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Sinninghe Damste JS
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Sinninghe Damste JS
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Constraints on the applicability of the organic temperature proxies U k' 37 , TE...
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A continental-weathering control on orbitally driven redox-nutrient cycling duri...
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The absence of intact polar lipid-derived GDGTs in marine waters dominated by Ma...
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Recognition of Early Eocene global carbon isotope excursions using lipids of mar...
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Arctic late Paleocene-early Eocene paleoenvironments with special emphasis on th...
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Early steroid sulfurisation in surface sediments of a permanebtly stratified lak...
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Recognition of Early Eocene global carbon isotope excursions using lipids of mar...
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Ocean temperature control on ice shelf and glacier extent around the Antarctic P...
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First evidence for the Cenomanian-Turonian oceanic anoxic event (OAE2, 'Bonarell...
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Pronounced subsurface cooling of North Atlantic waters off Northwest Africa duri...
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Response of the North Atlantic surface and intermediate ocean structure to clima...
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Climate conditions in the westernmost Mediterranean over the last two millennia:...
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Increasing P limitation and viral infection impact lipid remodeling of the picop...
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Rapid climate changes in the Western most Mediterranean (Alboran Sea) over the l...
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Four organic sea surface temperature proxies (UK'37, TEXH86, RI-OH' and LDI) in...
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Four organic sea surface temperature proxies (UK'37, TEXH86, RI-OH' and LDI) in...
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Edaphobacter lichenicola sp. nov., a member of the family Acidobacteriaceae from...
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Large ancient organic matter contributions to Arctic marine sediments (Svalbard)
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A cold and fresh ocean surface in the Nordic Seas during MIS 11: Significance fo...
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On the potential application of polar and temperate marine microalgae for EPA an...
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