Stable isotope data from marine sediment and invertebrates from Davis Station 2009/10

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Description

This metadata record contains an Excel file containing stable isotope analysis data of marine sediments and invertebrates collected at Davis Station from December 2009 to March 2010. Refer to Gillies et al. 2013 for sampling and analysis details. Gillies C.L., Stark J.S., Johnstone G.J., Smith S.D.A., 2013. Establishing a food web model for coastal Antarctic benthic communities: a case study from the Vestfold Hills, Marine Ecology Progress Series, Vol. 478: 27 – 41. Also refer to the Davis STP reports lodged under metadata record Davis_STP for methods and result details. Background of the Davis STP project Refer to the Davis STP reports lodged under metadata record Davis_STP.Quality: The original datasheet was reformatted to fit OBIS/ GBIF/IPT Biodiversity.AQ standard. The new datasheet "DavisStationStableIsotopes.csv" provides the dataset ID, event ID, recordNumber, occurrenceID, eventDate, decimalLatitude, decimalLongitude, continent, occurrenceStatus, basisOfRecord. The taxonomical organisation is provided to the lowest taxonomical rank that could be determined, after matched in WoRMS (World Register of Marine Species).

Enregistrements de données

Les données de cette ressource occurrence ont été publiées sous forme dune Archive Darwin Core (Darwin Core Archive ou DwC-A), le format standard pour partager des données de biodiversité en tant quensemble dun ou plusieurs tableurs de données. Le tableur de données du cœur de standard (core) contient 576 enregistrements.

Cet IPT archive les données et sert donc de dépôt de données. Les données et métadonnées de la ressource sont disponibles pour téléchargement dans la section téléchargements. Le tableau des versions liste les autres versions de chaque ressource rendues disponibles de façon publique et permet de tracer les modifications apportées à la ressource au fil du temps.

Versions

Le tableau ci-dessous naffiche que les versions publiées de la ressource accessibles publiquement.

Comment citer

Les chercheurs doivent citer cette ressource comme suit:

Gillies C.L., Stark J.S., Johnstone G.J., Smith S.D.A., 2013. Establishing a food web model for coastal Antarctic benthic communities: a case study from the Vestfold Hills, Marine Ecology Progress Series, Vol. 478: 27 – 41.

Droits

Les chercheurs doivent respecter la déclaration de droits suivante:

L’éditeur et détenteur des droits de cette ressource est Australian Antarctic Data Centre. Ce travail est sous licence Creative Commons Attribution (CC-BY) 4.0.

Enregistrement GBIF

Cette ressource a été enregistrée sur le portail GBIF, et possède lUUID GBIF suivante : 2a2bf4d1-5747-4c03-ae7b-328a7768345b. Australian Antarctic Data Centre publie cette ressource, et est enregistré dans le GBIF comme éditeur de données avec lapprobation du Atlas of Living Australia.

Mots-clé

Occurrence EARTH SCIENCE > BIOSPHERE > ECOSYSTEMS > MARINE ECOSYSTEMS > BENTHIC EARTH SCIENCE > OCEANS > MARINE SEDIMENTS EARTH SCIENCE > OCEANS > OCEAN CHEMISTRY > STABLE ISOTOPES EARTH SCIENCE > BIOLOGICAL CLASSIFICATION > ANIMALS/INVERTEBRATES EARTH SCIENCE > BIOLOGICAL CLASSIFICATION > ANIMALS/INVERTEBRATES > ARTHROPODS > CRUSTACEANS EARTH SCIENCE > BIOLOGICAL CLASSIFICATION > ANIMALS/INVERTEBRATES > MOLLUSKS > BIVALVES EARTH SCIENCE > BIOLOGICAL CLASSIFICATION > ANIMALS/INVERTEBRATES > ARTHROPODS > CRUSTACEANS EARTH SCIENCE > BIOLOGICAL CLASSIFICATION > ANIMALS/INVERTEBRATES > ECHINODERMS EARTH SCIENCE > BIOLOGICAL CLASSIFICATION > ANIMALS/VERTEBRATES > FISH EARTH SCIENCE > BIOLOGICAL CLASSIFICATION > ANIMALS/INVERTEBRATES > MOLLUSKS > GASTROPODS EARTH SCIENCE > BIOLOGICAL CLASSIFICATION > ANIMALS/INVERTEBRATES > ARTHROPODS > CRUSTACEANS EARTH SCIENCE > BIOLOGICAL CLASSIFICATION > PLANTS > MACROALGAE (SEAWEEDS) EARTH SCIENCE > BIOLOGICAL CLASSIFICATION > PLANTS > MICROALGAE EARTH SCIENCE > BIOLOGICAL CLASSIFICATION > PROTISTS > PLANKTON > PHYTOPLANKTON EARTH SCIENCE > BIOSPHERE > ECOSYSTEMS > AQUATIC ECOSYSTEMS > PLANKTON EARTH SCIENCE > CRYOSPHERE > SEA ICE EARTH SCIENCE > OCEANS > SEA ICE; Occurrence

Données externes

Les données de la ressource sont disponibles dans dautres formats

Point of truth metadata record	https://data.aad.gov.au/metadata/records/AAS_3217_Davis_STP_StableIsotopes ASCII DIF 9.9

Contacts

Chris Gillies

Créateur ●
Personne De Contact

Investigator

Earthwatch Australia

126 Bank St., South Melbourne

Melbourne

VIC

cgillies@earthwatch.org.au

DATA OFFICER AADC

Fournisseur Des Métadonnées ●
Personne De Contact

DATA CENTER CONTACT

Australia Antarctic Division

203 Channel Highway

7050 Kingston

Tasmania

metadata@aad.gov.au

+61 3 6232 3244

https://data.aad.gov.au/

Jonny Stark

Personne De Contact

Investigator

Australia Antarctic Division

203 Channel Highway

7050 Hobart

Tasmania

Jonny.Stark@aad.gov.au

http://www.antarctica.gov.au/

Glenn Johnstone

Personne De Contact

Investigator

Southern Cross University

NSW

Datta Officer AADC

Distributeur

Metadata provider

Australia Antarctic Division

203 Channel Highway

7050 Hobart

Tasmania

metadata@aad.gov.au

https://data.aad.gov.au/

Couverture géographique

OCEAN, SOUTHERN OCEAN, ANTARCTIC, POLAR,

Enveloppe géographique	Sud Ouest [-68,919, 77,706], Nord Est [-68,355, 78,959]

Couverture taxonomique

Stable isotopes analysis was conducted in marine sediments and invertebrates.

Phylum	Plantae, Porifera
Class	Asteroidea, Hydrozoa, Demospongiae, Pycnogonida
Order	Nudibranchia
Family	Arcturidae, Nephtyidae, Polynoidae, Terrebellidae
Genus	Chaetomorpha, Gymnogongrus, Tryopheosella, Ascidia, Pyrosoma, Diplasterias, Cucumaria, Holothuria, Staurocucumi, Tanais
Species	Himantothallus grandifolius, Iridaea cordata, Monostroma, Palmaria decipiens, Heterophoxus videns, Orchomenella franklini, Paramoera walkeri, Waldeckia obesa, Urticinopsis antarctica, Actinia, Isotealia antarctica, Urticinopsis antarctica, Acodontaster hodgsoni, Odontaster validus, Adamussium colbecki, Laternula elliptica, Sterechinus neumayeri, Chionodraco hamatus, Trematomus bernacchii, Pagothenia borchgrevinki, Neobuccinum eatoni, Amauropsis rossiana, Trophon longstaffi, Cymodocella tubicauda, Glyptonotus antarcticus, Parborlasia corrugatus, Austrodoris kerguelenensi, Marseniopsis mollis, Ophiosparte gigas, Perkinsiana antarctica, Flabelligera mundata, Nymphon australe

Couverture temporelle

Date de début / Date de fin	2009-12-01 / 2010-03-01

Méthodes déchantillonnage

We sampled several benthic macroalgae, in addition to pelagic particulate organic matter (POM),sediment POM, sea ice POM, and consumers from several different locations occupying the shallow, nearshore zone (0 to 30 m) around the Vestfold Hills, in the summer season from December 2009 to March 2010. Samples were collected from 20 sites visited once over the 4 mo sampling period. Consumers were collected as close to their potential food sources as recommended by Gillies et al. (2012a), with the exception of sea ice algae which was sampled prior to winter sea ice break out (midDecember) with sampling sites chosen to represent a mixture of nearshore and offshore locations. All sampling sites were within a 5 km radial distance of Davis Station, although we were careful not to sample within 500 m of the sewerage outfall to avoid potential contamination of isotope values. We aimed to collect many species across a range of feeding guilds in order to describe carbon flows and trophic pathways amongst the general benthic community.

Etendue de létude	The Vestfold Hills lie at 68°35’S, 77°58’E in Prydz Bay, Princess Elizabeth Land. The area is bound by the Sorsdal Glacier in the south and the Antarctic Plateau 24 km to the north. The region is surrounded by low-lying rocky hills, indented by 3 large fjords and several smaller bays and inlets. A number of small, rocky islands lie in close proximity to the coast. The area supports a rich benthic community (Tucker & Burton 1987), comparable with that of similar habitats from other parts of Antarctica (Tucker & Burton 1988). Winter sea ice breaks out in late spring (November to December), with the area relatively ice free from January to March. The Windmill Islands are located at 66°17’S, 110°31’E in Wilkes Land (1000 km east of the Vestfold Hills) in close proximity to the Vanderford Glacier. Spanning an area of 30 km along the coastline, the region is characterised by 50 islands, with 5 main peninsulas jutting out from the Antarctic Plateau. The peninsulas comprise low rocky hills with intervening snow-covered valleys and meet the water’s edge with a mix of low ice edges and rocky shores. In general, patches of bedrock and boulders occur at shallow depths near the shore, with the substrate sloping down to finer grades of sediment. The benthic fauna is comparable to other nearshore locations within Antarctica (Johnston et al. 2007). Winter seaice breaks out sporadically over the summer months (December to February), leaving a mosaic of ice-free and ice-covered areas during the summer period.
Contrôle qualité	The original datasheet was reformatted to fit GBIF/ IPT Biodiversity.AQ standard. The new datasheet "DavisStationStableIsotopes.csv" provides the dataset ID, event ID, recordNumber, occurrenceID, eventDate, decimalLatitude, decimalLongitude, continent, occurrenceStatus, basisOfRecord. The taxonomical organisation is provided to the lowest taxonomical rank that could be determined, after matched in WoRMS (World Register of Marine Species).

Etendue de létude

The Vestfold Hills lie at 68°35’S, 77°58’E in Prydz Bay, Princess Elizabeth Land. The area is bound by the Sorsdal Glacier in the south and the Antarctic Plateau 24 km to the north. The region is surrounded by low-lying rocky hills, indented by 3 large fjords and several smaller bays and inlets. A number of small, rocky islands lie in close proximity to the coast. The area supports a rich benthic community (Tucker & Burton 1987), comparable with that of similar habitats from other parts of Antarctica (Tucker & Burton 1988). Winter sea ice breaks out in late spring (November to December), with the area relatively ice free from January to March. The Windmill Islands are located at 66°17’S, 110°31’E in Wilkes Land (1000 km east of the Vestfold Hills) in close proximity to the Vanderford Glacier. Spanning an area of 30 km along the coastline, the region is characterised by 50 islands, with 5 main peninsulas jutting out from the Antarctic Plateau. The peninsulas comprise low rocky hills with intervening snow-covered valleys and meet the water’s edge with a mix of low ice edges and rocky shores. In general, patches of bedrock and boulders occur at shallow depths near the shore, with the substrate sloping down to finer grades of sediment. The benthic fauna is comparable to other nearshore locations within Antarctica (Johnston et al. 2007). Winter seaice breaks out sporadically over the summer months (December to February), leaving a mosaic of ice-free and ice-covered areas during the summer period.

Contrôle qualité

The original datasheet was reformatted to fit GBIF/ IPT Biodiversity.AQ standard. The new datasheet "DavisStationStableIsotopes.csv" provides the dataset ID, event ID, recordNumber, occurrenceID, eventDate, decimalLatitude, decimalLongitude, continent, occurrenceStatus, basisOfRecord. The taxonomical organisation is provided to the lowest taxonomical rank that could be determined, after matched in WoRMS (World Register of Marine Species).

Description des étapes de la méthode:

Sediment POM samples were collected by divers throughout the sampling period at depths of 6 to 30 m by coring (5 cm diameter by 10 cm long) and utilising only the top 1.5 cm section of the core

Métadonnées additionnelles

Identifiants alternatifs	2a2bf4d1-5747-4c03-ae7b-328a7768345b
	https://data.aad.gov.au/ipt/resource?r=david_station_stable_isotopes