R&D and Education

Fionnbarr Moore, Connie Kelleher, Karl Brady, Charise McKeon & Ian Lawler

“RMS Lusitania, The Story of a wreck” discusses the historical, archaeological and cultural significance of one of the world’s most important shipwrecks. The book was officially launched by Minister Josepha Madigan, Department of Culture, Heritage and the Gaeltacht and Minister Sean Canney, Department of Communications, Climate Action and the Environment in the Custom House on Thursday December 5th.

Expertise from Geological Survey Ireland (GSI) and the Marine Institute (MI) in collaboration with the Underwater Archaeology Unit (UAU), National Monuments Service and the National Museum of Ireland is drawn upon and combined with contributions from independent researchers, divers and a variety of specialists to give a fresh approach to the story of this wreck. The book is dedicated to all those who lost their lives on the RMS Lusitania.

A fresh approach to the story of this wreck is documented which tells of its building, its early voyages and its part in WWI. On 7th May 1915 the RMS Lusitania had almost completed a transatlantic voyage en route from New York to Liverpool when it was torpedoed by U-20. Within 18 minutes the Lusitania sank. The torpedo struck midship on the starboard side, under the bridge or just aft of it. A second explosion followed. Of the 1,960 people on board 1,193 lives were lost. Accounts from survivors and the rescue efforts that took place are documented. Rescue boats from Kinsale, Cobh and the surrounding areas assisted. Over 100 years after the event the question still remains as to what caused the second explosion.

The wreck of the Lusitania lies 11.5 nautical miles off the Old Head of Kinsale in a water depth of 93m. Diving and salvage became part of the history of this wreck since its sinking.  In 1995 an Underwater Heritage Order was placed on the wreck by the then Minister for Arts, Culture and Gealtacht Michael D. Higgins to ensure its protection and preservation. The role of the UAU is to ensure its continued protection. The INFOMAR project has worked closely with the UAU in carrying out multiple surveys of the wreck since 2002 to assist in its monitoring. While it is slowly collapsing the bow of the wreck is still proud of the seabed and structural elements of the wreck are still clearly visible. 

The book is a collaborative effort by the Department of Culture, Heritage and the Gaeltacht and the Department of Communications, Climate Action and Environment.

 

The book is on sale now both online and in bookshops nationwide priced at €20. Get your copy here.

Fionnbarr Moore, Connie Kelleher, Karl Brady, Charise McKeon &…


Ronan O'Toole, Maria Judge, Fabio Sacchetti, Thomas Furey, Eoin Mac Craith, Kevin Sheehan, Sheila Kelly, Sean Cullen, Fergal McGrath and Xavier Monteys.

Geological Society, London, Special Publications, 505, 9 September 2020,

 

Abstract
Through Ireland's national seabed mapping programme, Integrated Mapping for the Sustainable Development of Ireland's Marine Resource (INFOMAR), the collaboration between Geological Survey Ireland and the Marine Institute continues to comprehensively map Ireland's marine territory in high resolution. Through its work, the programme builds on earlier Irish seabed mapping efforts, including the Irish National Seabed Survey project in producing seabed mapping products that support Ireland's blue economy, European marine policy and international efforts to understand our global oceans. INFOMAR uses a variety of marine technologies to deliver accurate bathymetric maps and useful data products to end users through a free and open source licensing agreement. To reflect the diversity of applications these data products serve, a series of four case studies are presented here focusing on marine geophysical and geological data from locations within Ireland's marine territories. The case studies illustrate how data generated through seabed mapping may be interpreted to directly impact the generation of blue knowledge across a variety of marine environments ranging from shallow coastal and shelf waters to the deep oceanic depths of the continental slope of Ireland's marine area. The impact of Ireland's seabed mapping efforts is further considered in the context of national, European and international initiatives where Ireland's marine knowledge resource is leveraged to deliver positive benefit to the programme's stakeholders.

 

Full article available for download here: https://sp.lyellcollection.org/content/early/2020/09/08/SP505-2019-207

J. Guinan, C. McKeon, E. O'Keeffe, X. Monteys, F. Sacchetti, M. Coughlan and C. Nic Aonghusa

Quarterly Journal of Engineering Geology and Hydrogeology 9 September 2020.

 

Abstract
The characterization of the seafloor is a fundamental first step in informing resource management, marine spatial planning, conservation, fisheries, industry and research. Integrated Mapping for the Sustainable Development of Ireland's Marine Resource (INFOMAR), Ireland's national seabed mapping programme, delivers freely available, high-resolution seabed imagery derived from multibeam echosounder data in the Irish Exclusive Economic Zone. The European Union established the European Marine Observation and Data Network (EMODnet) Geology data portal, which provides harmonized broad-scale seabed substrate information for all European seas and confidence assessments of the information that underpins the geological interpretations. A multi-scale product has been produced using INFOMAR's high-resolution seabed substrate information at the 1:50 000 scale. As part of the Supporting Implementation of Maritime Spatial Planning in the Celtic Seas project, the EMODnet Geology seabed substrate data portal assisted in addressing the challenges associated with the implementation of the European Union's Marine Spatial Planning Directive. The seabed substrate data in the EMODnet Geology data portal were identified as a valuable tool for guiding the selection of sites for offshore wind farms in the Irish Sea and their subsequent characterization. This paper outlines the approach to delivering a multi-scale seabed substrate dataset for the Irish offshore and its applicability to marine spatial planning and the development of offshore energy resources.

Full article available for download here: https://qjegh.lyellcollection.org/content/early/2020/09/07/qjegh2020-033 

EUSeaMap 2019, A European broad-scale seabed habitat map, technical report.

EASME/EMFF/2018/1.3.1.8/Lot2/SI2.810241– EMODnet Thematic Lot n° 2 – Seabed Habitats.

Abstract

EUSeaMap 2019 is the third iteration of EUSeaMap. All versions have been produced as part of the EMODnet Seabed Habitats project, which is one of several thematic lots in EMODnet. The project has brought together a European consortium of specialists in benthic ecology and seabed habitat mapping. The partners first collaborated in EMODnet phase 1 (2009-2012) to deliver a prototype predictive seabed habitat map in four trial basins (Greater North Sea, Celtic Seas, Baltic, Western Mediterranean). This predictive model was named EUSeaMap (Cameron and Askew, 2011). In EMODnet Phase 2 (2012-2016), the consortium extended EUSeaMap coverage to all European regions (Populus et al, 2017).

In the new version, the spatial coverage was extended further North in order to include the Barents Sea. The spatial detail was substantially improved. This was made possible by improvements to the physical predictor variables created by the other EMODnet lots which are the input data to the EUSeaMap model. A substantial revision of the map creation process has also been carried out in order to make it more reproducible. This document describes all these modifications which have led to the elaboration of EUSeaMap 2019.

Authors

Vasquez Mickael, Manca Eleonora, Inghilesi Roberto, Martin Simon, Agnesi Sabrina, Al Hamdani Zyad, Annunziatellis Aldo, Bekkby Trine, Pesch Roland, Askew Natalie, Bentes Luis, Castle Lewis, Doncheva Valentina, Drakopoulou Vivi, Gonçalves Jorge, Laamanen Leena, Lillis Helen, Loukaidi Valia, McGrath Fergal, Mo Giulia, Monteiro Pedro, Muresan Mihaela, O'Keeffe Eimear, Populus Jacques, Pinder Jordan, Ridgeway Amy, Sakellariou Dimitris, Simboura Mika, Teaca Adrian, Tempera Fernando, Todorova Valentina, Tunesi Leonardo, Virtanen Elina (2020).

DOI 10.13155/74782 

 

EUSeaMap 2019, A European broad-scale seabed habitat map, technical…

The Atlantic Seabed Mapping Vision Statement and Roadmap arises from the activities of the Atlantic Seabed Mapping International Work Group and is conducted through the Atlantic Ocean Research Alliance (AORA) between Canada, the European Union and the United States of America. The progress and vision towards achieving a baseline seabed and habitat map of the Atlantic Ocean, was presented at the All Atlantic Ocean Research Forum, 6-7 February 2020, in Brussels, Belgium. The Seabed Mapping Group has, in the last five years, defined and tested all the necessary steps to map the previously uncharted seafloor of the Atlantic Ocean. With the onset of the UN Decade of Ocean Science for Sustainable Development, the Seabed Mapping Group calls on the international leaders to provide the resources and framework necessary to achieve this ambitious goal, in order to deliver on their commitment to the Galway and Belém Statements. Creating an accurate fact based map of the Atlantic seafloor is essential for the sustainable use of our ocean, and will greatly help us to achieve the UN Sustainable Development Goal, SDG 14 – Life Below Water. A diverse group of stakeholders participated in this work and the outcome summarized here in this roadmap is a result of extensive consultation with workshop and meeting participants, as well as others that were invited to comment on the work as it progressed. The editorial team would like to thank all those who contributed with comments and input. 

Brochure can be downloaded here. 

The Atlantic Seabed Mapping Vision Statement and Roadmap arises from…

Roy S., Georgiopoulou A., Benetti S., Sacchetti F.

Geological Society, London, Special Publications. 10.1144/SP500-2019-177 
http://sp.lyellcollection.org/content/early/2020/01/16/SP500-2019-177.abstract

This study analyses seismic data to investigate the kinematic indicators within the mass transport deposits (MTDs) of the Donegal Barra Fan complex in the Rockall Trough, along the NW European continental margin. Five episodes of mega-scale MTDs (DBF-01, -02, -03, -04 and -05) are identified. DBF-01 is the largest MTD in the Northwest British continental margin, comprising of 1907 km3 of sediments. Fold-and-thrusts were identified within the MTDs where they attain maximum thickness of c. 300–380 ms-TWT, but not at the toe region. This indicates that local erosion and deceleration caused bulking up of the MTD volume, but the MTD was not fully arrested due to the high mobility of the mass flow. MTD thickness distribution and thrust fault orientations indicate source areas and flow direction of MTD. The MTDs show a compensational stacking pattern with earlier deposits influencing the position and flow direction of succeeding slides, suggesting that glaciogenic debris flows are sensitive to topographic variability. We propose that increased sediment input associated with at least five expansions of the British Irish Ice Sheet to the shelf edge led to the development of these MTDs and that the youngest of them, DBF-05, corresponds to the Last Glacial Maximum.

Supplementary material at https://doi.org/10.6084/m9.figshare.c.4816911

McCullagh D., Benetti S., Plets R., Sacchetti F., O’Keeffe E. and Lyons K.

https://figshare.com/articles/Geomorphology_and_substrate_of_Galway_Bay_Western_Ireland/11769981
doi = 10.6084/m9.figshare.11769981.v1

A combination of multibeam bathymetry and backscatter, LiDAR altimetry and bathymetry, satellite images, and hydrodynamic model outputs were used to map the seafloor and coastline of Galway Bay (western Ireland). This is the first time these multiple datasets have been integrated into a single combined geomorphological and substrate map. The substrate of the bay is predominantly mud and sand with bedrock outcropping extensively around the coastline. The main depositional features are dunes, while the main erosional features are scours and outcropping bedrock. Hydrodynamic model outputs show good correlation between the direction and intensity of prevailing currents and the location and shape of the features in the bay. This indicates that although Galway Bay was shaped glacially through the passage of the British-Irish Ice Sheet across the bay and ensuing glacial and marine sediment deposition, many of the mapped seafloor landforms are modern and current-induced.

McCullagh D., Benetti S., Plets R., Sacchetti F., O’Keeffe E.…

D. O’Sullivan, Y. Leahy, J. Guinan, R. Ross, F. Sacchetti, Kerry Howell, David Lyons, Leonie O’Dowd,
Chapter 47 - The geomorphology and biology of a submarine canyon system incising Ireland’s shelf edge in the Northeast Atlantic Ocean,
Editor(s): Peter T. Harris, Elaine Baker,
Seafloor Geomorphology as Benthic Habitat (Second Edition),
Elsevier,
2020,
Pages 783-792,
ISBN 9780128149607,
https://doi.org/10.1016/B978-0-12-814960-7.00047-6.
(http://www.sciencedirect.com/science/article/pii/B9780128149607000476)
Abstract: This case study presents preliminary findings of an extensive offshore reef survey, funded by the European Maritime and Fisheries Fund Marine Biodiversity Scheme, along Ireland’s Northwest continental margin. The 2017 study focuses on one specific canyon system, and its biological habitats in relation to geomorphic features. The survey is primarily concerned with identifying geogenic and biogenic reefs and associated biological communities. High-definition video footage was acquired using a remotely operated underwater vehicle. We present five separate transects from within a previously undescribed canyon system with little anthropogenic interference. The video data identifies biologically sensitive, reef-forming, cold-water coral species at numerous locations. Typical fauna include anemones, sponges, crustaceans, corals, echinoderms, elasmobranchs, flatfish, and deep-sea fish such as the orange roughy. The findings will contribute to the provision of conservation objectives as established by the Government of Ireland’s National Parks and Wildlife Service.
Keywords: Geogenic; biogenic reef; cold-water coral; seabed geomorphology; benthic habitat; northeast Atlantic; ROV

Conor Cahalane, Aidan Magee, Xavier Monteys, Gema Casal, Jennifer A. Hanafin, P. Harris (2019) A comparison of Landsat 8, RapidEye and Pleiades products for improving empirical predictions of satellite-derived bathymetry, Remote Sensing of Environment, DOI: https://doi.org/10.1016/j.rse.2019.111414


Satellite derived bathymetry (SDB) enables rapid mapping of large coastal areas through measurement of optical penetration of the water column. The resolution of bathymetric mapping and achievable horizontal and vertical accuracies vary but generally, all SDB outputs are constrained by sensor type, water quality and other environmental conditions. Efforts to improve accuracy include physics-based methods (similar to radiative transfer models e.g. for atmospheric/vegetation studies) or detailed in-situ sampling of the seabed and water column, but the spatial component of SDB measurements is often under-utilised in SDB workflows despite promising results suggesting potential to improve accuracy significantly. In this study, a selection of satellite datasets (Landsat 8, RapidEye and Pleiades) at different spatial and spectral resolutions were tested using a log ratio transform to derive bathymetry in an Atlantic coastal embayment. A series of non-spatial and spatial linear analyses were then conducted and their influence on SDB prediction accuracy was assessed in addition to the significance of each model's parameters. Landsat 8 (30 m pixel size) performed relatively weak with the non-spatial model, but showed the best results with the spatial model. However, the highest spatial resolution imagery used – Pleiades (2 m pixel size) showed good results across both non-spatial and spatial models which suggests a suitability for SDB prediction at a higher spatial resolution than the others. In all cases, the spatial models were able to constrain the prediction differences at increased water depths.