Articles | Volume 21, issue 1
https://doi.org/10.5194/bg-21-49-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-21-49-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
03 Jan 2024
Research article |
| 03 Jan 2024
| 03 Jan 2024
Origin and role of non-skeletal carbonate in coralligenous build-ups: new geobiological perspectives in biomineralization processes
Mara Cipriani
Department of Biology, Ecology and Earth Sciences, University of Calabria, Via P. Bucci, cubo 15b, 87036, Rende, Cosenza, Italy
Carmine Apollaro
Department of Biology, Ecology and Earth Sciences, University of Calabria, Via P. Bucci, cubo 15b, 87036, Rende, Cosenza, Italy
Daniela Basso
Department of Earth and Environmental Sciences, University of Milano-Bicocca, Piazza dell'Ateneo Nuovo, 1, 20126, Milan, Italy
CoNISMa, National Inter-University Consortium for Marine Sciences, Piazzale Flaminio, 9, 00196, Rome, Italy
Pietro Bazzicalupo
Department of Earth and Environmental Sciences, University of Milano-Bicocca, Piazza dell'Ateneo Nuovo, 1, 20126, Milan, Italy
Marco Bertolino
Department of Earth, Environmental and Life Sciences, University of Genoa, 16126, Genoa, Italy
Valentina Alice Bracchi
Department of Earth and Environmental Sciences, University of Milano-Bicocca, Piazza dell'Ateneo Nuovo, 1, 20126, Milan, Italy
CoNISMa, National Inter-University Consortium for Marine Sciences, Piazzale Flaminio, 9, 00196, Rome, Italy
Fabio Bruno
Department of Mechanical, Energy and Management Engineering, University of Calabria, Via P. Bucci, cubo 45, 87036, Rende, Cosenza, Italy
Gabriele Costa
AGRIS Sardegna, Agricultural Research Agency of Sardinia, S.S. 291 Sassari-Fertilia, 07100, Bonassai, Sassari, Italy
Rocco Dominici
Department of Biology, Ecology and Earth Sciences, University of Calabria, Via P. Bucci, cubo 15b, 87036, Rende, Cosenza, Italy
Alessandro Gallo
Department of Mechanical, Energy and Management Engineering, University of Calabria, Via P. Bucci, cubo 45, 87036, Rende, Cosenza, Italy
Maurizio Muzzupappa
Department of Mechanical, Energy and Management Engineering, University of Calabria, Via P. Bucci, cubo 45, 87036, Rende, Cosenza, Italy
Antonietta Rosso
CoNISMa, National Inter-University Consortium for Marine Sciences, Piazzale Flaminio, 9, 00196, Rome, Italy
Department of Biological, Geological and Environmental Sciences, University of Catania, Corso Italia, 57, 95129, Catania, Italy
Rossana Sanfilippo
CoNISMa, National Inter-University Consortium for Marine Sciences, Piazzale Flaminio, 9, 00196, Rome, Italy
Department of Biological, Geological and Environmental Sciences, University of Catania, Corso Italia, 57, 95129, Catania, Italy
Francesco Sciuto
CoNISMa, National Inter-University Consortium for Marine Sciences, Piazzale Flaminio, 9, 00196, Rome, Italy
Department of Biological, Geological and Environmental Sciences, University of Catania, Corso Italia, 57, 95129, Catania, Italy
Giovanni Vespasiano
Department of Biology, Ecology and Earth Sciences, University of Calabria, Via P. Bucci, cubo 15b, 87036, Rende, Cosenza, Italy
Department of Biology, Ecology and Earth Sciences, University of Calabria, Via P. Bucci, cubo 15b, 87036, Rende, Cosenza, Italy
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Chiara Santinelli, Silvia Valsecchi, Simona Retelletti Brogi, Giancarlo Bachi, Giovanni Checcucci, Mirco Guerrazzi, Elisa Camatti, Stefano Caserini, Arianna Azzellino, and Daniela Basso
Biogeosciences, 21, 5131–5141, https://doi.org/10.5194/bg-21-5131-2024, https://doi.org/10.5194/bg-21-5131-2024, 2024
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Ocean liming is a technique proposed to mitigate ocean acidification. Every action we take has an impact on the environment and the effects on the invisible world are often overlooked. With this study, we show that lime addition impacts the dynamics of dissolved organic matter, one of the largest reservoirs of carbon on Earth, representing the main source of energy for marine microbes. Further studies to assess the impacts on marine ecosystems are therefore crucial before taking any action.
Li-Qing Jiang, Adam V. Subhas, Daniela Basso, Katja Fennel, and Jean-Pierre Gattuso
State Planet, 2-oae2023, 13, https://doi.org/10.5194/sp-2-oae2023-13-2023, https://doi.org/10.5194/sp-2-oae2023-13-2023, 2023
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This paper provides comprehensive guidelines for ocean alkalinity enhancement (OAE) researchers on archiving their metadata and data. It includes data standards for various OAE studies and a universal metadata template. Controlled vocabularies for terms like alkalinization methods are included. These guidelines also apply to ocean acidification data.
Ulf Riebesell, Daniela Basso, Sonja Geilert, Andrew W. Dale, and Matthias Kreuzburg
State Planet, 2-oae2023, 6, https://doi.org/10.5194/sp-2-oae2023-6-2023, https://doi.org/10.5194/sp-2-oae2023-6-2023, 2023
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Mesocosm experiments represent a highly valuable tool in determining the safe operating space of ocean alkalinity enhancement (OAE) applications. By combining realism and biological complexity with controllability and replication, they provide an ideal OAE test bed and a critical stepping stone towards field applications. Mesocosm approaches can also be helpful in testing the efficacy, efficiency and permanence of OAE applications.
Valentina Beccari, Ahuva Almogi-Labin, Daniela Basso, Giuliana Panieri, Yizhaq Makovsky, Irka Hajdas, and Silvia Spezzaferri
J. Micropalaeontol., 42, 13–29, https://doi.org/10.5194/jm-42-13-2023, https://doi.org/10.5194/jm-42-13-2023, 2023
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Planktonic gastropods (pteropods and heteropods) have been investigated in cores collected in the eastern Mediterranean along the Israeli coast in coral, pockmark, and channel areas. The sediment spans the last 5300 years. Our study reveals that neglecting the smaller fraction (> 63 µm) may result in a misinterpretation of the palaeoceanography. The presence of tropical and subtropical species reveals that the eastern Mediterranean acted as a refugium for these organisms.
Robin Fentimen, Eline Feenstra, Andres Rüggeberg, Efraim Hall, Valentin Rime, Torsten Vennemann, Irka Hajdas, Antonietta Rosso, David Van Rooij, Thierry Adatte, Hendrik Vogel, Norbert Frank, and Anneleen Foubert
Clim. Past, 18, 1915–1945, https://doi.org/10.5194/cp-18-1915-2022, https://doi.org/10.5194/cp-18-1915-2022, 2022
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The investigation of a 9 m long sediment core recovered at ca. 300 m water depth demonstrates that cold-water coral mound build-up within the East Melilla Coral Province (southeastern Alboran Sea) took place during both interglacial and glacial periods. Based on the combination of different analytical methods (e.g. radiometric dating, micropaleontology), we propose that corals never thrived but rather developed under stressful environmental conditions.
Giulia Piazza, Valentina A. Bracchi, Antonio Langone, Agostino N. Meroni, and Daniela Basso
Biogeosciences, 19, 1047–1065, https://doi.org/10.5194/bg-19-1047-2022, https://doi.org/10.5194/bg-19-1047-2022, 2022
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The coralline alga Lithothamnion corallioides is widely distributed in the Mediterranean Sea and NE Atlantic Ocean, where it constitutes rhodolith beds, which are diversity-rich ecosystems on the seabed. The boron incorporated in the calcified thallus of coralline algae (B/Ca) can be used to trace past changes in seawater carbonate and pH. This paper suggests a non-negligible effect of algal growth rate on B/Ca, recommending caution in adopting this proxy for paleoenvironmental reconstructions.
Valentina Alice Bracchi, Giulia Piazza, and Daniela Basso
Biogeosciences, 18, 6061–6076, https://doi.org/10.5194/bg-18-6061-2021, https://doi.org/10.5194/bg-18-6061-2021, 2021
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Ultrastructures of Lithothamnion corallioides, a crustose coralline alga collected from the Atlantic and Mediterranean Sea at different depths, show high-Mg-calcite cell walls formed by crystals with a specific shape and orientation that are unaffected by different environmental conditions of the living sites. This suggests that the biomineralization process is biologically controlled in coralline algae and can have interesting applications in paleontology.
Robin Fentimen, Eline Feenstra, Andres Rüggeberg, Efraim Hall, Valentin Rime, Torsten Vennemann, Irka Hajdas, Antonietta Rosso, David Van Rooij, Thierry Adatte, Hendrik Vogel, Norbert Frank, Thomas Krengel, and Anneleen Foubert
Clim. Past Discuss., https://doi.org/10.5194/cp-2020-82, https://doi.org/10.5194/cp-2020-82, 2020
Manuscript not accepted for further review
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This study describes the development of a cold-water Coral mound in the southeast alboran sea over the last 300 ky. Mound development follows interglacial-glacial cycles.
F. Bruno, A. Lagudi, L. Barbieri, M. Cozza, A. Cozza, R. Peluso, B. Davidde Petriaggi, R. Petriaggi, S. Rizvic, and D. Skarlatos
Int. Arch. Photogramm. Remote Sens. Spatial Inf. Sci., XLII-2-W10, 45–51, https://doi.org/10.5194/isprs-archives-XLII-2-W10-45-2019, https://doi.org/10.5194/isprs-archives-XLII-2-W10-45-2019, 2019
F. Bruno, A. Lagudi, M. Collina, S. Medaglia, B. Davidde Petriaggi, R. Petriaggi, S. Ricci, and C. Sacco Perasso
Int. Arch. Photogramm. Remote Sens. Spatial Inf. Sci., XLII-2-W10, 53–59, https://doi.org/10.5194/isprs-archives-XLII-2-W10-53-2019, https://doi.org/10.5194/isprs-archives-XLII-2-W10-53-2019, 2019
Related subject area
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Serpulid microbialitic bioherms from the upper Sarmatian (Middle Miocene) of the central Paratethys Sea (NW Hungary) – witnesses of a microbial sea
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Calcification response of planktic foraminifera to environmental change in the western Mediterranean Sea during the industrial era
Nature and origin of variations in pelagic carbonate production in the tropical ocean since the mid-Miocene (ODP Site 927)
Variation in calcification of Reticulofenestra coccoliths over the Oligocene–Early Miocene
The influence of near-surface sediment hydrothermalism on the TEX86 tetraether-lipid-based proxy and a new correction for ocean bottom lipid overprinting
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Anthropogenically induced environmental changes in the northeastern Adriatic Sea in the last 500 years (Panzano Bay, Gulf of Trieste)
Palaeohydrological changes over the last 50 ky in the central Gulf of Cadiz: complex forcing mechanisms mixing multi-scale processes
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Millennial changes in North Atlantic oxygen concentrations
Vanishing coccolith vital effects with alleviated carbon limitation
Late Pleistocene glacial–interglacial shell-size–isotope variability in planktonic foraminifera as a function of local hydrography
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Ruby Barrett, Joost de Vries, and Daniela N. Schmidt
Biogeosciences, 22, 791–807, https://doi.org/10.5194/bg-22-791-2025, https://doi.org/10.5194/bg-22-791-2025, 2025
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Planktic foraminifers are a plankton whose fossilised shell weight is used to reconstruct past environmental conditions such as seawater CO2. However, there is debate about whether other environmental drivers impact shell weight. Here we use a global data compilation and statistics to analyse what controls their weight. We find that the response varies between species and ocean basin, making it important to use regional calibrations and consider which species should be used to reconstruct CO2.
Wanli Xiang, Jan-Peter Duda, Andreas Pack, Mark van Zuilen, and Joachim Reitner
Biogeosciences, 21, 5653–5684, https://doi.org/10.5194/bg-21-5653-2024, https://doi.org/10.5194/bg-21-5653-2024, 2024
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We investigated the formation of early Archean (~3.5–3.4 Ga) carbonates in the Pilbara Craton, Western Australia, demonstrating the presence of an oceanic crust, an organo-carbonate, and a microbial carbonate factory. Notably, (a)biotic organic matter and hydrothermal fluids were centrally involved in carbonate precipitation. Since carbonates were widespread in the Archean, they may have constituted major carbon sinks that modulated early Earth’s carbon cycle and, hence, climate system.
Konstantina Agiadi, Iuliana Vasiliev, Geanina Butiseacă, George Kontakiotis, Danae Thivaiou, Evangelia Besiou, Stergios Zarkogiannis, Efterpi Koskeridou, Assimina Antonarakou, and Andreas Mulch
Biogeosciences, 21, 3869–3881, https://doi.org/10.5194/bg-21-3869-2024, https://doi.org/10.5194/bg-21-3869-2024, 2024
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Seven million years ago, the marine gateway connecting the Mediterranean Sea with the Atlantic Ocean started to close, and, as a result, water circulation ceased. To find out how this phenomenon affected the fish living in the Mediterranean Sea, we examined the changes in the isotopic composition of otoliths of two common fish species. Although the species living at the surface fared pretty well, the bottom-water fish starved and eventually became extinct in the Mediterranean.
Rafał Nawrot, Martin Zuschin, Adam Tomašových, Michał Kowalewski, and Daniele Scarponi
Biogeosciences, 21, 2177–2188, https://doi.org/10.5194/bg-21-2177-2024, https://doi.org/10.5194/bg-21-2177-2024, 2024
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The youngest fossil record is a crucial source of data on the history of marine ecosystems and their long-term alteration by humans. However, human activities that reshape ecosystems also alter sedimentary and biological processes that control the formation of the geological archives recording those impacts. Thus, humans have been transforming the marine fossil record in ways that affect our ability to reconstruct past ecological and climate dynamics.
Johan Renaudie and David B. Lazarus
EGUsphere, https://doi.org/10.5194/egusphere-2023-3087, https://doi.org/10.5194/egusphere-2023-3087, 2024
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We provide a new compilation of rates at which sediments deposited in the deep sea over the last 70 million years. We highlight a bias, linked to the drilling process, that makes it more likely for high rates to be recovered for younger sediments than for older ones. Correcting for this bias, the record show, contrary to previous estimates, a more stable history, thus providing some insights on the past mismatch between physico-chemical model estimates and observations.
Mariem Saavedra-Pellitero, Karl-Heinz Baumann, Nuria Bachiller-Jareno, Harold Lovell, Nele Manon Vollmar, and Elisa Malinverno
EGUsphere, https://doi.org/10.5194/egusphere-2023-2801, https://doi.org/10.5194/egusphere-2023-2801, 2023
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In this manuscript we combine micropalaeontology and remote-sensing. We compare the calcium carbonate produced by tiny marine algae called coccolithophores to satellite-derived particulate organic carbon in the Southern Ocean. They show good agreement north of the polar front, but hugely differ south of it. We argue that those highly reflective values could be due to small opal particles and we highlight the need to improve satellite algorithms in this unexplored part of the ocean.
Mathias Harzhauser, Oleg Mandic, and Werner E. Piller
Biogeosciences, 20, 4775–4794, https://doi.org/10.5194/bg-20-4775-2023, https://doi.org/10.5194/bg-20-4775-2023, 2023
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Bowl-shaped spirorbid microbialite bioherms formed during the late Middle Miocene (Sarmatian) in the central Paratethys Sea under a warm, arid climate. The microbialites and the surrounding sediment document a predominance of microbial activity in the shallow marine environments of the sea at that time. Modern microbialites are not analogues for these unique structures, which reflect a series of growth stages with an initial “start-up stage”, massive “keep-up stage” and termination of growth.
Walid Naciri, Arnoud Boom, Matthew Payne, Nicola Browne, Noreen J. Evans, Philip Holdship, Kai Rankenburg, Ramasamy Nagarajan, Bradley J. McDonald, Jennifer McIlwain, and Jens Zinke
Biogeosciences, 20, 1587–1604, https://doi.org/10.5194/bg-20-1587-2023, https://doi.org/10.5194/bg-20-1587-2023, 2023
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In this study, we tested the ability of massive boulder-like corals to act as archives of land use in Malaysian Borneo to palliate the lack of accurate instrumental data on deforestation before the 1980s. We used mass spectrometry to measure trace element ratios in coral cores to use as a proxy for sediment in river discharge. Results showed an extremely similar increase between our proxy and the river discharge instrumental record, demonstrating the use of these corals as reliable archives.
Thibauld M. Béjard, Andrés S. Rigual-Hernández, José A. Flores, Javier P. Tarruella, Xavier Durrieu de Madron, Isabel Cacho, Neghar Haghipour, Aidan Hunter, and Francisco J. Sierro
Biogeosciences, 20, 1505–1528, https://doi.org/10.5194/bg-20-1505-2023, https://doi.org/10.5194/bg-20-1505-2023, 2023
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The Mediterranean Sea is undergoing a rapid and unprecedented environmental change. Planktic foraminifera calcification is affected on different timescales. On seasonal and interannual scales, calcification trends differ according to the species and are linked mainly to sea surface temperatures and carbonate system parameters, while comparison with pre/post-industrial assemblages shows that all three species have reduced their calcification between 10 % to 35 % according to the species.
Pauline Cornuault, Thomas Westerhold, Heiko Pälike, Torsten Bickert, Karl-Heinz Baumann, and Michal Kucera
Biogeosciences, 20, 597–618, https://doi.org/10.5194/bg-20-597-2023, https://doi.org/10.5194/bg-20-597-2023, 2023
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We generated high-resolution records of carbonate accumulation rate from the Miocene to the Quaternary in the tropical Atlantic Ocean to characterize the variability in pelagic carbonate production during warm climates. It follows orbital cycles, responding to local changes in tropical conditions, as well as to long-term shifts in climate and ocean chemistry. These changes were sufficiently large to play a role in the carbon cycle and global climate evolution.
José Guitián, Miguel Ángel Fuertes, José-Abel Flores, Iván Hernández-Almeida, and Heather Stoll
Biogeosciences, 19, 5007–5019, https://doi.org/10.5194/bg-19-5007-2022, https://doi.org/10.5194/bg-19-5007-2022, 2022
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The effect of environmental conditions on the degree of calcification of marine phytoplankton remains unclear. This study implements a new microscopic approach to quantify the calcification of ancient coccolithophores, using North Atlantic sediments. Results show significant differences in the thickness and shape factor of coccoliths for samples with minimum dissolution, providing the first evaluation of phytoplankton physiology adaptation to million-year-scale variable environmental conditions.
Jeremy N. Bentley, Gregory T. Ventura, Clifford C. Walters, Stefan M. Sievert, and Jeffrey S. Seewald
Biogeosciences, 19, 4459–4477, https://doi.org/10.5194/bg-19-4459-2022, https://doi.org/10.5194/bg-19-4459-2022, 2022
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We demonstrate the TEX86 (TetraEther indeX of 86 carbon atoms) paleoclimate proxy can become heavily impacted by the ocean floor archaeal community. The impact results from source inputs, their diagenetic and catagenetic alteration, and further overprint by the additions of lipids from the ocean floor sedimentary archaeal community. We then present a method to correct the overprints by using IPLs (intact polar lipids) extracted from both water column and subsurface archaeal communities.
Bryan C. Lougheed and Brett Metcalfe
Biogeosciences, 19, 1195–1209, https://doi.org/10.5194/bg-19-1195-2022, https://doi.org/10.5194/bg-19-1195-2022, 2022
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Measurements on sea-dwelling shelled organisms called foraminifera retrieved from deep-sea sediment cores have been used to reconstruct sea surface temperature (SST) variation. To evaluate the method, we use a computer model to simulate millions of single foraminifera and how they become mixed in the sediment after being deposited on the seafloor. We compare the SST inferred from the single foraminifera in the sediment core to the true SST in the water, thus quantifying method uncertainties.
Thore Friesenhagen
Biogeosciences, 19, 777–805, https://doi.org/10.5194/bg-19-777-2022, https://doi.org/10.5194/bg-19-777-2022, 2022
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Size measurements of the planktonic foraminifer Globorotalia menardii and related forms are used to investigate the shell-size evolution for the last 8 million years in the eastern tropical Atlantic Ocean. Long-term changes in the shell size coincide with major climatic, palaeogeographic and palaeoceanographic changes and suggest the occurrence of a new G. menardii type in the Atlantic Ocean ca. 2 million years ago.
Nele Manon Vollmar, Karl-Heinz Baumann, Mariem Saavedra-Pellitero, and Iván Hernández-Almeida
Biogeosciences, 19, 585–612, https://doi.org/10.5194/bg-19-585-2022, https://doi.org/10.5194/bg-19-585-2022, 2022
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We studied recent (sub-)fossil remains of a type of algae (coccolithophores) off southernmost Chile and across the Drake Passage, adding to the scarce knowledge that exists in the Southern Ocean, a rapidly changing environment. We found that those can be used to reconstruct the surface ocean conditions in the north but not in the south. We also found variations in shape in the dominant species Emiliania huxleyi depending on the location, indicating subtle adaptations to environmental conditions.
Catherine V. Davis, Karen Wishner, Willem Renema, and Pincelli M. Hull
Biogeosciences, 18, 977–992, https://doi.org/10.5194/bg-18-977-2021, https://doi.org/10.5194/bg-18-977-2021, 2021
Práxedes Muñoz, Lorena Rebolledo, Laurent Dezileau, Antonio Maldonado, Christoph Mayr, Paola Cárdenas, Carina B. Lange, Katherine Lalangui, Gloria Sanchez, Marco Salamanca, Karen Araya, Ignacio Jara, Gabriel Easton, and Marcel Ramos
Biogeosciences, 17, 5763–5785, https://doi.org/10.5194/bg-17-5763-2020, https://doi.org/10.5194/bg-17-5763-2020, 2020
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We analyze marine sedimentary records to study temporal changes in oxygen and productivity in marine waters of central Chile. We observed increasing oxygenation and decreasing productivity from 6000 kyr ago to the modern era that seem to respond to El Niño–Southern Oscillation activity. In the past centuries, deoxygenation and higher productivity are re-established, mainly in the northern zones of Chile and Peru. Meanwhile, in north-central Chile the deoxygenation trend is maintained.
Luka Šupraha and Jorijntje Henderiks
Biogeosciences, 17, 2955–2969, https://doi.org/10.5194/bg-17-2955-2020, https://doi.org/10.5194/bg-17-2955-2020, 2020
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The cell size, degree of calcification and growth rates of coccolithophores impact their role in the carbon cycle and may also influence their adaptation to environmental change. Combining insights from culture experiments and the fossil record, we show that the selection for smaller cells over the past 15 Myr has been a common adaptive trait among different lineages. However, heavily calcified species maintained a more stable biogeochemical output than the ancestral lineage of E. huxleyi.
Niels J. de Winter, Clemens V. Ullmann, Anne M. Sørensen, Nicolas Thibault, Steven Goderis, Stijn J. M. Van Malderen, Christophe Snoeck, Stijn Goolaerts, Frank Vanhaecke, and Philippe Claeys
Biogeosciences, 17, 2897–2922, https://doi.org/10.5194/bg-17-2897-2020, https://doi.org/10.5194/bg-17-2897-2020, 2020
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In this study, we present a detailed investigation of the chemical composition of 12 specimens of very well preserved, 78-million-year-old oyster shells from southern Sweden. The chemical data show how the oysters grew, the environment in which they lived and how old they became and also provide valuable information about which chemical measurements we can use to learn more about ancient climate and environment from such shells. In turn, this can help improve climate reconstructions and models.
Hannah M. Palmer, Tessa M. Hill, Peter D. Roopnarine, Sarah E. Myhre, Katherine R. Reyes, and Jonas T. Donnenfield
Biogeosciences, 17, 2923–2937, https://doi.org/10.5194/bg-17-2923-2020, https://doi.org/10.5194/bg-17-2923-2020, 2020
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Modern climate change is causing expansions of low-oxygen zones, with detrimental impacts to marine life. To better predict future ocean oxygen change, we study past expansions and contractions of low-oxygen zones using microfossils of seafloor organisms. We find that, along the San Diego margin, the low-oxygen zone expanded into more shallow water in the last 400 years, but the conditions within and below the low-oxygen zone did not change significantly in the last 1500 years.
Yuanyuan Hong, Moriaki Yasuhara, Hokuto Iwatani, and Briony Mamo
Biogeosciences, 16, 585–604, https://doi.org/10.5194/bg-16-585-2019, https://doi.org/10.5194/bg-16-585-2019, 2019
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This study analyzed microfaunal assemblages in surface sediments from 52 sites in Hong Kong marine waters. We selected 18 species for linear regression modeling to statistically reveal the relationship between species distribution and environmental factors. These results show environmental preferences of commonly distributed species on Asian coasts, providing a robust baseline for past environmental reconstruction of the broad Asian region using microfossils in sediment cores.
Jorge Domingo Carrillo-Briceño, Zoneibe Luz, Austin Hendy, László Kocsis, Orangel Aguilera, and Torsten Vennemann
Biogeosciences, 16, 33–56, https://doi.org/10.5194/bg-16-33-2019, https://doi.org/10.5194/bg-16-33-2019, 2019
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By combining taxonomy and geochemistry, we corroborated the described paleoenvironments from a Neogene fossiliferous deposit of South America. Shark teeth specimens were used for taxonomic identification and as proxies for geochemical analyses. With a multidisciplinary approach we refined the understanding about the paleoenvironmental setting and the paleoecological characteristics of the studied groups, in our case, for the bull shark and its incursions into brackish waters.
Anna Binczewska, Bjørg Risebrobakken, Irina Polovodova Asteman, Matthias Moros, Amandine Tisserand, Eystein Jansen, and Andrzej Witkowski
Biogeosciences, 15, 5909–5928, https://doi.org/10.5194/bg-15-5909-2018, https://doi.org/10.5194/bg-15-5909-2018, 2018
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Primary productivity is an important factor in the functioning and structuring of the coastal ecosystem. Thus, two sediment cores from the Skagerrak (North Sea) were investigated in order to obtain a comprehensive picture of primary productivity changes during the last millennium and identify associated forcing factors (e.g. anthropogenic, climate). The cores were dated and analysed for palaeoproductivity proxies and palaeothermometers.
Sami A. Jokinen, Joonas J. Virtasalo, Tom Jilbert, Jérôme Kaiser, Olaf Dellwig, Helge W. Arz, Jari Hänninen, Laura Arppe, Miia Collander, and Timo Saarinen
Biogeosciences, 15, 3975–4001, https://doi.org/10.5194/bg-15-3975-2018, https://doi.org/10.5194/bg-15-3975-2018, 2018
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Oxygen deficiency is a major environmental problem deteriorating seafloor habitats especially in the coastal ocean with large human impact. Here we apply a wide set of chemical and physical analyses to a 1500-year long sediment record and show that, although long-term climate variability has modulated seafloor oxygenation in the coastal northern Baltic Sea, the oxygen loss over the 20th century is unprecedentedly severe, emphasizing the need to reduce anthropogenic nutrient input in the future.
Saúl González-Lemos, José Guitián, Miguel-Ángel Fuertes, José-Abel Flores, and Heather M. Stoll
Biogeosciences, 15, 1079–1091, https://doi.org/10.5194/bg-15-1079-2018, https://doi.org/10.5194/bg-15-1079-2018, 2018
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Changes in atmospheric carbon dioxide affect ocean chemistry and the ability of marine organisms to manufacture shells from calcium carbonate. We describe a technique to obtain more reproducible measurements of the thickness of calcium carbonate shells made by microscopic marine algae called coccolithophores, which will allow researchers to compare how the shell thickness responds to variations in ocean chemistry in the past and present.
Ulrich Kotthoff, Jeroen Groeneveld, Jeanine L. Ash, Anne-Sophie Fanget, Nadine Quintana Krupinski, Odile Peyron, Anna Stepanova, Jonathan Warnock, Niels A. G. M. Van Helmond, Benjamin H. Passey, Ole Rønø Clausen, Ole Bennike, Elinor Andrén, Wojciech Granoszewski, Thomas Andrén, Helena L. Filipsson, Marit-Solveig Seidenkrantz, Caroline P. Slomp, and Thorsten Bauersachs
Biogeosciences, 14, 5607–5632, https://doi.org/10.5194/bg-14-5607-2017, https://doi.org/10.5194/bg-14-5607-2017, 2017
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We present reconstructions of paleotemperature, paleosalinity, and paleoecology from the Little Belt (Site M0059) over the past ~ 8000 years and evaluate the applicability of numerous proxies. Conditions were lacustrine until ~ 7400 cal yr BP. A transition to brackish–marine conditions then occurred within ~ 200 years. Salinity proxies rarely allowed quantitative estimates but revealed congruent results, while quantitative temperature reconstructions differed depending on the proxies used.
Shuichang Zhang, Xiaomei Wang, Huajian Wang, Emma U. Hammarlund, Jin Su, Yu Wang, and Donald E. Canfield
Biogeosciences, 14, 2133–2149, https://doi.org/10.5194/bg-14-2133-2017, https://doi.org/10.5194/bg-14-2133-2017, 2017
Liza M. Roger, Annette D. George, Jeremy Shaw, Robert D. Hart, Malcolm Roberts, Thomas Becker, Bradley J. McDonald, and Noreen J. Evans
Biogeosciences, 14, 1721–1737, https://doi.org/10.5194/bg-14-1721-2017, https://doi.org/10.5194/bg-14-1721-2017, 2017
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The shell compositions of bivalve species from south Western Australia are described here to better understand the factors involved in their formation. The shell composition can be used to reconstruct past environmental conditions, but certain species manifest an offset compared to the environmental parameters measured. As shown here, shells that experience the same conditions can present different compositions in relation to structure, organic composition and environmental conditions.
Johan Vellekoop, Lineke Woelders, Sanem Açikalin, Jan Smit, Bas van de Schootbrugge, Ismail Ö. Yilmaz, Henk Brinkhuis, and Robert P. Speijer
Biogeosciences, 14, 885–900, https://doi.org/10.5194/bg-14-885-2017, https://doi.org/10.5194/bg-14-885-2017, 2017
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The Cretaceous–Paleogene boundary, ~ 66 Ma, is characterized by a mass extinction. We studied groups of both surface-dwelling and bottom-dwelling organisms to unravel the oceanographic consequences of these extinctions. Our integrated records indicate that a reduction of the transport of organic matter to the sea floor resulted in enhanced recycling of nutrients in the upper water column and decreased food supply at the sea floor in the first tens of thousands of years after the extinctions.
Johan Renaudie
Biogeosciences, 13, 6003–6014, https://doi.org/10.5194/bg-13-6003-2016, https://doi.org/10.5194/bg-13-6003-2016, 2016
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Marine planktonic diatoms are today both the main silica and carbon exporter to the deep sea. However, 50 million years ago, radiolarians were the main silica exporter and diatoms were a rare, geographically restricted group. Quantification of their rise to dominance suggest that diatom abundance is primarily controlled by the continental weathering and has a negative feedback, observable on a geological timescale, on the carbon cycle.
Jelena Vidović, Rafał Nawrot, Ivo Gallmetzer, Alexandra Haselmair, Adam Tomašových, Michael Stachowitsch, Vlasta Ćosović, and Martin Zuschin
Biogeosciences, 13, 5965–5981, https://doi.org/10.5194/bg-13-5965-2016, https://doi.org/10.5194/bg-13-5965-2016, 2016
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We studied the ecological history of the Gulf of Trieste. Before the 20th century, the only activity here was ore mining, releasing high amounts of mercury into its northern part, Panzano Bay. Mercury did not cause changes to microorganisms, as it is not bioavailable. In the 20th century, agriculture caused nutrient enrichment in the bay and increased diversity of microorganisms. Industrial activities increased the concentrations of pollutants, causing only minor changes to microorganisms.
Aurélie Penaud, Frédérique Eynaud, Antje Helga Luise Voelker, and Jean-Louis Turon
Biogeosciences, 13, 5357–5377, https://doi.org/10.5194/bg-13-5357-2016, https://doi.org/10.5194/bg-13-5357-2016, 2016
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This paper presents new analyses conducted at high resolution in the Gulf of Cadiz over the last 50 ky. Palaeohydrological changes in these subtropical latitudes are discussed through dinoflagellate cyst assemblages but also dinocyst transfer function results, implying sea surface temperature and salinity as well as annual productivity reconstructions. This study is thus important for our understanding of past and future productivity regimes, also implying consequences on the biological pump.
William Hardy, Aurélie Penaud, Fabienne Marret, Germain Bayon, Tania Marsset, and Laurence Droz
Biogeosciences, 13, 4823–4841, https://doi.org/10.5194/bg-13-4823-2016, https://doi.org/10.5194/bg-13-4823-2016, 2016
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Our approach is based on a multi-proxy study from a core collected off the Congo River and discusses surface oceanic conditions (upwelling cells, river-induced upwelling), land–sea interactions and terrestrial erosion and in particular enables us to spatially constrain the migration of atmospheric systems. This paper thus presents new data highlighting, with the highest resolution ever reached in this region, the great correlation between phytoplanktonic organisms and monsoonal mechanisms.
Philippine Campagne, Xavier Crosta, Sabine Schmidt, Marie Noëlle Houssais, Olivier Ther, and Guillaume Massé
Biogeosciences, 13, 4205–4218, https://doi.org/10.5194/bg-13-4205-2016, https://doi.org/10.5194/bg-13-4205-2016, 2016
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Diatoms and biomarkers have been recently used for palaeoclimate reconstructions in the Southern Ocean. Few sediment-based ecological studies have investigated their relationships with environmental conditions. Here, we compare high-resolution sedimentary records with meteorological data to study relationships between our proxies and recent atmospheric and sea surface changes. Our results indicate that coupled wind pattern and sea surface variability act as the proximal forcing at that scale.
Niels A. G. M. van Helmond, Appy Sluijs, Nina M. Papadomanolaki, A. Guy Plint, Darren R. Gröcke, Martin A. Pearce, James S. Eldrett, João Trabucho-Alexandre, Ireneusz Walaszczyk, Bas van de Schootbrugge, and Henk Brinkhuis
Biogeosciences, 13, 2859–2872, https://doi.org/10.5194/bg-13-2859-2016, https://doi.org/10.5194/bg-13-2859-2016, 2016
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Over the past decades large changes have been observed in the biogeographical dispersion of marine life resulting from climate change. To better understand present and future trends it is important to document and fully understand the biogeographical response of marine life during episodes of environmental change in the geological past.
Here we investigate the response of phytoplankton, the base of the marine food web, to a rapid cold spell, interrupting greenhouse conditions during the Cretaceous.
Thomas C. Brachert, Markus Reuter, Stefan Krüger, Julia Kirkerowicz, and James S. Klaus
Biogeosciences, 13, 1469–1489, https://doi.org/10.5194/bg-13-1469-2016, https://doi.org/10.5194/bg-13-1469-2016, 2016
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We present stable isotope proxy data and calcification records from fossil reef corals. The corals investigated derive from the Florida carbonate platform and are of middle Pliocene to early Pleistocene age. From the data we infer an environment subject to intermittent upwelling on annual to decadal timescales. Calcification rates were enhanced during periods of upwelling. This is likely an effect of dampened SSTs during the upwelling.
B. A. A. Hoogakker, D. J. R. Thornalley, and S. Barker
Biogeosciences, 13, 211–221, https://doi.org/10.5194/bg-13-211-2016, https://doi.org/10.5194/bg-13-211-2016, 2016
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Models predict a decrease in future ocean O2, driven by surface water warming and freshening in the polar regions, causing a reduction in ocean circulation. Here we assess this effect in the past, focussing on the response of deep and intermediate waters from the North Atlantic during large-scale ice rafting and millennial-scale cooling events of the last glacial.
Our assessment agrees with the models but also highlights the importance of biological processes driving ocean O2 change.
M. Hermoso, I. Z. X. Chan, H. L. O. McClelland, A. M. C. Heureux, and R. E. M. Rickaby
Biogeosciences, 13, 301–312, https://doi.org/10.5194/bg-13-301-2016, https://doi.org/10.5194/bg-13-301-2016, 2016
B. Metcalfe, W. Feldmeijer, M. de Vringer-Picon, G.-J. A. Brummer, F. J. C. Peeters, and G. M. Ganssen
Biogeosciences, 12, 4781–4807, https://doi.org/10.5194/bg-12-4781-2015, https://doi.org/10.5194/bg-12-4781-2015, 2015
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Iron biogeochemical budgets during the natural ocean fertilisation experiment KEOPS-2 showed that complex circulation and transport pathways were responsible for differences in the mode and strength of iron supply, with vertical supply dominant on the plateau and lateral supply dominant in the plume. The exchange of iron between dissolved, biogenic and lithogenic pools was highly dynamic, resulting in a decoupling of iron supply and carbon export and controlling the efficiency of fertilisation.
J. P. D'Olivo, M. T. McCulloch, S. M. Eggins, and J. Trotter
Biogeosciences, 12, 1223–1236, https://doi.org/10.5194/bg-12-1223-2015, https://doi.org/10.5194/bg-12-1223-2015, 2015
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The boron isotope composition in the skeleton of massive Porites corals from the central Great Barrier Reef is used to reconstruct the seawater pH over the 1940-2009 period. The long-term decline in the coral-reconstructed seawater pH is in close agreement with estimates based on the CO2 uptake by surface waters due to rising atmospheric levels. We also observed a significant relationship between terrestrial runoff data and the inshore coral boron isotopes records.
J. Schönfeld, W. Kuhnt, Z. Erdem, S. Flögel, N. Glock, M. Aquit, M. Frank, and A. Holbourn
Biogeosciences, 12, 1169–1189, https://doi.org/10.5194/bg-12-1169-2015, https://doi.org/10.5194/bg-12-1169-2015, 2015
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Today’s oceans show distinct mid-depth oxygen minima while whole oceanic basins became transiently anoxic in the Mesozoic. To constrain past bottom-water oxygenation, we compared sediments from the Peruvian OMZ with the Cenomanian OAE 2 from Morocco. Corg accumulation rates in laminated OAE 2 sections match Holocene rates off Peru. Laminated deposits are found at oxygen levels of < 7µmol kg-1; crab burrows appear at 10µmol kg-1 today, both defining threshold values for palaeoreconstructions.
S. C. Löhr and M. J. Kennedy
Biogeosciences, 11, 4971–4983, https://doi.org/10.5194/bg-11-4971-2014, https://doi.org/10.5194/bg-11-4971-2014, 2014
R. Hoffmann, J. A. Schultz, R. Schellhorn, E. Rybacki, H. Keupp, S. R. Gerden, R. Lemanis, and S. Zachow
Biogeosciences, 11, 2721–2739, https://doi.org/10.5194/bg-11-2721-2014, https://doi.org/10.5194/bg-11-2721-2014, 2014
T. J. Algeo, P. A. Meyers, R. S. Robinson, H. Rowe, and G. Q. Jiang
Biogeosciences, 11, 1273–1295, https://doi.org/10.5194/bg-11-1273-2014, https://doi.org/10.5194/bg-11-1273-2014, 2014
C. Berger, K. J. S. Meier, H. Kinkel, and K.-H. Baumann
Biogeosciences, 11, 929–944, https://doi.org/10.5194/bg-11-929-2014, https://doi.org/10.5194/bg-11-929-2014, 2014
T. Caley, S. Zaragosi, J. Bourget, P. Martinez, B. Malaizé, F. Eynaud, L. Rossignol, T. Garlan, and N. Ellouz-Zimmermann
Biogeosciences, 10, 7347–7359, https://doi.org/10.5194/bg-10-7347-2013, https://doi.org/10.5194/bg-10-7347-2013, 2013
N. Preto, C. Agnini, M. Rigo, M. Sprovieri, and H. Westphal
Biogeosciences, 10, 6053–6068, https://doi.org/10.5194/bg-10-6053-2013, https://doi.org/10.5194/bg-10-6053-2013, 2013
I. Polovodova Asteman, K. Nordberg, and H. L. Filipsson
Biogeosciences, 10, 1275–1290, https://doi.org/10.5194/bg-10-1275-2013, https://doi.org/10.5194/bg-10-1275-2013, 2013
J.-E. Tesdal, E. D. Galbraith, and M. Kienast
Biogeosciences, 10, 101–118, https://doi.org/10.5194/bg-10-101-2013, https://doi.org/10.5194/bg-10-101-2013, 2013
L. Durantou, A. Rochon, D. Ledu, G. Massé, S. Schmidt, and M. Babin
Biogeosciences, 9, 5391–5406, https://doi.org/10.5194/bg-9-5391-2012, https://doi.org/10.5194/bg-9-5391-2012, 2012
Cited articles
Achlatis, M., Van der Zande R. M., Schönberg, C. H. L., Fang, J. K. H., Hoegh-Guldberg, O., and Sophie Dove, S.: Sponge bioerosion on changing reefs: ocean warming poses physiological constraints to the success of a photosymbiotic excavating sponge, Sci. Rep., 7, 10705, https://doi.org/10.1038/s41598-017-10947-1, 2017.
Aguirre, J., Perfectti, F., and Braga, J. C.: Integrating phylogeny, molecular clocks, and the fossil record in the evolution of coralline algae (Corallinales and Sporolithales, Rhodophyta), Paleobiology, 34, 519–533, 2010.
Altermann, W., Böhmer, C., Gitter, F., Heimann, F., Heller, I., Läuchli, B., and Putz, C.: “Defining biominerals and organominerals: direct and indirect indicators of life, Perry et al., Sediment. Geol., 201, 157–179”, Sediment. Geol., Response, 213, 150–151, 2009.
Anbu, P., Kang, C. H., Shin, Y. J., and So, J. S.: Formations of calcium carbonate minerals by bacteria and its multiple applications, Springer Plus, 5, 250, https://doi.org/10.1186/s40064-016-1869-2, 2016.
Ballesteros, E.: Mediterranean Coralligenous Assemblages, in Oceanography and Marine Biology, Ann. Rev., 44, 123–195, 2006.
Basso, D., Nalin, R., and Massari, F.: Genesis and composition of the Pleistocene Coralligene de plateau of the Cutro Terrace (Calabria, southern Italy), Jb. Geol. Paläont. Abh., 244, 173–182, 2007.
Basso, D., Nalin, R., and Nelson, C. S.: Shallow-water Sporolithon Rhodoliths from North Island (New Zealand), Palaios, 24, 92–103, 2009.
Basso, D., Bracchi, V. A., Bazzicalupo, P., Martini, M., Maspero, F., and Bavestrello, G.: Living coralligenous as geo-historical structure built by coralline algae, Front. Earth Sci., 10, 961632, https://doi.org/10.3389/feart.2022.961632, 2022.
Bazylinski, D. A. and Frankel, R. B.: Magnetosome formation in prokaryotes, Nat. Rev. Microbiol., 2, 217–230, 2004.
Blakemore, R.: Magnetotactic Bacteria, Science, 190, 377–379, 1975.
Bellan-Santini, D., Lacaze, J. C., and Poizat, C.: Les biocénoses marines et littorales de Méditerranée, Synthèse, menaces et perspectives, Muséum National d'Histoire Naturelle, Sécretariat de la Flore et de la Faune, Paris, 246 pp., 1994.
Belmonte, G., Ingrosso, G., Poto, M., Quarta, G., D'elia, M., Onorato, O. and Calcagnile, L.: Biogenic stalactites in submarine caves at the Cape of Otranto (SE Italy): dating and hypothesis on their formation, Mar. Ecol., 30, 376–382, 2009.
Belmonte, G., Guido, A., Mastandrea, A., Onorato, R., Rosso, A., and Sanfilippo, R.: Animal Forests in Submarine Caves, in: Perspectives on the Marine Animal Forests of the World, edited by: Rossi, S. and Bramanti, L., 129–145, Springer Nature Switzerland AG, 2020.
Benzerara, K., Miot, J., Morin, G., Ona-Nguema, G., Skouri-Panet, F., and Ferard, C.: Significance, mechanisms and environmental implications of microbial biomineralization, Cr. Geosci., 343, 160–167, 2011.
Bertolino, M., Calcinai, B., Cattaneo-Vietti, R., Cerrano, C., Lafratta, A., Pansini, M., Pica, D., and Bavestrello, G.: Stability of the sponge assemblage of Mediterranean coralligenous concretions along a millennial time span, Mar. Ecol., 35, 149–158, 2013.
Bertolino, M., Calcinai, B., Cattaneo-Vietti, R., Cerrano, C., Lafratta, A., Pansini, M., Pica, D., and Bavestrello, G.: Stability of the sponge assemblage of Mediterranean coralligenous concretions along a millennial time span, Ecology, 35, https://doi.org/10.1111/maec.12063, 2014.
Bertolino, M., Costa, G., Carella, M., Cattaneo-Vietti, R., Cerrano, C., Pansini, M., Quarta, G., Calcagnile, L., and Bavestrello, G.: The dynamics of a Mediterranean coralligenous sponge assemblage at decennial and millennial temporal scales, PLoS ONE, 12, e0177945, https://doi.org/10.1371/journal.pone.0177945, 2017a.
Bertolino, M., Cattaneo-Vietti, R., Costa, G., Pansini, M., Fraschetti, S., and Bavestrello, G.: Have Climate Changes Driven the Diversity of a Mediterranean Coralligenous Sponge Assemblage on a Millennial Time scale?, Palaeogeogr. Palaeocl., 487, 355–363, 2017b.
Bertolino, M., Costa, G., Cattaneo-Vietti, R., Pansini, M., Quarta, G., Calcagnile, L., and Bavestrello, G.: Ancient and recent sponge assemblages from the Tyrrhenian coralligenous over millennia (Mediterranean Sea), Facies, 65, 1–12, 2019.
Borch, T., Kretzschmar, R., Kappler, A., Van Cappellen, P., Ginder-Vogel, M., Voegelin, A., and Campbell, K.: Biogeochemical redox processes and their impact on contaminant dynamics, Environ. Sci. Technol., 44, 15–23, 2010.
Bosence, D. W. J. and Pedley, H. M.: Sedimentology and Palaeoecology of a Miocene Coralline Algal Biostrome from the Maltese Islands, Palaeogeogr. Palaeocl., 38, 9–43, 1982.
Bracchi, V. A., Nalin, R., and Basso, D.: Paleoecology and Dynamics of Coralline Dominated Facies during a Pleistocene Transgressive-Regressive Cycle (Capo Colonna Marine Terrace, Southern Italy), Palaeogeogr. Palaeocl., 414, 296–309, 2014.
Bracchi, V., Savini, A., Marchese, F., Palamara, S., Basso, D., and Corselli, C.: Coralligenous Habitat in the Mediterranean Sea: a Geomorphological Description from Remote Data, Ital. J. Geosci., 134, 32–40, 2015.
Bracchi, V. A., Nalin, R., and Basso, D.: Morpho-structural Heterogeneity of Shallow-Water Coralligenous in a Pleistocene Marine Terrace (Le Castella, Italy), Palaeogeogr. Palaeocl., 454, 101–112, 2016.
Bracchi, V. A., Basso, D., Marchese, F., Corselli C., and Savini A.: Coralligenous morphotypes on subhorizontal substrate: A new categorization, Cont. Shelf Res., 144, 10–20, 2017.
Bracchi, V. A., Basso, D., Savini, A. E., and Corselli, C.: Algal Reefs (Coralligenous) from Glacial Stages: Origin and Nature of a Submerged Tabular Relief (Hyblean Plateau, Italy), Mar. Geol., 411, 119–132, 2019.
Bracchi V. A., Bazzicalupo P., Fallati L., Varzi A. G., Savini A., Negri M. P., Rosso A., Sanfilippo R., Guido A., Bertolino M., Costa, G., De Ponti, E., Leonardi, R., Muzzupappa, M., and Basso, D.: The main builders of Mediterranean coralligenous: 2D and 3D quantitative approaches for its identification, Front. Earth Sci., 10, 910522, https://doi.org/10.3389/feart.2022.910522, 2022.
Braga, J. C., Martìn, J. M., and Riding, R.: Controls on microbial dome development along a carbonate-siliciclastic shelf-basin transect, Miocene, S.E. Spain, Palaios, 10, 347–361, 1995.
Bressan, G., Babbini, L., Ghirardelli, L., and Basso, D.: Bio-costruzione e bio-distruzione di corallinales nel mar mediterraneo, Biol. Mar. Mediterr., 8, 131–174, 2001.
Buczynski, C. and Chafetz, H. S.: Habit of bacterially induced precipitates of calcium carbonate and the influence of medium viscosity on mineralogy, J. Sediment. Petrol., 61, 226–233, 1991.
Calcinai, B., Bavestrello, G., Cuttone, G., and Cerrano, C.: Excavating sponges from the Adriatic Sea: description of Cliona adriatica sp. nov. (Demospongiae: Clionaidae) and estimation of its boring activity, J. Mar. Biol. Assoc. UK, 91, 339–346, 2011.
Calcinai, B., Bertolino, M., Bavestrello, G., Montori, S., Mori, M., Pica, D., Valisano, L., and Cerrano, C.: Comparison between the sponge fauna living outside and inside the coralligenous bioconstruction: a quantitative approach, Mediterr. Mar. Sci., 16, 413–418, 2015.
Calcinai, B., Sacco Perasso, C., Davide Petriaggi, B., and Ricci, S.: Endolithic and epilithic sponges of archaeological marble statues recovered in the Blue Grotto, Capri (Italy) and in the Antikythera shipwreck (Greece), Facies, 65, 21, https://doi.org/10.1007/s10347-019-0562-7, 2019.
Carannante, G. and Simone, L.: Rhodolith Facies in the Central-southern Apennines Mountains, Italy, in: Models for Carbonate Stratigraphy from Miocene Reef Complexes of Mediterranean Regions, Italy, edited by: Franseen, E. K., Esteban, M., Ward, W. C., and Rouchy, J. M., 261–275, SEPM Concepts Sedimentol. Paleontol., 1996.
Cerrano, C., Bastari, A., Calcinai, B., Di Camillo, C., Pica, D., Puce, S., Valisano, L., and Torsani, F.: Temperate mesophotic ecosystems: gaps and perspectives of an emerging conservation challenge for the Mediterranean Sea, The Eur. Zool. J., 8, 370–388, 2019.
Cerrano, C., Bavestrello, G., Bianchi, C. N., Calcinai, B., Cattaneo-Vietti, R., Morri, C., and Sarà, M.: The Role of Sponge Bioerosion in Mediterranean Coralligenous Accretion, in: Mediterranean Ecosystems: Structures and Processes, edited by: Faranda, F. M., Guglielmo, L., and Spezie, G., 235–240, Springer Milan, 2001.
Chafetz, H. S.: Marine peloids: a product of bacterially induced precipitation of calcite, J. Sediment. Petrol., 56, 812–817, 1986.
Cipriani, M., Basso, D., Bazzicalupo, P., Bertolino, M., Bracchi, V. A., Bruno, F., Costa, G., Dominici, R., Gallo, A., Muzzupappa, M., Rosso, A., Sanfilippo, R., Sciuto, F., and Guido, A.: The role of non-skeletal carbonate component in Mediterranean Coralligenous: new insight from the CRESCIBLUREEF project, Rend, Online Soc. Geol. It., 59, 75–79, 2023.
Corriero, G., Scalera Liaci, L., Ruggiero, D., and Pansini, M.: The sponge community of a semi-submerged Mediterranean cave, Mar. Ecol., 21, 85–96, 2000.
Costa, G., Bavestrello, G., Micaroni, V., Pansini, M., Strano, F., and Bertolino, M.: Sponge Community Variation along the Apulian Coasts (Otranto Strait) over a Pluri-Decennial Time Span. Does Water Warming Drive a Sponge Diversity Increasing in the Mediterranean Sea?, J. Mar. Biol. Ass., 99, 1519–1534, 2019.
Deias, C., Guido, A., Sanfilippo, R., Apollaro, C., Dominici, R., Cipriani, M., Barca, D., and Vespasiano, G.: Elemental Fractionation in Sabellariidae (Polychaeta) Biocement and Comparison with Seawater Pattern: A New Environmental Proxy in a High-Biodiversity Ecosystem?, Water, 15, 1549, https://doi.org/10.3390/w15081549, 2023.
Delecat, S. and Reitner, J.: Sponge communities from the Lower Liassic of Adnet (Northern Calcareous Alps, Austria), Facies, 51, 385–404, 2005.
Delecat, S., Peckman, J., and Reitner, J.: Non-rigid cryptic sponges in oyster patch reefs (Lower Kimmeridgian, Langenberg/Oker, Germany), Facies, 45, 231–254, 2001.
Di Geronimo, I., Di Geronimo, R., Improta, S., Rosso, A., andSanfilippo, R.: Preliminary Observations on a Columnar Coralline Build-Up from off SE Sicily, Biol. Mar. Mediterr., 8, 1–10, 2001.
Di Geronimo, I., Di Geronimo, R., Rosso, A., and Sanfilippo, R.: Structural and Taphonomic Analysis of a Columnar Coralline Algal Build-Up from SE Sicily, Geobios, 35, 86–95, 2002.
Donato, G., Sanfilippo, R., Sciuto, F., D’Alpa, F., Serio, D., Bracchi,V. A., Bazzicalupo, P., Negri, P., Guido, A., Bertolino, M., Costa, G., and Basso, D.: Biodiversity of a Coralligenous Build-up off Marzamemi (SE Sicily, Ionian Sea), in UNEP SPA/RAC, Proceedings of the 4th Mediterranean Symposium on the Conservation of the Coralligenous and Other Calcareous Bio-Concretions, Genova, Italy, 151–152, 2022.
Dupraz, C. and Strasser, A.: Microbialites and micro-encrusters in shallow coral bioherms (Middle-Late Oxfordian, Swiss Jura Mountains), Facies, 40,101–130, 1999.
Dupraz, C., Reid, P. R., Braissant, O., Decho, A. W., Norman, R. S., and Visscher, P. T.: Processes of carbonate precipitation in modern microbial mats, Earth Sci. Rev., 96, 141–162, 2009.
Evcen, A. and Çinar, M. E.: Bioeroding sponge species (Porifera) in the Aegean Sea (Eastern Mediterranean), J. Black Sea/Medit. Environ., 21, 285–306, 2015.
Fichez, R.: Absence of redox potential discontinuity in dark submarine cave sediments as evidence of oligotrophic conditions, Estuar. Coast. Shelf Sci., 31, 875–881, 1990.
Fichez, R.: Suspended particulate organic matter in a Mediterranean submarine cave, Mar. Biol., 108, 167–174, 1991.
Folk, R. L. and Chafetz, H. S.: Bacterially induced microscale and nanoscale carbonate precipitates, in: Microbial Sediments, edited by: Riding, R. E. and Awramik, S. M., 40–49, Springer-Verlag, Berlin, Germany, 2000.
Garrabou, J. and Ballesteros, E.: Growth of Mesophyllum alternans and Lithophyllum frondosum (Corallinales, Rhodophyta) in the northwestern Mediterranean, Eur. J. Phycol., 35, 1–10, 2000.
Gennaro, P., Piazzi, L., Cecchi, E., Montefalcone, M., Morri, C., and Bianchi, C. N.: Monitoring and assessment of the ecological status of coralligenous habitat, The coralligenous cliff, ISPRA, Manuali e Linee Guida, 191bis, 2020.
Gischler, E., Heindel, K., Birgel, D., Brunner, B., Reitner, J., and Peckmann, J.: Cryptic biostalactites in a submerged karst cave of the Belize Barrier Reef revisited: Pendant bioconstructions cemented by microbial micrite, Palaeogeogr. Palaeocl., 278, 34–51, 2017a.
Gischler, E., Birgel, D., Brunner, B., Eisenhauer, A., Meyer, G., Buhre, S., and Peckmann, J.: A giant underwater stalactite from the Blue Hole, Belize, revisited: a complex history of massive carbonate accretion under changing meteoric and marine conditions, J. Sediment. Res., 87, 1260–1284, 2017b.
Glynn, P. W. and Manzello, D. P.: Bioerosion and coral reef growth: a dynamic balance, in: Coral Reefs in the Anthropocene, edited by: Birkeland, C., 67–97, Dordrecht, Springer, 2015.
Grotzinger, J. P. and Knoll, A. H.: Stromatolites in Precambrian carbonates: evolutionary mileposts or environmental dipsticks?, Annu. Rev. Earth Planet. Sci., 27, 313–358, 1999.
Guido, A., Mastandrea, A., Rosso, A., Sanfilippo, R., and Russo, F.: Micrite precipitation induced by sulphate reducing bacteria in serpulid bioconstructions from submarine caves (Syracuse, Sicily), Rend. Online Soc. Geol. Ital., 21, 933–934, 2012.
Guido, A., Heindel, K., Birgel, D., Rosso, A., Mastandrea, A., Sanfilippo, R., Russo, F., and Peckmann, J.: Pendant bioconstructions cemented by microbial carbonate in submerged marine caves (Holocene, SE Sicily), Palaeogeogr. Palaeocl., 388, 166–180, 2013.
Guido, A., Mastandrea, A., Rosso, A., Sanfilippo, R., Tosti, F., Riding, R., and Russo, F.: Commensal symbiosis between agglutinated polychaetes and sulfate reducing bacteria, Geobiology, 12, 265–275, 2014.
Guido, A., Mastandrea, A., Stefani, M., and Russo, F.: Role of autochthonous versus detrital micrite in depositional geometries of Middle Triassic carbonate platform systems, Geol. Soc. Am. Bull., 128, 989–999, 2016.
Guido, A., Rosso, A., Sanfilippo, R., Russo, F., and Mastandrea, A.: Microbial biomineralization in biotic crusts from a Pleistocene Marine Cave (NW Sicily, Italy), Geomicrobiol J., 34, 864–872, 2017a.
Guido, A., Jimenez, C., Achilleos, K., Rosso, A., Sanfilippo, R., Hadjioannou, L., Petrou, A., Russo, F., and Mastandrea, A.: Cryptic serpulid microbialite bioconstructions in the Kakoskali submarine cave (Cyprus, Eastern Mediterranean), Facies, 63, 21, https://doi.org/10.1007/s10347-017-0502-3, 2017b.
Guido, A., Gerovasileiou, V., Russo, F. Rosso, A., Sanfilippo, R., Voultsiadou, E., and Mastandrea, A.: Composition and biostratinomy of sponge-rich biogenic crusts in submarine caves (Aegean Sea, Eastern Mediterrenean), Palaeogeogr. Palaeocl., 534, 109338, https://doi.org/10.1016/j.palaeo.2019.109338, 2019a.
Guido, A., Gerovasileios, V., Russo, F., Rosso, A., Sanfilippo, R., Voultsiadou, E., and Mastandrea, A.: Dataset of biogenic crusts from submarine caves of the Aegean Sea: An example of sponges vs microbialites competition in cryptic environments, Data in Brief, 27, https://doi.org/10.1016/j.dib.2019.104745, 2019b.
Guido, A., Rosso, A., Sanfilippo, R., Miriello, D., and Belmonte, G.: Skeletal vs microbialite geobiological role in bioconstructions of confined marine environments, Palaeogeogr. Palaeocl., 593, 110920, https://doi.org/10.1016/j.palaeo.2022.110920, 2022.
Harmelin, J. G.: Organisation spatiale des communautés sessiles des grottes sousmarines de Méditerranée, in Rapports et Procés-Verbaux de la Commission International pour l'exploitation de la Mer Méditerranée, Monaco, 5, 149–153, 1985.
Hong, J. S.: Contribution a l'étude des Peuplements d'un Fond de Concrétionnement Corllaigène dans la Région Marsaillaise en Méditerranéee Nord-Occidentale, Bull. Korea Oc. Res. Develop. Inst., 4, 27–51, 1982.
Ingrosso, G., Abbiati, M., Badalamenti, F., Bavestrello, G., Belmonte, G., Cannas, R., Benedetti Cecchi, L., Bertolino, M., Bevilacqua, S., Bianchi, C. N., Bo, M., Boscari, E., Cardone, F., Cattaneo-Vietti, R., Cau, A., Cerrano, C., Chemello, R., Chimienti, G., Congiu, L., Corriero, G., Costantini, F., De Leo, F., Donnarumma, L., Falace, A., Fraschetti, S., Giangrande, A., Gravina, M. F., Guarnieri, G., Mastrototaro, F., Milazzo, M., Morri, C., Musco, L., Pezzolesi, L., Piraino, S., Prada, F., Ponti, M., Rindi, F., Russo, G. F., Sandulli, R., Villamor, A., Zane, L., and Boero, F.: Mediterranean Bioconstructions along the Italian Coast, Adv. Mar. Biol., 79, 61–136, 2018.
Jimenez, C., Achilleos, K., Petrou, A., Hadjioannou, L., Guido, A., Rosso, A., Gerovasileiou, V., Albano, P. G., Di Franco, D., Andreou, V., and Abu Alhaija, R.: A dream within a dream: Kakoskali Cave, a unique marine ecosystem in Cyprus (Levantine Sea), in: Marine Caves of the Eastern Mediterranean Sea, Biodiversity, Threats and Conservation, edited by: Oztürk, B., Turkish Marine Research Foundation (TUDAV), Istanbul, Turkey, Publication, 53, 91–110, 2019.
Kazanidis, G., Guido, A., Rosso, A., Sanfilippo, R., Roberts, J. M., and Gerovasileiou, V.: One on Top of the Other: Exploring the Habitat Cascades Phenomenon in Iconic Biogenic Marine Habitats, Diversity, 14, 290, https://doi.org/10.3390/d14040290, 2022.
Kazmierczak, J., Coleman, M. L., Gruszczynski, M., and Kempe, S.: Cyanobacterial key to the genesis of micritic and peloidal limestones in ancient seas, Acta Palaeontol. Pol., 41, 319–338, 1996.
Kennard, J. M. and James, N. P.: Thrombolites and stromatolites: two distinct types of microbial structures, Palaios, 1, 492–503, 1986.
Komeili, A.: Molecular mechanisms of magnetosome formation, Annu. Rev. Biochem., 76, 351–366, 2007.
La Rivière, M., Michez, N., Delavenne, J., Andres, S., Fréjefond, C., Janson, A.-L., Abadie, A., Amouroux, J.-M., Bellan, G., Bellan-Santini, D., Chevaldonné, P., Cimiterra, N., Derolez, V., Fernez, T., Fourt, M., Frisoni, F., Grillas, P., Harmelin, J. G., Jordana, E., Klesczewski, M., Labrune, C., Mouronval, J. B., Ouisse, V., Palomba, L., Pasqualini, V, Pelaprat, C., Pérez, T., Pergent, G., Pergent-Martini, C., Sartoretto, S., Thibaut, T., Vacelet, J., and Verlaque, M.: Fiches descriptives des biocénoses benthiques de Méditerranée, Paris: UMS PatriNat (OFB-CNRS-MNHN), 660, https://doi.org/10.1016/j.cgh.2020.03.064, 2021.
Laborel, J.: Le concrétionnement algal “Coralligene” et son importance géomorphologique en Méditerranée, Rec. Trav. Stn. Mar. d'Endoume, 37, 37–60, 1961.
Leinfelder, R. and Keupp, H.: Upper Jurassic mud mounds: Allochthonous sedimentation versus autochthonous carbonate production, in: Mud Mounds: A Polygenetic Spectrum of Fine-grained Carbonate, edited by: Reitner, J. and Neuweiler, F., 17–26, Facies, 1995.
Lowenstam, H. A. and Weiner, S.: On biomineralization, in: Biomineralization: Principles and Concepts in Bioinorganic Materials Chemistry, edited by: Mann, S., 216 pp., Oxford University Press, New York, 1989.
Mann, S.: Mineralization in biological systems, Struct. Bonding, 54, 125–174, 1983.
Mann, S.: Biomineralization: principles and concepts in bioinorganic materials chemistry, Oxford University Press, Oxford, 2001.
Marchese, F., Bracchi, V. A., Lisi, G., Basso, D., Corselli, C., and Savini, A.: Assessing Fine-Scale Distribution and Volume of Mediterranean Algal Reefs through Terrain Analysis of Multibeam Bathymetric Data, A Case Study in the Southern Adriatic Continental Shelf, Water, 12, 157, https://doi.org/10.3390/w12010157, 2020.
Marion, A. F.: Esquisse d'une topographie zoologique du Golfe de Marseille, Ann. Mus. Hist. Natur. Marseille, 1, 1–108, 1883.
Marlow, J., Schönberg, C. H. L., Davy, S. K., Haris, A., Jompa, J., and Bell, J. J.: Bioeroding sponge assemblages: the importance of substrate availability and sediment, J. Mar. Biol. Assoc. UK, 99, 343–358, 2018.
Monty, C. L. V.: The origin and development of cryptalgal fabrics, in: Stromatolites, Development in Sedimentology, edited by: Walter, M. R., 198–249, Elsevier, New York, 1976.
Nalin, R., Basso, D., and Massari, F.: Pleistocene coralline algal build-ups (coralligène de plateau) and associated bioclastic deposits in the sedimentary cover of Cutro marine terrace (Calabria, southern Italy), Geol. Soc. Lond. Spec. Publ., 255, 11–22, 2006.
Nava, H. and Carballo, J. L.: Environmental factors shaping boring sponge assemblages at Mexican Pacific coral reefs, Mar. Ecol. Evol. Persp., 34, 269–279, 2013.
Neuweiler, F., Gautret, P., Thiel, V., Lange, R., Michaelis, W., and Reitner, J.: Petrology of Lower Cretaceous carbonate mud mounds (Albian, N. Spain): insights into organomineralic deposits of the geological record, Sedimentology, 46, 837–859, 1999.
Neuweiler, F., Rutsch, M., Geipel, G., Reimer, A., and Heise, K. H.: Soluble humic substances from in situ precipitated microcrystalline calcium carbonate, internal sediment, and spar cement in a Cretaceous carbonate mud-mound, Geology, 28, 851–854, 2000.
Neuweiler, F., D'orazio, V., Immenhauser, A., Geipel, G., Heise, K.-H., Cocozza, C., and Miano, T. M.: Fulvic-acid-like organic compounds control nucleation of marine calcite under suboxic conditions, Geology, 31, 681–684, 2003.
Neuweiler, F., Daoust, I., Bourque, P. A., and Burdige, D.: Degradative Calcification of a Modern Siliceous Sponge from the Great Bahama Bank, The Bahamas: A Guide for Interpretation of Ancient Sponge-Bearing Limestones, J. Sediment. Res., 77, 552–563, 2007.
Neuweiler, F., Kershaw, S., Boulvain, F., Matysik, M., Sendino, C., Mcmenamin, M., and Munnecke, A.: Keratose sponges in ancient carbonates – A problem of interpretation, Sedimentology, 70, 927–969, 2023.
Onorato, R., Forti, P., Belmonte, G., Costantini, A., and Poto, M.: La grotta sottomarina lu Lampiùne: novità esplorative e prime indagini ecologiche, Thalass, Salentina, 26, 55–64, 2003.
Onorato, R. and Belmonte, G.: Submarine caves of the Salento Peninsula: Faunal aspects, Thalass, Salentina, 39, 47–72, 2017.
Pérès, J. M.: Major Benthic Assemblages, in Marine Ecology, edited by: Kinne O., John-Wiley Publ. Lond., 5, 373–522, 1982.
Pérès, J. M. and Picard, J.: Nouveau manuel de bionomie benthique de la Méditerranée, Rec. Trav. Stat. Mar. Endoume, 31, 137 pp., 1964.
Perry, R. S., Mcloughlin, N., Lynne, B. Y., Septhon, M. A., Oliver, J. D., Perry, C. C., Campbell, K., Engel, M. H., Farmer, J. D., Brasier, M. D., and Staley, J. T.: Defining biominerals and organominerals: direct and indirect indicators of life, Sediment. Geol., 201, 157–179, 2007.
Phillips, A. J., Gerlach, R., Lauchnor, E., Mitchell, A. C., Cunningham, A. B., and Spangler, L.: Engineered applications of ureolytic biomineralization: a review, Biofouling, 29, 715–733, 2013.
Pickard, N. A. H.: Evidence for microbial influence on the development of Lower Carboniferous buildups, in: Recent Advances in Lower Carboniferous Geology, edited by: Strogen, P., Somerville, I. D., and Jones, G. L., Geol. Soc. Lond. Spec. Publ., 107, 65–82, 1996.
Pratt, B. R.: Microbial contribution to reefal mud-mounds in ancient deep-water settings: Evidence from the Cambrian, in: Microbial Sediments, edited by: Riding, R. E. and Awramik, M., 282–288, Springer, Berlin, 2000.
Rasser, M. W.: Coralline Red Algal Limestones of the Late Eocene Alpine Foreland Basin in Upper Austria: Component Analysis, Facies and Palecology, Facies, 42, 59–92, 2000.
Reid, R. P., Visscher, P. T., Decho, A. W., Stolz, J. K., Bebout, B. M., Dupraz, C., Mactintyre, I. G., Paerl, H. W., Pinckney, J. L., Prufert-Bebout, L., Steppe, T. F., and DesMarais, D. J.: The role of microbes in accretion, lamination and early lithification of modern marine stromatolites, Nature, 406, 989–992, https://doi.org/10.1038/35023158, 2000.
Reitner, J.: Modern cryptic microbialite/metazoan facies from Lizard Island (Great Barrier Reef, Australia): formation and concepts, Facies, 29, 3–40, 1993.
Reitner, J. and Neuweiler, F.: Mud Mounds: A polygenetic spectrum of fine-grained carbonate buildups, Facies, 32, 1–70, 1995.
Reitner, J., Gautret, P., Marin, F., and Neuweiler, F.: Automicrites in modern marine microbialite. Formation model via organic matrices (Lizard Island, Great Barrier Reef, Australia), Bull. Inst. Océanogr. (Monaco), 14, 237–264, 1995.
Reolid, M.: Taphonomy of the Oxfordian-Lowermost Kimmeridgian Siliceous Sponges of the Prebetic Zone (Southern Iberia), J. Taphonomy, 5, 71–90, 2007.
Reolid, M.: Interactions between microbes and siliceous sponges from Upper Jurassic buildups of External Prebetic (SE Spain), Lect. Notes Earth Sci., 131, 319–330, 2010.
Riding, R.: Microbial carbonates: the geological record of calcified bacterial-algal mats and biofilms, Sedimentology, 47, 179–214, 2000.
Riding, R.: Structure and Composition of Organic Reefs and Carbonate Mud Mounds: Concepts and Categories, Earth-Sci. Rev., 58, 163–231, 2002.
Riding, R.: Microbialites, stromatolites, and thrombolites, in: Encyclopedia of Geobiology, Encyclopedia of Earth Science Series, edited by: Reitner, J. and Thiel, V., Springer, Heidelberg, 635–654, 2011.
Riding, R. and Liang, L.: Geobiology of microbial carbonates: metazoan and seawater saturation state influences on secular trends during the Phanerozoic, Palaeogeogr. Palaeocl., 219, 101–115, 2005.
Riding, R. and Tomás, S.: Stromatolite reef crusts, Early Cretaceous, Spain: bacterial origin of in situ precipitated peloid microspar?, Sedimentology, 53, 23–34, 2006.
Riding, R. and Virgone, A.: Hybrid Carbonates: in situ abiotic, microbial and skeletal coprecipitates, Earth Sci. Rev., 208, 103300, https://doi.org/10.1016/j.earscirev.2020.103300, 2020.
Riding, R., Liang, L., and Braga, J. C.: Millennial-scale ocean acidification and late Quaternary decline of cryptic bacterial crusts in tropical reefs, Geobiology, 12, 387–405, 2014.
Rosell, D. and Uriz, M. J.: Do associated zooxanthellae and the nature of the substratum affect survival, attachment and growth of Cliona viridis (Porifera: Hadromerida)? An experimental approach, Mar. Biol., 114, 503–507, 1992.
Rosso A. and Sanfilippo R.: The contribution of bryozoans and serpuloideans to coralligenous concretions from SE Sicily, in: UNEP-MAP-RAC/SPA, Proc. First Symposium on the Coralligenous and other calcareous bio-concretions of the Mediterranean Sea, Tabarka, 123–128, 2009.
Rosso, A., Sanfilippo, R., Guido, A., Gerovasileiou, V., Taddei Ruggiero, E., and Belmonte, G.: Colonisers of the dark: biostalactite-associated metazoans from “lu Lampiùne” submarine cave (Apulia, Mediterranean Sea), Mar. Ecol. 42, e12634, https://doi.org/10.1111/maec.12634, 2020.
Rosso, A., Altieri, C., Bazzicalupo, P., Bertolino, M., Bracchi, V.A., Bruno, F., Cipriani, M., Costa, G., D’alpa, F., Donato, G., Fallati, L., Gallo, A., Guido, A., Leonardi, R., Muzzupappa, M., Negri, M. P., Sanfilippo, R., Savini, A., Sciuto, F., Serio, D., Taddei Ruggiero, E., Varzi, A. G., Viola, A., and Basso D.: Bridging together research and technological innovation: first results and expected bearings of the project cresciblureef on mediterranean coralligenous. 4th Mediterranean Symposium on the conservation of Coralligenous & other Calcareous Bio-Concretions, Genoa, 108–113, 2023.
Sanfilippo, R., Rosso, A., Guido, A, Mastandrea, A., Russo, F., Riding, R., and Taddei Ruggiero, E.: Metazoan/microbial biostalactites from present-day submarine caves in the Mediterranean Sea, Mar. Ecol., 36, 1277–1293, 2015.
Sanfilippo, R., Rosso, A., Guido A., and Gerovasileiou, V.: Serpulid communities from two marine caves in the Aegean Sea, eastern Mediterranean, J. Mar. Biol. Assoc. UK, 97, 1059–1068, 2017.
Sartoretto, S., Verlaque, M., and Labore, J.: Age of settlement and accumulation rate of submarine “coralligène” (−10 to −60 m) of the northwestern Mediterranean Sea; relation to Holocene rise in sea level, Mar. Geol., 130, 317–331, 1996.
Schönberg, C. H. L.: A history of sponge erosion: from past myths and hypotheses to recent approaches, in: Current Developments in Bioerosion, edited by: Wisshak, M. and Tapanila, L., 165–202, Springer-Verlag Berlin, 2008.
Sciuto, F., Altieri, C., Basso, D., D’Alpa, F., Donato, G., Bracchi,V. A., Cipriani, M., Guido, A., Rosso, A., Sanfilippo, R., Serio, D., and Viola, A.: Preliminary data on ostracods and foraminifers living on coralligenous bioconstructions Offshore Marzamemi (Ionian Sea, Se Sicily), Rev. Micropaléontol., 18, 100711, https://doi.org/10.1016/j.revmic.2023.100711, 2023.
Scott, P. J. B., Moser, K. A., and Risk, M. J.: Bioerosion of concrete and limestone by marine organisms: a 13 year experiment from Jamaica, Mar. Pollut. Bull., 19, 219–222, 1988.
Shen, Y. and Neuweiler, F.: Questioning the microbial origin of automicrite in Ordovician, Calathid–Demosponge carbonate mounds, Sedimentology, 65, 303–333, 2018.
Stockman, K. W., Ginsburg, R. N., and Shinn, E. A.: The production of lime mud by algae in South Florida, J. Sediment. Petrol., 37, 633–648, 1967.
Titschack, J., Nelson, C. S., Beck, T., Freiwald, A., and Radtke, U.: Sedimentary Evolution of a Late Pleistocene Temperate Red Algal Reef (Coralligène) on Rhodes, Greece: Correlation with Global Sea-Level Fluctuations, Sedimentology, 55, 1747–1776, 2008.
Trichet, J. and Défarge, C.: Non biologically supported organomineralization, in: Proc. 7th Int. Symp. Biomineralization, edited by: Allemand, D. and Cuif, J. P., Bulletinde l'Institut Océanographique de Monaco, 14, 203–236, 1995.
Tucker, M. E. and Wright, V. P.: Carbonate Sedimentology, London, Blackwell Scientific Publications, 488 pp., 1990.
Turicchia, E., Abbiati, M., Bettuzzi, M., Calcinai, B., Morigi, M. P., Summers, A. P., and Ponti, M.: Bioconstruction and Bioerosion in the Northern Adriatic Coralligenous Reefs Quantified by X-Ray Computed Tomography, Front. Mar. Sci., 8, 790869, https://doi.org/10.3389/fmars.2021.790869, 2022.
Van Driessche, A. E. S., Stawski, T. M., and Kellermeier, M.: Calcium sulfate precipitation pathways in natural and engineered environments, Chem. Geol., 530, 119274, https://doi.org/10.1016/j.chemgeo.2019.119274, 2019.
Varzi, A. G., Fallati, L., Savini, A., Bracchi, V. A., Bazzicalupo, P., Rosso, A., Sanfilippo, R., Bertolino, M., Muzzupappa, M., and Basso, D.: Geomorphological mapping of Coralligenous reefs offshore southeastern Sicily (Ionian Sea), J. Maps, 19, 2161963, https://doi.org/10.1080/17445647.2022.2161963, 2023.
Warnkle, K.: Calcification processes of siliceous sponges in Visean Limestones (Counties Sligo and Leitrim, northwestern Ireland), Facies, 33, 215–228, 1995.
Weiner, S. and Dove, P. M.: An overview of biomineralization processes and the problem of the vital effect, Biomineralization, 54, 1–29, 2003.
Wolf, K. H.: Gradational sedimentary products of calcareous algae, Sedimentology, 5, 1–37, https://doi.org/10.1111/j.1365-3091.1965.tb01556.x, 1965.
Wood, R.: Are reefs and mounds really so different?, Sediment. Geol., 145, 161–171, 2001.
Short summary
Who constructs the build-ups of the Mediterranean Sea? What is the role of skeletal and soft-bodied organisms in these bioconstructions? Do bacteria play a role in their formation? In this research, for the first time, the coralligenous of the Mediterranean shelf is studied from a geobiological point of view with an interdisciplinary biological and geological approach, highlighting important biotic relationships that can be used in interpreting the fossil build-up systems.
Who constructs the build-ups of the Mediterranean Sea? What is the role of skeletal and...
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