GM4.4 | Sea level and wave conditions proxies from Pliocene to Pleistocene interglacials: The state-of-the-art and future perspectives
EDI Poster session
Sea level and wave conditions proxies from Pliocene to Pleistocene interglacials: The state-of-the-art and future perspectives
Convener: Ciro Cerrone | Co-conveners: Denovan Chauveau, Nikos Georgiou, Kathrine Maxwell
Posters on site
| Attendance Tue, 16 Apr, 16:15–18:00 (CEST) | Display Tue, 16 Apr, 14:00–18:00
 
Hall X3
Posters virtual
| Attendance Tue, 16 Apr, 14:00–15:45 (CEST) | Display Tue, 16 Apr, 08:30–18:00
 
vHall X3
Tue, 16:15
Tue, 14:00
Interglacials are warm intervals in Earth's climatic history characterized by high global average temperatures, low land ice extension, and rising sea levels. Geological records from many sites around the globe allow the identification of several interglacials since the late Pliocene, each different in duration, sea level variability and wave intensity. The study of these periods became particularly pertinent to unravel sea-level oscillations, wave regime variations, and refine models of polar ice melting in the near future. Relative sea level (RSL) and wave conditions are reconstructed using sea-level proxies, which are formed in relationship to the past position of sea level (i.e., marine terraces, tidal notches, beach ridge systems, coral reef structures, upper limit of L. lithophaga burrows, storm deposits or elements combined). Although we have a comprehensive understanding of the global sea level dynamics during the current interglacial (Holocene), our knowledge of these dynamics during past interglacials remains limited. Hence, building a synthesis of sea level and wave conditions on a multi-millennial scale could help assess sea level impacts in a future warmer world.
This session invites the international sea level community to present studies broadly related to Plio-Pleistocene interglacials, and in particular on new field data, synthesis and databases, wave conditions proxies, extreme events (i.e., extreme waves, storms, coastal flooding), sea-level reconstructions, and coastal modelling. State-of-the-art of sea-level research during Early to Late Quaternary interglacials and beyond will better constrain projections of potential future warming scenarios. We also welcome contributions on: i) geochronology methods (i.e., U-series dating; Optically stimulated luminescence (OSL), Thermoluminescence (TL), infrared-stimulated luminescence (IRSL), Electron spin resonance dating (ESR) and amino acid racemization (AAR) and ii) remote sensing techniques applied to constrain sea-level proxies both in active and steady tectonic settings.

Posters on site: Tue, 16 Apr, 16:15–18:00 | Hall X3

Display time: Tue, 16 Apr, 14:00–Tue, 16 Apr, 18:00
Chairpersons: Ciro Cerrone, Denovan Chauveau, Nikos Georgiou
X3.58
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EGU24-8118
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ECS
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Denovan Chauveau, Nikos Georgiou, Ciro Cerrone, Silas Dean, Anne-Morwenn Pastier, and Alessio Rovere

Understanding past sea-level variations is essential to constrain future patterns of sea-level rise in response to warmer climate conditions. Due to good preservation and the possibility to use various geochemical methods to date fossil sea-level index points, the Last Interglacial (Marine Isotope Stage (MIS) 5e; 130-116 ka ago) is often regarded as one of the best climate analogs for a future slightly warmer climate. Some MIS 5e coastal stratigraphic sequences, especially fossil coral reefs in tectonically stable areas, are characterized by abrupt shifts in their geological facies or steps within the reef topography, which have been often interpreted as proxies for abrupt sea-level fluctuations within the interglacial. However, the observational evidence and magnitude of such abrupt changes are controversial. Here, we run nearly 50 thousand simulations of a 2D kinematic reef model that can reproduce reef growth and demise through time. Our aim is to investigate the parameter space, the sea-level scenarios, and the processes by which double-stepped MIS 5e fossil reefs can form. Our results show that the only sea-level history that could explain the generation of an emerged MIS 5e backstepped reef is an abrupt rise in sea level, followed by a short-term peak. Any other multiple-stepped stratigraphy can be explained by the interplay between accommodation space, marine erosion, and bedrock slope, rather than by abrupt changes in sea level. 

How to cite: Chauveau, D., Georgiou, N., Cerrone, C., Dean, S., Pastier, A.-M., and Rovere, A.: Sea level oscillations within the Last Interglacial: insights from coral reef stratigraphic forward modelling, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-8118, https://doi.org/10.5194/egusphere-egu24-8118, 2024.

X3.59
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EGU24-4885
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ECS
Huigyeong Ryu, Jun-Ho Lee, Hoi Soo Jung, and Jaeryul Shin

The study of marine terraces, which include a paleo-shoreline record, provides information on global sea level fluctuations and crustal uplift rates during the Late Quaternary period. This data is helpful in preparing for sea level rise in the upcoming 'Global boiling'. Currently, widely recognized sea level fluctuation curves are derived from oxygen isotope stages in ice cores and deep-sea cores. The data shows a 30-50m sea level fall during Marine Isotope Stage (MIS) 5d-5a. However, some studies conducted in various parts of the world have reported smaller declines in sea level than is commonly known. For instance, studies on the marine terraces of the east coast of the Korean Peninsula suggest that sea level may have been as low as -5 to -10 m during MIS5a and MIS5c. In this study, we investigated the marine deposits in Haenam, located on the southwestern coast of the Korean Peninsula. We found deposits in the sedimentary layers that correspond to MIS5c, which were located beneath layers formed during MIS5e. The age of the sediments was determined using optically stimulated luminescence (OSL) dating. Based on the altitude, formation process, and absolute age of the sediments, it is inferred that sea level was similar to the present during MIS5c in Haenam. Recent research on the southwestern coast of the Korean Peninsula has accumulated data on marine deposits formed during MIS5a and MIS5c. This paper presents the results of studies on sea level during MIS5a and MIS5c on the west and south coasts of the Korean Peninsula. This study suggests one perspective for MIS5a and MIS5c sea level across East Asia and to raise new questions. Specifically, the paper questions why sea levels are similar to present during what is known to be a glacial period. This study offers a fresh perspective on sea level fluctuations in East Asia and can improve our comprehension of the intricate correlation between sea level and climate change.

How to cite: Ryu, H., Lee, J.-H., Jung, H. S., and Shin, J.: The Sea Level during MIS5a, MIS5c in the Southwestern Coast of South Korea, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-4885, https://doi.org/10.5194/egusphere-egu24-4885, 2024.

X3.60
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EGU24-5716
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Highlight
Julius Jara Muñoz, Jurgen Mey, Roland Freisleben, Kevin Pedoja, and Daniel Melnick

TerraceM is an open-source software written in MATLAB for mapping and analyzing marine terraces. In this latest release, TerraceM-3 has undergone significant evolution, which leverages the capabilities of machine learning to introduce an automated marine terrace mapping feature. This new version includes a neural network that has been meticulously trained with over 1000 mapped marine terraces. This allows TerraceM-3 users to effortlessly map marine terraces and precisely determine their elevation through the automated mapping of their shoreline angles. In addition, TerraceM-3 incorporates two new functionalities: 1) Photon profile mapping, which includes mapping of satellite LiDAR profiles from the IceSat-2 mission, which broadens the applicability of TerraceM-3 beyond the availability of topographic data. 2) Indicative meaning calculator that accounts for the factors that can alter the initial sea-level position using global datasets (wave conditions and tidal ranges). This method facilitates the direct assessment of uncertainties in the reconstructions of the paleo-sea-level based on marine terraces. TerraceM-3 is a complete toolkit for researchers and students engaged in marine terrace analysis by offering a unique blend of numerical methods, statistical analyses techniques and additional enhanced functionalities to precisely map marine terraces and using them as markers of tectonic deformation.

How to cite: Jara Muñoz, J., Mey, J., Freisleben, R., Pedoja, K., and Melnick, D.: TerraceM 3.0: Advancing marine terrace mapping through integrated machine learning methods, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-5716, https://doi.org/10.5194/egusphere-egu24-5716, 2024.

X3.61
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EGU24-15894
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ECS
Silas Dean, Nikos Georgiou, Robert K. Poirier, William R. Doar III, Dominik Brill, Denovan Chauveau, Ciro Cerrone, and Alessio Rovere

The degree to which the Last Interglacial (Marine Isotope Stage 5e; ~125,000 Before Present) can serve as an analog for future sea-level rise caused by anthropogenic climate change is a matter of great importance. Refining knowledge of factors such as glacio-hydro-isostatic conditions and ice-sheet histories leading up to and since the Last Interglacial will help resolve this question, and well-constrained, well-dated indicators of relative sea level will provide crucial data towards this end. We conducted stratigraphic surveys on several well-exposed outcrops along the Intercoastal Waterway canal near Myrtle Beach, South Carolina, on the East Coast of the United States. In addition to photogrammetry records of the outcrop, optically stimulated luminescence analysis has produced new dates that provide information about sea level history during the Last Interglacial and subsequent interstadials, while also helping to clarify the complex local stratigraphic context, which consists of a series of coastal beach ridges and paleoshorelines left by highstands. The dates are linked to precisely constrained DGPS elevations referenced to the local hydrographic datum, a technique which has not been widely used in the study area. The new data will be preserved as sea-level index points in the format specified by the World Atlas of Last Interglacial Shorelines as part of the WARMCOASTS project and are an especially important contribution since they add additional points in a passive margin area considered to be tectonically stable since the investigated time period.

How to cite: Dean, S., Georgiou, N., Poirier, R. K., Doar III, W. R., Brill, D., Chauveau, D., Cerrone, C., and Rovere, A.: OSL Dated Sea-Level for MIS 5e Interglacial in South Carolina, United States, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-15894, https://doi.org/10.5194/egusphere-egu24-15894, 2024.

X3.62
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EGU24-16272
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Highlight
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Christine Authemayou, Pedro Luis Dunán Avila, Marion Jaud, Kevin Pedoja, Julius Jara Muñoz, Leandro Peñalver Hernández, France Floc'h, Stéphane Bertin, Arelis Nuñez Labañino, Pedro de Jesus Benítez Frometa, Hassan Ross Cabrera, pauline Letortu, Angel Raúl Rodríguez Valdés, Noel Coutín Lobaina, and Denovan Chauveau

To assess coastal hazard where Coastal boulder deposits (CBDs) are found, it is crucial to constrain the forces governing their emplacement: from either storms/tropical cyclones or tsunamis. Here we focus on the CBDs on the island of Cuba and the extreme climatic events responsible for their formation. Four sites are being studied to identify the CBDs produced during known hurricanes over the last fifty years.The selected CBDs are located on a low-lying coral reef terrace on the Cuban shore, emplaced by the Cuban hurricane of 1935, Lili hurricane of 1996 and Matthew hurricane of 2016. These meteorological events associated with reported geomorphological objects are analyzed to quantify the hydrodynamic parameters of such extreme events (maximum orbital velocity). Furthermore, the quantification of CBDs volume by stereophotogrammetry (using Agisoft Metashape Professional version 1.7.2) and CBDs density by water immersion method on samples allow us to use deterministic and theoretical approaches ( hydrodynamics equations of Nandasena et al., 2013, 2022 ) to assess the assumed associated hydrodynamic parameters (minimum flow velocity) responsible for the dislocation of the coral reef terraces and transport of the resulted boulders. Finally, we compare these velocities with ones  calculated from the meteorological  events to discuss the reliability of these approaches to determine the climatic or tsunamigenic origin of the past extreme waves from geomorphological analyses of CBDs.

How to cite: Authemayou, C., Dunán Avila, P. L., Jaud, M., Pedoja, K., Jara Muñoz, J., Peñalver Hernández, L., Floc'h, F., Bertin, S., Nuñez Labañino, A., Benítez Frometa, P. D. J., Ross Cabrera, H., Letortu, P., Rodríguez Valdés, A. R., Coutín Lobaina, N., and Chauveau, D.: Geomorphological signatures of known climatic extreme events and validation of theoritical emplacement approach: Boulders on Cuban low-lying Marine Terraces , EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-16272, https://doi.org/10.5194/egusphere-egu24-16272, 2024.

X3.63
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EGU24-16538
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ECS
Ciro Cerrone, Luca Lämmle, Giovanni Scicchitano, Archimedes Perez Filho, Denovan Chauveau, Nikos Georgiou, Silas Dean, and Alessio Rovere

Geological sea-level proxies, such as fossil intertidal or foreshore deposits, store fundamental information that allow reconstructing past changes in sea level, which may be used to evaluate the volume of ice sheets during past warm periods. Studies on Last Interglacial (LIG; Marine Isotope Stage 5e, ~ 125 ka) sea-level proxies are particularly important, as this highstand is a process analogue for the current interglacial, including warming caused by human greenhouse gas emissions. In fact, the LIG was characterized by slightly higher temperatures than the pre-industrial, that caused higher global sea level and, in turn, smaller ice-sheets.

This work was done in the framework of the WARMCOAST Project funded by the European Research Council (ERC) under the European Union’s Horizon 2020 Research and Innovative Program (Grant Agreement No. 802414). This part of the project aims at surveying new geological sea-level proxies along the western Atlantic Brazilian coast, from Rio Grande do Sul to São Paulo and in southern Bahia State. Classical geological and geomorphological surveys were carried out in the field. We collected several samples for OSL dating and micropaleontological analysis. Samples consist mostly of shallow-water marine sands of supposed LIG age. The elevation of each proxy has been measured by a GNSS RTK station with centimetric precision and referred to a local geoid model (MAPGEO2015).

In this work, we report the results of the field campaign along the Brazil coast and, the new data are interpreted in terms of Glacio-Isostatic Adjustment processes affecting the coasts since the Last Interglacial. 

How to cite: Cerrone, C., Lämmle, L., Scicchitano, G., Perez Filho, A., Chauveau, D., Georgiou, N., Dean, S., and Rovere, A.: Last Interglacial sea-level proxies along the Brazilian western Atlantic coasts, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-16538, https://doi.org/10.5194/egusphere-egu24-16538, 2024.

X3.64
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EGU24-17200
Alessio Rovere, Karla Rubio Sandoval, Deirdre D. Ryan, Sebastian Richiano, Luciana M. Giachetti, Andrew Hollyday, Jordon Bright, Evan J. Gowan, Marta Pappalardo, Jacqueline Austermann, and Darrell S. Kaufman

Geological indicators of past relative sea level changes are fundamental to reconstruct the extent of former ice sheet during past interglacials, which are considered analogs for future climate conditions. Four interglacials, dating from Holocene to Pliocene, have left sea-level imprints in the proximity of the coastal town of Camarones in Central Patagonia, Argentina. Sea-level index points were preserved as beach ridges deposited by storm waves above modern sea level. We used highly accurate survey techniques to measure the elevation of these deposits. Satellite-derived wave measurements and wave runup models were then employed to calculate their indicative meaning (i.e., their elevation with respect to sea level at the time of deposition). The paleo relative sea levels (i.e., uncorrected for post-depositional vertical land motions) associated with the four interglacials (with 1σ uncertainties) are 6±1.5 m (Holocene); 8.7±2.1 m (MIS 5e); 14.5±1.5 m (MIS 9 or 11); and 36.2±2.7 m (Early Pliocene). Ages have been obtained using both published (U-series, Electron Spin Resonance, and Radiocarbon) and new (Amino Acid Racemization and Radiocarbon) dating constraints. We compare our results with published glacial isostatic adjustment and mantle dynamic topography predictions, and we highlight that refining these models before calculating the global mean sea level for the interglacials mentioned above is necessary. Our high-resolution data provide a significant benchmark for paleo relative sea-level studies in the Southwestern Atlantic.

This project has received funding from the European Research Council (ERC) under the European Union’s Horizon 2020 re- search and innovation programme (grant agreement no. 802414)

How to cite: Rovere, A., Rubio Sandoval, K., Ryan, D. D., Richiano, S., Giachetti, L. M., Hollyday, A., Bright, J., Gowan, E. J., Pappalardo, M., Austermann, J., and Kaufman, D. S.: Quaternary and Pliocene sea-level changes at Camarones, central Patagonia, Argentina, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-17200, https://doi.org/10.5194/egusphere-egu24-17200, 2024.

X3.65
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EGU24-17311
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ECS
Lyndon Nawanao, Noelynna Ramos, Robelyn Mangahas, Hsun-Ming Hu, and Chuan-Chou Shen

Corals have been used as proxies of relative sea-level (RSL) change and key inputs in refining glacial isostatic adjustment (GIA) models globally. Along subduction zones, interseismic, coseismic, and postseismic processes act as local drivers of relative sea-level changes, which can also be used to elucidate past tectonic deformation. In this study, we present new radiometric (Th-230) ages of marine-limiting sea-level proxies (i.e., emerged fossil coral reefs) along the coasts of Southwest Panay Peninsula and Nogas Island facing the Negros Trench forearc. Real-time kinematic (RTK) GNSS and drone surveys were conducted to determine the elevations relative to the tide datum and the extent of the emerged fossil coral reefs. In the Southwest Panay Peninsula, emerged fossil coral reefs were observed at 4.20 m and 3.967–4.647 m above mean low low water (amllw), with Th-230 ages of 12.44 kya and 8.65–8.82 kya BP, respectively. About 15 km from the trench forearc, Mid-Holocene emerged fossil coral reefs dated 6.37–7.55 kya BP with elevations 1.596–2.810 m amllw. Late Holocene emerged fossil coral reefs were dated 4.33–1.48 kya BP with elevations 1.256–2.280 m amllw. On the western side of Nogas Island facing the trench forearc, emerged fossil coral reef platforms dated 1.08–1.66 kya BP with elevations 1.446–1.960 m amllw. The calculated RSL of these marine-limiting sea-level indicators is generally higher compared to the ICE-6G C and ICE-7G NA sea-level curve models and other coral proxies in Southeast Asia and Palawan that have relatively low tectonic deformation activities. In this study, we highlight the spatiotemporal variability of RSL coral proxies in local scales along the trench forearc. These initial results further imply active tectonic deformation induced along the Negros Trench since the Holocene. 

 

Keywords: fossil coral reefs, relative sea level, Holocene, Negros Trench forearc, Southwest Panay Peninsula, Nogas Island, Philippines

How to cite: Nawanao, L., Ramos, N., Mangahas, R., Hu, H.-M., and Shen, C.-C.: Early-to-Late Holocene Emerged Fossil Corals along the Negros Trench Forearc, Philippines, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-17311, https://doi.org/10.5194/egusphere-egu24-17311, 2024.

X3.66
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EGU24-20690
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ECS
Nikos Georgiou, Silas Dean, Alexander R. Simms, Denovan Chauveau, Ciro Cerrone, and Alessio Rovere

During past Interglacial periods, global ocean volume increased as a result of the higher temperatures and the melting of ice sheets, consequently leading to a rise in global sea levels. However, on timescales ranging from years to a few decades, regional sea level variability deviates from the global pattern, due to a combination of vertical land movements (earth’s crust viscoelastic response to glacial and ice sheet melting, tectonics), thermohaline circulation, wind forcing and land water storage. Therefore, decoding the regional sea-level variability during Interglacial periods is crucial for advancing climate models’ precision, especially for vulnerable coastlines.

Beach ridge plains are valuable fossil geological archives, offering significant potential for the analysis of sea-level fluctuations, climatic shifts and catastrophic events. The extraction of these information can be achieved through the measured elevation of the dune-beach contact and the beach berm, the analysis of the fossil beach ridge orientation, the geometry of the internal stratigraphy and by dating of the beach deposits using optically stimulated luminescence (OSL) signals from quartz.

In this study, we present results from our fieldwork campaign in the northern Gulf of Mexico, where we utilized a GNSS RTK station to obtain centimeter-level precision in measuring the elevation of the beach ridge sets, originally detected through freely available LIDAR datasets. Concurrently, a Ground Penetrating Radar (GPR) was employed to determine the stratigraphy of the beach ridge plains. Both surveyed areas, Apalachicola and Pensacola, contain fossil beach ridge sets varying in elevation from +2.5m up to a maximum of +7.5-8m above mean sea level, detected in more inland locations. Recent studies suggest that during the Last Interglacial period sea level in the area reached up to ~5m. The exact timing of the formation of the more elevated inland beach ridges remains uncertain, as does the question of whether their present elevation is attributable to post-Last Interglacial vertical land movements. Through in-depth analysis of the data collected during the WARMCOASTS ERC project, we aim to unravel the formation processes of these beach ridges and trace their development and evolution over time.

How to cite: Georgiou, N., Dean, S., Simms, A. R., Chauveau, D., Cerrone, C., and Rovere, A.: Interglacial beach ridge plains across the northern Gulf of Mexico, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-20690, https://doi.org/10.5194/egusphere-egu24-20690, 2024.

X3.67
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EGU24-21933
The long-term relationship between sea level and sediments in the Adriatic Sea
(withdrawn)
Paolo Stocchi

Posters virtual: Tue, 16 Apr, 14:00–15:45 | vHall X3

Display time: Tue, 16 Apr, 08:30–Tue, 16 Apr, 18:00
Chairpersons: Ciro Cerrone, Denovan Chauveau, Nikos Georgiou
vX3.6
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EGU24-8724
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Vincenzo De Santis, Paolo Montagna, Giovanni Scicchitano, Giuseppe Mastronuzzi, Edwige Pons Brancu, Giovanni Scardino, Josè Eugenio Ortiz, Yolanda Sanchez Palencia, Trinidad Torres, and Massimo Caldara

Geomorphological studies in the Ionian Sea margin of Apulia region (southern Italy) enabled the identification of

1) three terraced deposits: TD1, TD2, and TD3, divided in several sub-units;

2) three related palaeoshorelines: PS1, PS2, PS3.

The higher PS2 (30±2 m a.p.s.l.) dates to the first highstand of MIS 5.5. The ages of 127.851±1.47 and 128.4±26.2 ky BP from the sub-units of TD2 marking the transgression, suggest that at ca. 128 ky BP the transgression toward the first highstand of MIS 5.5 was still occurring.

The lower PS3 (19±2 m a.p.s.l.) dates to a second highstand of MIS 5.5. The age of 122.49 ±1.25 ky BP from TD3 is the most reliable chronological constraint for this second highstand.

Also considering the above mentioned contraints, and since it was not possible to attribute an absolute age for the TD2 sub-units which mark the first MIS 5.5 highstand, we adopt, in this paper, for the first highstand of MIS 5.5, the age given by Kopp et al. (2013), namely between 125 and 123 ky BP.

In particular we considered two possible scenarios:

1) scenario 1, assuming the first highstand of MIS 5.5 at 125 ky BP

2) scenario 2, assuming the first highstand of MIS 5.5 at 123 ky BP

In both scenarios, we considered a mean sea level value during the first highstand of MIS 5.5 at + 7.5±1.5 m. We then calculated the uplift rate of PS2 for both scenarios, assuming a constant rate up to present.

With these assumptions, we tentatively calculate the position of PS3 at ⁓ 122 ky and of the dated layer of the lowest transgressive sub-unit of TD2 (today at +3.80 m, dated at ⁓ 128 ky BP), this latter assumed as deposited from 5 to 10 metres of water depth.

A mean uplift rate of ca. 0.18 mm/yr was quantified, with a minimum possible of 0.15 mm/yr and a maximum possible of 0.21 mm/yr, for both scenarios. This range of uplift rates fits well within the regional setting.

Accordingly, the mean elevation of PS3 at time of its formation (i.e., the sea level at ⁓122 ky BP, namely the second highstand of MIS 5.5) was -2.96 and -3.32 m for scenario 1 and 2, respectively. Taking into account all the uncertainties in PS2 and PS3 elevations, and in sea level at the first highstand of MIS 5.5, the whole range of the RSL values during the second highstand of MIS 5.5 is -8.38 to +2.45 m for scenario 1, and -8.79 to +2.15 m for scenario 2.

On the other hand, using the three possible values of uplift rate, we calculated also the position and then the sea level indicated by the dated layer at ⁓ 128 ky BP at Torre Castelluccia, which ranged from -5.5 to -18.08 m, with a mean value of -11.79 m.

Finally, we hypotesise that the observed alternating abundance of marine gastropods Bolma rugosa (Linneo) and Thetystrombus latus (Gmelin) across the recognised deposits can be interpreded as a palaeoclimatic indicator, although in a merely qualitative way and, for now, only in the study area.

 

 

 

How to cite: De Santis, V., Montagna, P., Scicchitano, G., Mastronuzzi, G., Pons Brancu, E., Scardino, G., Ortiz, J. E., Sanchez Palencia, Y., Torres, T., and Caldara, M.: Two highstands during the last interglacial: insights from palaeoshorelines and marine terraced deposits of ionian coast of Apulia, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-8724, https://doi.org/10.5194/egusphere-egu24-8724, 2024.

vX3.7
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EGU24-21053
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Highlight
Potential resilient of the Mediterranean coastal plains to climate change: from past to future
(withdrawn)
Gaia Mattei, Angela Rizzo, Matteo Vacchi, and Pietro Patrizio Ciro Aucelli