Marine biological data from the 2004 voyage of the R/V Tangaroa (TAN0402) to the Ross Sea, Antarctica. The main objective of the New Zealand Ministry of Fisheries (now Ministry for Primary Industries) project (BioRoss) was to carry out a quantitative survey of the biodiversity of selected marine communities in the Ross Sea region, including the Balleny Islands. The survey programme was divided into two separate objectives. 1. Ross Sea component (14 days): This comprised 5 across-shelf (generally aligned SW-NE) transects from 50m bottom depth to the shelf edge (∼750m). Each transect was to be multibeamed (in an offshore direction) to establish bathymetry (& backscatter), and to be sampled along the return path within three depth strata (750-500, 500-250, 250-50m) by grab/camera, epibenthic sled/camera, and trawl. 2. Balleny Islands component (3 days): This comprised sampling seamounts associated with the Balleny Islands. Three features were targeted – the slopes of the islands of Young/Borradaile/Buckle (effectively a single seamount), Sturge Island and Balleny Seamount . On each seamount a minimum of 4 random (by depth and direction) stations were to be sampled using the three methods (grab/camera, epibenthic sled/camera, trawl).
During the Trans-Antarctic Expedition 1955-1958, the distribution of phytoplankton in the southern ocean and Ross Sea was investigated from fifty-seven samples taken at roughly 30-mile intervals between southern New Zealand and McMurdo Sound. The greatest diversity of species occurred between 55° and 60°S, just north of the Antarctic Convergence. Maximum concentration was found at 70° to 72°S, where Corethron crioplhilum was profoundly dominant. A predominately sub-Antarctic assemblage between 52° and 64°S was dominated by nine species not found in significant quantities elsewhere in the series of samples. Only two of these extended in appreciable numbers into the Ross Sea. Six of the commonest species ranged from sub-Antarctic waters southwards across the Antarctic Convergence, and two were not recorded north of the Ross Sea.
This dataset contains the underway data collected during the Tangaroa Voyage TAN0003 in 2000. This voyage carried out marine science studies off the Antarctic coast between the Dibble ice tongue and Ninnis Glacier as part of an experiment to study the effect of the Mertz Polynya on Antarctic bottom water formation. The voyage departed on 12th February 2000 from and returned on the 24th March 2000 to Wellington, NZ. Data include: latitude, longitude, date, time, ship heading, pitch, roll, relative humidity, air temperature, salinity, sea temperature, wind direction, and wind speed.
The biological data from the IPY-CAML voyage (TAN0802) by the R/V Tangaroa is available as an Darwin Core archive through the Southwestern Pacific OBIS IPT node. The TAN0802 voyage departed from Wellington, New Zealand, on 26 Jan 2008 and returned to Wellington, New Zealand, on 21 Mar 2008. The survey was concentrated mainly in the Ross Sea and the waters around Scott Island and the Balleny Islands. Biological data were collected using a variety of gear, including: bottom trawls, beam trawls, epibenthic sleds, van Veen grabs, rosette water bottles and MOCNESS tows.
Total column ozone and ozone partial columns measured in Dobson Units (1DU = 2.69×1016 ozone molecules/cm2). Dobson spectrophotometer instruments are located at Lauder (45.04oS, 169.68oE), New Zealand, and at Arrival Heights (77.82oS, 166.65oE), Antarctica. Archives of the measurements are maintained at NIWA, Lauder, and in various international data archives. A combined data set of satellite-based total column ozone measurements providing global coverage is maintained at NIWA using measurements from a variety of satellite-based instruments including TOMS, GOME, SBUV, and OMI.
The known macroalgal flora of the Balleny Islands, Southern Ocean, has more than doubled as a result of expeditions to the area over the past 8 years and their subsequent study is reported here. The samples collected as part of a benthic survey at Borradaile Island, one of the Balleny Islands group, during the 2006 Tiama expedition have been analysed to provide an assessment of benthic community structure. We provide a quantitative assessment of shallow water macrofaunal community composition and seafloor sediment characteristics, and a more qualitative assessment of seafloor habitat structure and epifaunal/floral community composition. The Borradaile Island sites were located in a high energy environment, sediments had relatively high organic and chlorophyll a content, and considerably lower concentrations of degraded plant material (phaeophytin) than noted in previously surveyed southern Ross Sea locations. This could be a reflection of the higher light levels and the large amount of algal detritus noted at the higher latitude Borradaile sites. Borradaile Island macrofaunal diversity was within the range noted for the more southern sites; macrofaunal abundance, however, was more variable. Epifaunal diversity was very low at the Borradaile Island sites, with the seastar Odontaster validus the only large epifaunal taxon found. In contrast, the Borradaile Island dive sites had high macroalgal diversity. Although not observed at the Borradaile Island dive sites, the Tiama voyage researchers noted shallow water areas with high diversities of encrusting organisms. This study has provided the first analysis of shallow water benthic communities of the Balleny Islands. While it has shown some interesting similarities and contrasts in benthic diversity with other coastal Ross Sea locations, this information from Borradaile Island may not be representative of the entire Balleny area, and further surveys from other sites within the Balleny group are recommended. In 2005, Ministry of Fisheries (MFish) scientists and Ministry of Foreign Affairs and Trade (MFAT) personnel prepared a paper for submission to CCAMLR justifying a Marine Protected Area (MPA) designation for the islands. To collect data in support of the MPA proposal, MFish commissioned a month-long targeted research voyage to the Balleny Islands in February 2006, using the yacht Tiama, (“Balleny Islands Ecology Research Voyage”; ZBD2005-01). MFish also obtained additional samples from the Balleny Islands during a 7-week voyage to the Ross Sea using Tangaroa (“Ross Sea Biodiversity”; ZBD2005-03). In 2004, Tangaroa sampled 49 sites in the Ballenys region as part of a BioRoss voyage (TAN0402 - Biodiversity of deepwater invertebrates and fish communities of the North Western Ross Sea), The Tiama and Tangaroa voyages were very successful, providing important ecological information and specimens from the Balleny Islands area, and supplementary information for the Antarctic Working Group Research Programme. The Tiama voyage included a survey of shallow water benthic faunal communities and habitats using the methods developed for NIWA’s coastal Antarctic research project, ICECUBE (ZBD2001-02). To our knowledge this is the first quantitative sampling of shallow water benthos around these islands. The objectives of this study were (1) to describe and characterise macroalgae diversity from the Balleny Islands and the Western Ross Sea, and (2) to describe and quantify benthic community structure from one location at the Balleny Islands. This report describes the macroalgal collections obtained on recent and earlier voyages and expeditions to the region as well as presenting an analysis of results of the Tiama’s shallow water benthic survey. The diversity of macroalgal and benthic communities and habitats are compared to that of other Ross Sea locations. The data in this sampling event resource has been published as a Darwin Core Archive (DwC-A), which is a standardized format for sharing biodiversity data as a set of one or more data tables. See also: Nelson, W.; Cummings, V.; D’Archino, R.; Halliday, J.; Marriott, P.; Neill, K. (2010). Macroalgae and benthic biodiversity of the Balleny Islands, Southern Ocean. New Zealand Aquatic Environment and Biodiversity Report No. 55
Water chemistry data collected the Andrill Coulman High site on the Ross Ice Shelf in December 2010.