Modulation of potassium channel function by methionine oxidation and reduction

Oxidation of amino acid residues in proteins can be caused by a variety of oxidizing agents normally produced by cells. The oxidation of methionine in proteins to methionine sulfoxide is implicated in aging as well as in pathological conditions, and it is a reversible reaction mediated by a ubiquitous enzyme, peptide methionine sulfoxide reductase. The reversibility of methionine oxidation suggests that it could act as a cellular regulatory mechanism although no such in vivo activity has been demonstrated. We show here that oxidation of a methionine residue in a voltage-dependent potassium channel modulates its inactivation. When this methionine residue is oxidized to methionine sulfoxide, the inactivation is disrupted, and it is reversed by coexpression with peptide methionine sulfoxide reductase. The results suggest that oxidation and reduction of methionine could play a dynamic role in the cellular signal transduction process in a variety of systems.

Methionine residues as endogenous antioxidants in proteins

Cysteine and methionine are the two sulfur-containing residues normally found in proteins. Cysteine residues function in the catalytic cycle of many enzymes, and they can form disulfide bonds that contribute to protein structure. In contrast, the specific functions of methionine residues are not known. We propose that methionine residues constitute an important antioxidant defense mechanism. A variety of oxidants react readily with methionine to form methionine sulfoxide, and surface exposed methionine residues create an extremely high concentration of reactant, available as an efficient oxidant scavenger. Reduction back to methionine by methionine sulfoxide reductases would allow the antioxidant system to function catalytically. The effect of hydrogen peroxide exposure upon glutamine synthetase from Escherichia coli was studied as an in vitro model system. Eight of the 16 methionine residues could be oxidized with little effect on catalytic activity of the enzyme. The oxidizable methionine residues were found to be relatively surface exposed, whereas the intact residues were generally buried within the core of the protein. Furthermore, the susceptible residues were physically arranged in an array that guarded the entrance to the active site.

Cystine-mediated oxidative defence in Lactobacillus reuteri BR11

Lactobacillus reuteri BR11 possesses an abundant cystine uptake (Cyu) ABC-transporter that was previously found to be involved in a novel mechanism of oxidative defence mediated by cystine. The current study aimed to elucidate this mechanism with a focus on the role of the co-transcribed cystathionine ã-lyase (Cgl). Growth studies of wild-type L. reuteri BR11 and mutants inactivated in cgl and the cystine-binding protein encoding gene cyuC showed that in contrast to the Cyu transporter, whose inactivation led to growth arrest in aerated cultures, Cgl is not crucial for oxidative defence. However, the role of Cgl in oxidative defence became apparent in the presence of severe oxidative damage and cysteine deprivation. Cysteine was found to be protective against oxidative stress, and the action of Cgl in both cysteine biosynthesis and degradation poses a seemingly futile pathway that deprives the intracellular cysteine pool. To further characterise the relationship between Cgl activity and cysteine and their roles in oxidative defence, enzymatic assays were performed on purified Cgl, and intracellular concentrations of cysteine, cystathionine and methionine were determined. Cgl was highly active towards cystine and cystathionine and less active towards cysteine in vitro, suggesting the main function of Cgl to be cysteine biosynthesis. Cysteine was found at high concentrations in the cell, but the levels were not significantly affected by inactivation of cgl or growth under aerobic conditions. It was concluded that both anabolic and catabolic activities of Cgl towards cysteine contribute to oxidative defence, the former by maintaining an intracellular reservoir of thiol analogous to glutathione, and the latter by producing H2S which is readily secreted, thus creating a reducing extracellular environment. The significance of the Cyu transporter to the physiology of L. reuteri BR11 prompted a phylogenetic study to determine its presence in bacteria. Orthologs of the Cyu transporter that are closest matches to the Cyu transporter are only limited to several species of Lactobacillus and Leuconostoc. Outside the Lactobacillales order, the closest matching orthologs belong to Proteobacteria, and there are more orthologs in Proteobacteria than non-Lactobacillales Firmicutes, suggesting that the Cyu transporter locus was present in the ancestor of the Proteobacteria and Firmicutes, and over evolutionary time has been lost or diverged in many Firmicutes. The clustering of the Cyu transporter locus with a gene encoding a Cgl family protein is even rarer. It was only found in L. reuteri, Lactobacillus vaginalis, Weissella paramesenteroides, the Lactobacillus casei group, and several Campylobacter sp. An accompanying phylogenetic study of L. reuteri BR11 using multi-locus sequence analysis showed that L. reuteri BR11 had diverged from more than 100 strains of L. reuteri isolated from various hosts and geographical locations. However, comparison with other Lactobacillus species supported the current classification of BR11 as L. reuteri. The most closely related species to L. reuteri is L. vaginalis or Lactobacillus antri, depending on the housekeeping gene used for analysis. The close evolutionary relationship of L. vaginalis to L. reuteri and the high degree of sequence identity between the cgl-cyuABC loci in both species suggest that the Cyu system is highly likely to perform similar functions in L. vaginalis. In search of other genes that function in oxidative defence, a number of mutants which were inactivated in genes that confer increased resistance to oxidative stress in other bacteria were constructed. The genes targeted were ahpC (peroxidase component of the alkyl hydroperoxide reductase system), tpx (thiol peroxidase), osmC (osmotically induced protein C), mntH (Mn2+/Fe2+ transporter), gshA (ã-glutamylcysteine synthetase) and msrA (methionine sulfoxide reductase). The ahpC and mntH mutants had slightly lower minimum inhibitory concentrations of organic peroxides, suggesting these genes might be involved in resistance to organic peroxides in L. reuteri. However, none of the mutants exhibited growth defects in aerated cultures, in stark contrast to the cyuC mutant. This may be due to compensatory functions of other genes, a hypothesis which cannot be tested until a robust protocol for constructing markerless multiple gene deletion mutants in L. reuteri is developed. These results highlight the importance of the Cyu transporter in oxidative defence and provide a foundation for extending the research of this system in other bacteria.

果实对酵母拮抗菌和外源水杨酸诱导的抗病性应答机理

用生物和非生物因子来进行采后病害的防治，是一个非常有效的方法。诱导抗性作为控制果蔬采后病害的生物技术，已成为该领域的一个研究热点。然而诱导抗性的机制非常复杂，涉及到寄主、病原菌、激发子之间的相互作用关系。本研究主要利用酵母拮抗菌Pichia membranefaciens和SA处理果实，观察其抗性诱导表达和对采后青霉病菌（Penicillium expansum）的抑制作用，并从蛋白质组学水平上对诱导抗性的机理进行了分析。研究结果表明： 1、酵母拮抗菌P. membranefaciens (5 × 107 cells·ml-1)和SA(0.5 mM)处理采后甜樱桃果实，能够明显地降低病害的发病率和病斑直径。酵母菌和SA处理影响到了果实抗氧化酶的活性，同时还改变了POD同工酶谱和甜樱桃果实的总蛋白含量，并诱导了新的蛋白质条带产生。用光学显微镜和扫描电子显微镜技术观察发现，在in vitro条件下P. membranefaciens能够紧密地结合与病原菌的菌丝，而在in vivo条件下这种结合较为松散。 2、借鉴其它模式植物的方法，我们建立了一整套适用于多汁类植物材料的蛋白质组学研究方法。对于芒果，桃，甜樱桃、苹果以及冬枣等果实，都取得了重复性非常好的2-D图谱。我们应用该技术进一步研究了P. membranefaciens (1 × 108 cells·ml-1)以及SA (0.5 mM)处理对桃果实蛋白质组的诱导影响。结果显示，两种激发子处理都能够诱导桃果实产生抗性，从而减轻青霉病引起的腐烂。在诱导处理1 d以后，酵母拮抗菌和SA分别诱导22和16个蛋白的差异表达。质谱鉴定的蛋白属于6大类：代谢，防御反应，转录，能量途径以及细胞结构。有6个蛋白受到两种激发子的共同调控。其中，4种蛋白(包括glutathione peroxidase, polyphenol oxidase precursor, catalase和methionine sulfoxide reductase) 属于抗氧化蛋白，涉及到活性氧代谢。另2个蛋白（Major allergen Pru av 1和peroxidase）是病程相关蛋白，直接参与植物的防御反应。同时一些磷酸化酶和转录因子也受到两种激发子的调节从而参与果实的抗病反应。酶学测定和Northern杂交的结果表明，拮抗菌与SA处理均能影响过氧化氢酶活性及其基因的表达。 3、采前用较高浓度SA (2 mM) 短时间（10s）处理不同成熟期的甜樱桃果实，能够明显降低果实青霉病的病斑直径，并能减轻较低成熟度果实的发病率。在没有接菌的情况下，SA诱导了33个差异表达的蛋白，其中用质谱鉴定出了26个。而在接种病原菌的情况下，SA诱导了19个差异表达的蛋白，并鉴定出了其中的12个。这些蛋白分别涉及到代谢、防御反应、转录、能量途径、信号转导等过程。在没有接种病原菌的情况下，SA处理诱导了Putative DnaJ heat shock protein, PR1-like protein, Peroxidase, Major allergen Pru av 1 (Pru a 1)和Catalase等与抗病有关的蛋白。而在接种病原菌的情况下，诱导了PR1-like protein, Peroxidase和Catalase蛋白的差异表达。通过酶活性测定以及对细胞学定位的研究，我们发现在没有接种病原菌的情况下，POD的活性受到SA的诱导。但是在接种病原菌以后，诱导效果不明显。

Competition between humic substances and α-amino acids by metal species

The aim of the present work was to carry out experimental comparison between humic substances (HS) and representative α-amino acids (methionine, methionine sulfoxide and cysteine hydrochloride) in relation to the complexation of biologically active trace elements (Al, Cu, Pb, Mn, Zn, Cd and Ni). A mobile time-controlled tangential-flow UF technique was applied to differentiate between HS-metal and α-aminoacids-metal complexes. Metal determinations were conventionally carried out using a ICP-OES. The results showed that HS may be considered as a selective complexing agents with higher metal bonding capability in relation to Al, Cu and Pb, the fact that may be clinically important.

The Carmaphycins: New Proteasome Inhibitors Exhibiting an alpha,beta-Epoxyketone Warhead from a Marine Cyanobacterium

Two new peptidic proteasome inhibitors were isolated as trace components from a Curacao collection of the marine cyanobacterium Symploca sp. Carmaphycin A (1) and carmaphycin B (2) feature a leucine-derived a,beta-epoxyketone warhead directly connected to either methionine sulfoxide or methionine sulfone. Their structures were elucidated on the basis of extensive NMR and MS analyses and confirmed by total synthesis, which in turn provided more material for further biological evaluations. Pure carmaphycins A and B were found to inhibit the beta 5 subunit (chymotrypsin-like activity) of the S. cerevisiae 20S proteasome in the low nanomolar range. Additionally, they exhibited strong cytotoxicity to lung and colon cancer cell lines, as well as exquisite antiproliferative effects in the NCI60 cell-line panel. These assay results as well as initial structural biology studies suggest a distinctive binding mode for these new inhibitors.

Evolutionäre Veränderungen in der Nutzung redox-aktiver Aminosäuren und ihre Ursachen

Gewebe, Zellen und speziell Zellkompartimente unterscheiden sich in ihrer Sauerstoffkonzentration, Stoffwechselrate und in der Konzentration an gebildeten reaktiven Sauerstoffspezies. Um eine mögliche Änderung in der Aminosäurennutzung durch den Einfluss von Sauerstoff und seinen reaktiven Spezies untersuchen zu können wurden, Bereiche bzw. Kompartimente der menschlichen Zelle definiert, die einen Referenzrahmen bildeten und bekannt dafür sind, einen relativ hohen Grad an reaktiven Sauerstoffspezies aufzuweisen. Aus dem Vergleich wurde deutlich, dass vor allem die beiden redox-aktiven und schwefeltragenden Aminosäuren Cystein und Methionin durch eine besondere Verteilung und Nutzung charakterisiert sind. Cystein ist hierbei diejenige Aminosäure mit den deutlichsten Änderungen in den fünf untersuchten Modellen der oxidativen Belastung. In all diesen Modellen war die Nutzung von Cystein deutlich reduziert, wohingegen Methionin in Proteinen des Mitochondriums und der Elektronentransportkette angereichert war. Dieser auf den ersten Blick paradoxe Unterschied zwischen Cystein und Methionin wurde näher untersucht, indem die differenzierte Methioninnutzung in verschiedenen Zellkompartimenten von Homo sapiens charakterisiert wurde.rnDie sehr leicht zu oxidierende Aminosäure Methionin zeigt ein ungewöhnliches Verteilungsmuster in ihrer Nutzungshäufigkeit. Entgegen mancher Erwartung wird Methionin in zellulären Bereichen hoher oxidativer Belastung und starker Radikalproduktion intensiv verwendet. Dieses Verteilungsmuster findet man sowohl im intrazellulären Vergleich, als auch im Vergleich verschiedener Spezies untereinander, was daraufhin deutet, dass es einen lokalen Bedarf an redox-aktiven Aminosäuren gibt, der einen sehr starken Effekt auf die Nutzungshäufigkeit von Methionin ausübt. Eine hohe Stoffwechselrate, die im Allgemeinen mit einer erhöhten Produktion von Oxidantien assoziiert wird, scheint ein maßgeblicher Faktor der Akkumulation von Methionin in Proteinen der Atmungskette zu sein. Die Notwendigkeit, oxidiertes Antioxidans wieder zu reduzieren, findet auch bei Methionin Anwendung, denn zu Methioninsulfoxid oxidiertes Methionin wird durch die Methioninsulfoxidreduktase wieder zu Methionin reduziert. Daher kann die spezifische Akkumulation von Methionin in Proteinen, die verstärkt reaktiven Sauerstoffspezies ausgesetzt sind, als eine systematische Strategie angesehen werden, um andere labile Strukturen vor ungewollter Oxidation zu schützen. rnDa Cystein in allen untersuchten Modellen der oxidativen Belastung und im Besonderen in Membranproteinen der inneren Mitochondrienmembran lebensspannenabhängig depletiert war, wurde dieses Merkmal näher untersucht. Deshalb wurde die Hypothese getestet, ob ein besonderer Redox-Mechanismus der Thiolfunktion für diese selektive Depletion einer im Allgemeinen als harmlos oder antioxidativ geltenden Aminosäure verantwortlich ist. Um den Effekt von Cysteinresten in Membranen nachzustellen, wurden primäre humane Lungenfibroblasten (IMR90) mit diversen Modellsubstanzen behandelt. Geringe Konzentrationen der lipophilen Substanz Dodecanthiol verursachten eine signifikante Toxizität in IMR90-Zellen, die von einer schnellen Zunahme an polyubiquitinierten Proteinen und anderen Indikatoren des proteotoxischen Stresses, wie Sequestosom 1 (P62), HSP70 und HSP90 begleitet wurde. Dieser Effekt konnte spezifisch der Chemie der Thiolfunktion in Membranen zugeordnet werden, da Dodecanol (DOH), Dodecylmethylsulfid (DMS), Butanthiol oder wasserlösliche Thiole weder eine cytotoxische Wirkung noch eine Polyubiquitinierung von Proteinen verursachten. Die Ergebnisse stimmen mit der Hypothese überein, dass Thiole innerhalb von biologischen Membranen als radikalische Kettentransferagentien wirken. Diese Eigenschaft wird in der Polymerchemie durch Nutzung von lipophilen Thiolen in hydrophoben Milieus technisch für die Produktion von Polymeren benutzt. Da die Thiylradikal-spezifische Reaktion von cis-Fettsäuren zu trans-Fettsäuren in 12SH behandelten Zellen verstärkt ablief, kann gefolgert werden, dass 12SH zellulär radikalisiert wurde. In lebenden Organismen kann demnach die Oxidation von Cystein die Schädigung von Membranen beschleunigen und damit Einfallstore für die laterale Radikalisierung von integralen Membranproteinen schaffen, welche möglicherweise der Langlebigkeit abträglich ist, zumindest, wenn sie in der inneren Mitochondrienmembran auftritt.

Macrocyclic chelator-coupled gastrin-based radiopharmaceuticals for targeting of gastrin receptor-expressing tumours

PURPOSE: Diethylenetriamine-pentaacetic acid (DTPA)-coupled minigastrins are unsuitable for therapeutic application with the available beta-emitting radiometals due to low complex stability. Low tumour-to-kidney ratio of the known radiopharmaceuticals is further limiting their potency. We used macrocyclic chelators for coupling to increase complex stability, modified the peptide sequence to enhance radiolytic stability and studied tumour-to-kidney ratio and metabolic stability using (111)In-labelled derivatives. METHODS: Gastrin derivatives with decreasing numbers of glutamic acids were synthesised using (111)In as surrogate for therapeutic radiometals for in vitro and in vivo studies. Gastrin receptor affinities of the (nat)In-metallated compounds were determined by receptor autoradiography using (125)I-CCK as radioligand. Internalisation was evaluated in AR4-2J cells. Enzymatic stability was determined by incubating the (111)In-labelled peptides in human serum. Biodistribution was performed in AR4-2J-bearing Lewis rats. RESULTS: IC(50) values of the (nat)In-metallated gastrin derivatives vary between 1.2 and 4.8 nmol/L for all methionine-containing derivatives. Replacement of methionine by norleucine, isoleucine, methionine-sulfoxide and methionine-sulfone resulted in significant decrease of receptor affinity (IC(50) between 9.9 and 1,195 nmol/L). All cholecystokinin receptor affinities were >100 nmol/L. All (111)In-labelled radiopeptides showed receptor-specific internalisation. Serum mean-life times varied between 2.0 and 72.6 h, positively correlating with the number of Glu residues. All (111)In-labelled macrocyclic chelator conjugates showed higher tumour-to-kidney ratios after 24 h (0.37-0.99) compared to (111)In-DTPA-minigastrin 0 (0.05). Tumour wash out between 4 and 24 h was low. Imaging studies confirmed receptor-specific blocking of the tumour uptake. CONCLUSIONS: Reducing the number of glutamates increased tumour-to-kidney ratio but resulted in lower metabolic stability. The properties of the macrocyclic chelator-bearing derivatives make them potentially suitable for clinical purposes.

Oxidative Stress in Hypobaric Hypoxia and Influence on Vessel-Tone Modifying Mediators

Increased pulmonary artery pressure is a well-known phenomenon of hypoxia and is seen in patients with chronic pulmonary diseases, and also in mountaineers on high altitude expedition. Different mediators are known to regulate pulmonary artery vessel tone. However, exact mechanisms are not fully understood and a multimodal process consisting of a whole panel of mediators is supposed to cause pulmonary artery vasoconstriction. We hypothesized that increased hypoxemia is associated with an increase in vasoconstrictive mediators and decrease of vasodilatators leading to a vasoconstrictive net effect. Furthermore, we suggested oxidative stress being partly involved in changement of these parameters. Oxygen saturation (Sao2) and clinical parameters were assessed in 34 volunteers before and during a Swiss research expedition to Mount Muztagh Ata (7549 m) in Western China. Blood samples were taken at four different sites up to an altitude of 6865 m. A mass spectrometry-based targeted metabolomic platform was used to detect multiple parameters, and revealed functional impairment of enzymes that require oxidation-sensitive cofactors. Specifically, the tetrahydrobiopterin (BH4)-dependent enzyme nitric oxide synthase (NOS) showed significantly lower activities (citrulline-to-arginine ratio decreased from baseline median 0.21 to 0.14 at 6265 m), indicating lower NO availability resulting in less vasodilatative activity. Correspondingly, an increase in systemic oxidative stress was found with a significant increase of the percentage of methionine sulfoxide from a median 6% under normoxic condition to a median level of 30% (p<0.001) in camp 1 at 5533 m. Furthermore, significant increase in vasoconstrictive mediators (e.g., tryptophan, serotonin, and peroxidation-sensitive lipids) were found. During ascent up to 6865 m, significant altitude-dependent changes in multiple vessel-tone modifying mediators with excess in vasoconstrictive metabolites could be demonstrated. These changes, as well as highly significant increase in systemic oxidative stress, may be predictive for increase in acute mountain sickness score and changes in Sao2.

Chemical and amino acid compositions of bottom sediments from the Canary upwelling

Amino acid composition of bottom sediments on the northwestern continental slope of Africa is determined. Correlation similar to that found earlier in Caspian sediments between type of amino acid spectra of Atlantic sediments and distribution of reduced forms of sulfur in them is found. These correlations result from geochemical activity of benthic biocoenosis, which transforms sulfur compounds.

Geochemical analysis of sediments and interstitial water in sediment cores from the North-West African continental margin and from the Central Pacific

A. Continental slope sediments off Spanish-Sahara and Senegal contain up to 4% organic carbon and up to 0.4% total nitrogen. The highest concentrations were found in sediments from water depths between 1000 and 2000 m. The regional and vertical distribution of organic matter differs significantly. Off Spanish-Sahara the organic matter content of sediment deposited during glacial times (Wuerm, Late Riss) is high whereas sediments deposited during interglacial times (Recent, Eem) are low in organic matter. Opposite distribution was found in sediments off Senegal. The sediments contain 30 to 130 ppm of fixed nitrogen. In most sediments this corresponds to 2-8 % of the total nitrogen. Only in sediments deposited during interglacial times off Spanish-Sahara up to 20 % of the total nitrogen is contained as inorganically bound nitrogen. Positive correlations of the fixed nitrogen concentrations to the amounts of clay, alumina, and potassium suggest that it is primarily fixed to illites. The amino acid nitrogen and hexosamine nitrogen account for 17 to 26 % and 1.3 to 2.4 %, respectively of the total nitrogen content of the sediments. The concentrations vary between 200 and 850 ppm amino acid nitrogen and 20 to 70 ppm hexosamine nitrogen, both parallel the fluctiations of organic matter in the sediment. Fulvic acids, humic acids, and the total organic matter of the sediments may be clearly differentiated from one another and their amino acid and hexosamine contents and their amino acid composition: a) Fulvic acids contain only half as much amino acids as humic acids b) The molar amino acid/hexosamine ratios of the fulvic acids are half those of the humic acids and the total organic matter of the sediment c) The amino acid spectra of fulvic acids are characterized by an enrichment of aspartic acid, alanine, and methionine sulfoxide and a depletion of glycine, valine, isoleucine, leucine, tyrosine, phenylalanine, lysine, and arginine compared to the spectra of the humic acids and those of the total organic matter fraction of the sediment. d) The amino acid spectra of the humic acids and those of the total organic matter fraction of the sediments are about the same with the exception that arginine is clearly enriched in the total organic matter. In general, as indicated by the amino compounds humic acids resemble closer the total organic matter composition than the low molecular fulvic acids do. This supports the general idea that during the course of diagenesis in reducing sediments organic matter stabilizes from a fulvic-like structure to humic-like structure and finally to kerogen. The decomposition rates of single aminio acids differ significantly from one another. Generally amino acids which are preferentially contained in humic acids and the total organic matter fraction show a smaller loss with time than those preferably well documented in case of the basic amino acids lysine and arginine which- although thermally unstable- are the most stable amino acids in the sediments. A favoured incorporation of these compounds into high molecular substances as well as into clay minerals may explain their relatively high "stability" in the sediment. The nitrogen loss from the sediments due to the activity of sulphate-reducing bacteria amounts to 20-40 % of the total organic nitrogen now present. At least 40 % of the organic nitrogen which is liberated by sulphate-reducing bacteria can be explained ny decomposition of amino acids alone. B. Deep-sea sediments from the Central Pacific The deep-seas sediments contain 1 to 2 orders of magnitude less organic matter than the continental slope sediments off NW Africa, i.e. 0.04 to 0.3 % organic carbon. The fixed nitrogen content of the deep-sea sediments ranges from 60 to 270 ppm or from 20 to 45 % of the total nitrogen content. While ammonia is the prevailing inorganic nitrogen compound in anoxic pore waters, nitrate predominates in the oxic environment of the deep-sea sediments. Near the sediment/water interface interstital nitrate concentrations of around 30 µg-at. N/l were recorded. These generally increase with sediment depth by 10 to 15 µg-at. NO3- N/l. This suggests the presence of free oxygen and the activity of nitrifying bacteria in the interstitial waters. The ammonia content of the interstitial water of the oxic deep-sea sediments ranges from 2 to 60 µg-at. N/l and thus is several orders of magnitude less than in anoxic sediments. In contrast to recorded nitrate gradients towards the sediments/water interface, there are no ammonia concentration gradients. However, ammonia concentrations appear to be characteristic for certain regional areas. It is suggested that this regional differentiation is caused by ion exchange reactions involving potassium and ammonium ions rather than by different decomposition rates of organic matter. C. C/N ratios All estimated C/N ratios of surface sediments vary between 3 and 9 in the deep-sea and the continental margin, respectively. Whereas the C/N ratios generally increase with depth in the sediment cores off NW Africa they decrease in the deep-sea cores. The lowest values of around 1.3 were found in the deeper sections of the deep-sea cores, the highest of around 10 in the sediments off NW Africa. The wide range of the C/N ratios as well as their opposite behaviour with increasing sediment depth in both the deep-sea and continental margin sediment cores, can be attributed mainly to the combination of the following three factors: 1. Inorganic and organic substances bound within the latticed of clay minerals tend to decrease the C/N ratios. 2. Organic matter not protected by absorption on the clay minerals tends to increase C/N ratios 3. Diagenetic alteration of organic matter by micro-organisms tends to increase C/N ratios through preferential loss of nitrogen The diagenetic changes of the microbially decomposable organic matter results in both oxic and anoxic environments in a preferential loss of nitrogen and hence in higher C/N ratios of the organic fraction. This holds true for most of the continental margin sediments off NW Africa which contain relatively high amounts of organic matter so that factors 2 and 3 predominate there. The relative low C/N ratios of the sediments deposited during interglacial times off Spanish-Sahara, which are low in organic carbon, show the increasing influence of factor 1 - the nitrogen-rich organic substances bound to clay minerals. In the deep-sea sediments from the Central Pacific this factor completely predominates so that the C/N rations of the sediments approach that of the substance absorbed to clay minerals with decreasing organic matter content. In the deeper core sections the unprotected organic matter has been completely destroyed so that the C/N ratios of the total sediments eventually fall into the same range as those of the pure clay mineral fraction.