Monitoring Carbonate Production and Degradation (Azores, Portugal)
Project code: DFG-Fr 1134/12
Coordinator: André Freiwald
Project Staff: Max Wisshak (GZN)
Project Partner: Kirsten + Joachim Jakobsen (Rebikoff-Niggeler Foundation)
Duration: 2006-2009
Studies on the various facies of the widespread cool-water carbonate factory in the N-Atlantic are far advanced, however, quantitative data on growth and degradation rates are almost lacking. This project focused on the warm-temperate Azores Archipelago because of its remote location far from land, its poorly studied carbonate environment and because of the easy accessibility to a manned submersible at the island Faial. By covering a wide environmental gradient with respect to light regime and different water-mass properties along a bathymetric transect (0-500 m), we budgeted carbonate-accretion and bioerosion rates with an experimental approach.
Complementing, we undertook detailed morphological and geochemical analyses (stable 18O and 13C isotopes, trace elements) of selected long-living calcareous epibenthos (stylasterids, corals, oysters) for growth-rate analyses and for the detection of subtle climate variability in this area. In this respect, the main focus was laid on the exceptional occurrence of enigmatic deep-water oysters, which we established as a new species Neopycnodonte zibrowii. With the aid of radiocarbon dating, we where able to reveal that these oysters reach a remarkable centennial longevity of more than 400 years and thus range among the longest-lived non-colonial organisms we know on earth. With mainly Mesozoic relatives, this species is aptly called a "living fossil" and occurs in close association with another relict of ancient time, the small crinoid Cyathidium foresti.
The experiment itself comprises quantitative and qualitative monitoring of carbonate production and degradation as well as the recording of in situ environmental data (temperature, salinity and photosynthetically active radiation along with depth). The anticipated results are expected to yield (1) warm-temperate carbonate-production and bioerosion rates, (2) enhanced insight in the suitability of stable isotopes for growth rate studies and high-resolution climate variability analyses, (3) knowledge on the bathymetric as well as biogeographic distribution of bioeroding and carbonate-accreting agents and (4) new insights in the relative contribution of boring organisms versus grazers on different substrate orientations to the process of bioerosion.

- The bathymetric transect with the five deployment sites (0, 5, 50, 150 and 500 m), covering all photic zones from the intertidal euphotic zone down to aphotic depths. The inset illustrates the principal design of the experimental panels with four sets of carbonate and PVC substrates facing up- and downwards, two of which fenced from grazing organisms with the aid of a PVC mesh. In addition, mollusc shells and autonomous temperature and salinity data loggers were mounted on the experimental frames. On the schematic hardground to the left, the most important sessile calcareous epizoans to be investigated are illustrated (© M. Wisshak).
The Azores archipelago has been chosen as an ideal site for this experimental approach where K. and J. Jakobsen of the Rebikoff-Niggeler Foundation provide us with the unique chance to carry out a sophisticated bioerosion and carbonate-accretion experiment with the aid of a submersible at comparably very low costs. The modern submersible "Lula" is equipped with high-end video equipment, various sensors and a manipulator and allows us to cover a bathymetric transect reaching down to 500 m water depth. This gives us a maximum of control on the selection of proper experimental sites and a successful and efficient deployment and recovery, respectively.

- The submersible "Lula" in action. B: The large semi-spherical front window and the two pilots of "Lula". C: A typical hardground inhabited by various hard and soft-bodied benthic organisms. D: A spectacular occurrence of giant oysters of the new species Neopycnodonte zibrowii densely occupying an overhanging hardground cropping out in 490 m water depth. E: One representative of the diverse stylasterids, that thrive well at Faials southern slope - another prime candidate for longevity and stable isotope studies in the proposed project. F: The manipulator of "Lula" in action (all images © Rebikoff-Niggerler Foundation).
During September 2006, the experimental frames were successfully deployed in the south Faial Channel in intense collaboration with K. and J. Jakobsen, supported by C. Michels. Two of the panels were positioned at various depth stations between 5 and 500 m water depth and were recovered in 2007 and 2008 after one and two years of exposure, respectively. During a total of 15 missions with research submersible "Lula", selected sample material of calcareous epibenthos, as well as numerous water samples were taken, and the habitat characteristics and faunal diversity was documented.

- A. Mounting the panels in a purpose built release mechanism. B: "Lula" on its way to the dive site; The neighbouring volcano Pico in the background. C+D: Two of the experimental frames sitting next to each other on the sea-floor in 150 m water depth. E: A large gorgonian in about 350 m water depth. F: A rocky overhanging outcrop with large deep-sea oysters attached to it (A+B © Max Wisshak; C-F © Rebikoff-Niggerler Foundation).
One month ahead and as a valuable addition to the ongoing project, three further experimental frames were deployed in arctic Spitsbergen at almost 80° northern latitude in the course of the polar expedition of the
MS Merian 2/3. In this case, the deployment was carried out with the aid of the approved research submersible "Jago".

- A. The reseach vessel "MS Merian" and the submersible "Jago" at Spitsbergen. B: Recovery of "Jago" after a successful sampling dive. C: After hooking in one of the panels to the submersible ?Jago?. D: One of the deployed panels in 46 m water depth - the maximum of the local rodolithe occurrence (calcareous red algae). E: In order to assess the depth of the photic zonation, detailed light measurements were carried out. F: One of the sampled rhodolithe spheres (all images © Max Wisshak).
Publications on the Azores Project
- Wisshak M, Form A, Jakobsen J & Freiwald A (2010) Temperate carbonate cycling and water mass properties from intertidal to bathyal depths (Azores). Biogeosciences 7:3279-2396
- Wisshak M, Form A, Jakobsen J & Freiwald A (2010) Temperate carbonate cycling and water mass properties from intertidal to bathyal depths (Azores, N-Atlantic). Biogeosciences Discussssions 7:3297-3333
- Wisshak M, López Correa M, Zibrowius H, Jakobsen J & Freiwald, A (2009) Skeletal reorganisation affects geochemical signals, exemplified in the stylasterid hydrocoral Errina dabneyi (Azores Archipelago). Marine Ecology Progress Series 397:197-208
- Wisshak M, Neumann C, Jakobsen J & Freiwald A (2009) Reply to the Comment on "The ‘living-fossil community’ of the cyrtocrinoid Cyathidium foresti and the deep-sea oyster Neopycnodonte zibrowii (Azores Archipelago). [Palaeontology, Palaeoclimatology, Palaeoecology 271:77-83]". Palaeontology, Palaeoclimatology, Palaeoecology
- Wisshak M, Neumann C, Jakobsen J & Freiwald A (2009) The ‘living-fossil community’ of the cyrtocrinoid Cyathidium foresti and the deep-sea oyster Neopycnodonte zibrowii (Azores Archipelago). Palaeontology, Palaeoclimatology, Palaeoecology 271:77-83
- Wisshak M, López Correa M, Gofas S, Salas C, Taviani M, Jakobsen J & Freiwald A (2009) Shell architecture, element composition, and stable isotope signature of the giant deep-sea oyster Neopycnodonte zibrowii sp. n. from the NE Atlantic. Deep-Sea Research I 56:374-404
