUCQ D.
2017. Monitoring of natural oil seepage in the
Lower Congo Basin using SAR observations.
Remote Sens Environ. 191: 258-272.
KLOTZ P, SCHLOSS IR, DUMONT D. 2018. Effects
of a chronic oil spill on the planktonic system
in San Jorge Gulf, Argentina: a one-vertical-
dimension modeling approach. Oceanogra-
phy. 31 (4): 81-91. DOI: https://doi.org/10.56
70/oceanog.2018.413
KLUSER S, RICHARD JP, GIULIANI G, DEBONO A,
PEDUZZI P. 2006. Illegal oil discharge in Euro-
pean seas. Environment Alert Bulletin. 7.
Geneva: UNEP/DEWA-Europe/GRID. 4 p.
https://unepgrid.ch/storage/app/media/
legacy/23/ew_oildischarge.en.pdf.
KVENVOLDEN KA, COOPER CK. 2003. Natural
seepage of crude oil into the marine environ-
ment. Geo Mar Let. 23: 140-146.
KVENVOLDEN KA, ROGERS BW. 2005. Gaia’s
breath-global methane exhalations. Mar Pet
Geol. 22: 579-590.
MARGHANY M. 2014. Oil spill pollution automat-
ic detection from MultiSAR satellite data
using genetic algorithm. In: MARGHANY M,
editor. Advanced geoscience remote sensing.
INTECH. p. 51-71. DOI: http://doi.org/10.577
2/58572
MARZIALETTI PA. 2012. Monitoreo de derrames
de hidrocarburos en cuerpos de agua mediante
técnicas de sensado remoto [thesis]. Córdoba:
Universidad Nacional de Córdoba. 141 p.
NAJOUI Z, RIAZANOFF S, DEFFONTAINES B, XAVIER
JP. 2018. Estimated location of the seafloor
sources of marine natural oil seeps from sea
surface outbreaks: a new “source path proce-
dure” applied to the northern Gulf of Mexico.
Mar Petrol Geol. 91: 190-201.
NUNZIATA F, MIGLIOCCIO M. 2015. Oil spill mon-
itoring and damage assessment via PolSAR
measurements. Aquatic Procedia. 3: 95-102.
OPPENHEIMER M, GLAVOVIC BC, JHINKEL J, VA N
DE WAL R, MAGNAN AK, ABD-ELGAWAD A,
CAI R, CIFUENTES-JARA M, DECONTO RM,
GHOSH T, et al. 2019. Sea level rise and impli-
cations for low-lying islands, coasts and com-
munities. In: PÖRTNER H-O, ROBERTS DC,
MASSON-DELMOTTE V, Z HAI P, TIGNOR M,
POLOCZANSKA E, MINTENBECK K, ALEGRÍA A,
NICOLAI M, OKEM E, et al. editors. IPCC spe-
cial report on the ocean and cryosphere in a
changing climate. Cambridge University
Press. p. 321-445.
239
ISLA AND CORTIZO: SAN JORGE GULF OIL SEEPS
PALMA ED, MATANO RP, TONINI MH, MARTOS P,
COMBES V. 2020. Dynamical analysis of the
oceanic circulation in the Gulf of San Jorge,
Argentina. J Mar Syst. 203: 103261.
PHRAMPUS BJ, HORNBACH MJ. 2012. Recent
changes to the Gulf Stream causing wide-
spread gas hydrate destabilization. Nature.
490: 7421.
PICKERING MD, HORSBURGH KJ, BLUNDELL JR,
HIRSCHI JJ, NICHOLS RJ, VERLAAN M, WELLS
NC. 2017. The impact of future sea-level rise
on the global tides. Cont Shelf Res. 142: 50-68.
RISARO DB, CHIDICHIMO MP, PIOLA AR. 2022.
Interannual variability and trends of sea sur-
face temperature around southern South
America. Front Mar Sci. 9: 829144.
SYLWAN CQ. 2001. Geology of the Golfo San
Jorge Basin, Argentina. J Iber Geol. 27: 123-
157.
WANG Y, CHEN D, SONG Z. 2013. Detecting sur-
face oil slick related to gas hydrate/petroleum
on the ocean bed of South China Sea by
ENVI/ASAR radar data. J Asian Earth Sci. 65:
21-26.
240 MARINE AND FISHERY SCIENCES 37 (1): 233-240 (2024)