Chemical composition of Holocene sediment core M40/4_SL71 from the Eastern Mediterranean Sea
Cobertura |
LATITUDE: 34.811160 * LONGITUDE: 23.194160 * DATE/TIME START: 1998-01-25T07:12:00 * DATE/TIME END: 1998-01-25T07:12:00 * MINIMUM DEPTH, sediment/rock: 0.12 m * MAXIMUM DEPTH, sediment/rock: 4.18 m |
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Data(s) |
11/03/2015
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Formato |
text/tab-separated-values, 398 data points |
Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.843934 doi:10.1594/PANGAEA.843934 |
Idioma(s) |
en |
Publicador |
PANGAEA |
Relação |
doi:10.1594/PANGAEA.758621 Möbius, Jürgen (2013): Isotope fractionation during nitrogen remineralization (ammonification): Implications for nitrogen isotope biogeochemistry. Geochimica et Cosmochimica Acta, 105, 422-432, doi:10.1016/j.gca.2012.11.048 Möbius, Jürgen; Lahajnar, Niko; Emeis, Kay-Christian (2010): Diagenetic control of nitrogen isotope ratios in Holocene sapropels and recent sediments from the Eastern Mediterranean Sea. Biogeosciences, 7, 3901-3914, doi:10.5194/bg-7-3901-2010 |
Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
Palavras-Chave | #Amino acid, total hydrolysable; Amino acid analyser, Biochrom 30; Amino acids/hexosamines ratio; Calcium carbonate; Carbon, inorganic, total; Carbon, organic, total; Carbon, total; Degradation index of amino acids (Dauwe et al., 1999); delta 15N; DEPTH, sediment/rock; Element analyser CNS, Carlo Erba NA1500; Gravity corer (Kiel type); Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; M40/4; M40/4_SL71; Mass spectrometer Finnigan MAT 252; Meteor (1986); Nitrogen, total; Opal, biogenic silica; Reactivity index of amino acids (Jennerjahn & Ittekkot, 1997); SL |
Tipo |
Dataset |