Mediterranean cold-water coral measurements


Autoria(s): Titschack, Jürgen; Fink, Hiske G; Baum, Gunilla; Wienberg, Claudia; Hebbeln, Dierk; Freiwald, André
Cobertura

MEDIAN LATITUDE: 37.855498 * MEDIAN LONGITUDE: 11.941742 * SOUTH-BOUND LATITUDE: 35.434500 * WEST-BOUND LONGITUDE: -2.513833 * NORTH-BOUND LATITUDE: 39.557200 * EAST-BOUND LONGITUDE: 18.456000 * DATE/TIME START: 2006-10-01T21:44:00 * DATE/TIME END: 2009-06-06T15:27:00

Data(s)

27/10/2016

Resumo

This study presents aggradation rates supplemented for the first time by carbonate accumulation rates from Mediterranean cold-water coral sites considering three different regional and geomorphological settings: (i) a cold-water coral ridge (eastern Melilla coral province, Alboran Sea), (ii) a cold-water coral rubble talus deposit at the base of a submarine cliff (Urania Bank, Strait of Sicily) and (iii) a cold-water coral deposit rooted on a predefined topographic high overgrown by cold-water corals (Santa Maria di Leuca coral province, Ionian Sea). The mean aggradation rates of the respective cold-water coral deposits vary between 10 and 530 cm kyr?1 and the mean carbonate accumulation rates range between 8 and 396 g cm?2 kyr?1 with a maximum of 503 g cm?2 kyr?1 reached in the eastern Melilla coral province. Compared to other deep-water depositional environments the Mediterranean cold-water coral sites reveal significantly higher carbonate accumulation rates that were even in the range of the highest productive shallow-water Mediterranean carbonate factories (e.g. Cladocora caespitosa coral reefs). Focusing exclusively on cold-water coral occurrences, the carbonate accumulation rates of the Mediterranean cold-water coral sites are in the lower range of those obtained for the prolific Norwegian coral occurrences, but exhibit much higher rates than the cold-water coral mounds off Ireland. This study clearly indicates that cold-water corals have the potential to act as important carbonate factories and regional carbonate sinks within the Mediterranean Sea. Moreover, the data highlight the potential of cold-water corals to store carbonate with rates in the range of tropical shallow-water reefs. In order to evaluate the contribution of the cold-water coral carbonate factory to the regional or global carbonate/carbon cycle, an improved understanding of the temporal and spatial variability in aggradation and carbonate accumulation rates and areal estimates of the respective regions is needed.

Formato

application/zip, 18 datasets

Identificador

https://doi.pangaea.de/10.1594/PANGAEA.867277

Idioma(s)

en

Publicador

PANGAEA

Direitos

Access constraints: access rights needed

Fonte

Supplement to: Titschack, Jürgen; Fink, Hiske G; Baum, Gunilla; Wienberg, Claudia; Hebbeln, Dierk; Freiwald, André (2016): Mediterranean cold-water corals - an important regional carbonate factory? The Depositional Record, 2(1), 74-96, doi:10.1002/dep2.14

Palavras-Chave #Acc rate carb; Accumulation rate, carbonate; Age; AGE; Age, 14C AMS; Age, 14C calibrated, CALIB 6.0 and Marine09 (Reimer et al., 2009); Age, dated; Age, dated material; Age, dated standard error; Age, maximum/old; Age, minimum/young; Age dated; Age max; Age min; Age std e; Aggradation rate, max; Aggradation rate, mean; Aggradation rate, min; Aragonite; Arg; Backgr.-sed.-derived; Backgr.-sed.-derived carbonate [wt.%]; background-sediment-derived; bin 0: [0.00,5.00); bin 0: [-8.00,-7.69); bin 1: [5.00,10.00); bin 1: [-7.69,-7.38); bin 10: [-4.88,-4.56); bin 10: [50.00,55.00); bin 11: [-4.56,-4.25); bin 11: [55.00,60.00); bin 12: [-4.25,-3.94); bin 12: [60.00,65.00); bin 13: [-3.94,-3.63); bin 13: [65.00,70.00); bin 14: [-3.63,-3.31); bin 14: [70.00,75.00); bin 15: [-3.31,-3.00); bin 15: [75.00,80.00); bin 16: [-3.00,-2.69); bin 16: [80.00,85.00); bin 17: [-2.69,-2.38); bin 17: [85.00,90.00]; bin 18: [-2.38,-2.06); bin 19: [-2.06,-1.75); bin 2: [10.00,15.00); bin 2: [-7.38,-7.06); bin 20: [-1.75,-1.44); bin 21: [-1.44,-1.13); bin 22: [-1.13,-0.81); bin 23: [-0.81,-0.50); bin 24: [-0.50,-0.19); bin 25: [-0.19,0.13); bin 26: [0.13,0.44); bin 27: [0.44,0.75); bin 28: [0.75,1.06); bin 29: [1.06,1.38); bin 3: [15.00,20.00); bin 3: [-7.06,-6.75); bin 30: [1.38,1.69); bin 31: [1.69,2.00]; bin 4: [20.00,25.00); bin 4: [-6.75,-6.44); bin 5: [25.00,30.00); bin 5: [-6.44,-6.13); bin 6: [30.00,35.00); bin 6: [-6.13,-5.81); bin 7: [35.00,40.00); bin 7: [-5.81,-5.50); bin 8: [40.00,45.00); bin 8: [-5.50,-5.19); bin 9: [45.00,50.00); bin 9: [-5.19,-4.88); Calendar years; Calendar years, maximum/old; Calendar years, minimum/young; Cal yrs; Cal yrs max; Cal yrs min; Carb; Carbonates; Center for Marine Environmental Sciences; Clast angle distr; Clast angle distribution; Clay min; Clay minerals; Comment; Computer tomography (CT) Toshiba Aquilion 64; CWC-fact.-derived; CWC-fact.-derived carbonate [wt.%]; D50; Dated material; Depth; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Depth bot; Depth top; Dol; Dolomite; Event; factory-derived; Feldspar; Fraction; Fsp; GeoB; Geosciences, University of Bremen; Gp; Gypsum; Halite; Hbl; High magnesium calcite; Hl; HMC; Hornblende; Kurt; Kurtosis; Label; LMC; Location; Lower; Low magnesium calcite; MARUM; Max; Max, background-sediment-derived; Max, factory-derived; Mean; Mean, background-sediment-derived; Mean, factory-derived; Mean, grain size; Median; Median, grain size; Min; Min, background-sediment-derived; Min, factory-derived; Minerals, other; Min other; Mode; Mode, grain size; n; no. Labels; No slice; No voxels; Number; Number of slice; Number of voxels; Py; Pyrite, FeS2; Quartz; Qz; Sample code/label; Sedimentation rate; Sed rate; Size fraction; Skew; Skewness; Standard deviation; Std dev; Upper; X-ray diffraction (Philips X'Pert Pro)
Tipo

Dataset