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J.S. Sinninghe Damsté

J.S. Sinninghe Damsté

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Earth Science
Netherlands
2026

J.S. Sinninghe Damsté publication distribution in Earth Science in 2026

The chart shows the distribution of publications by all Research.com ranked scientists in the field of Earth Science in 2026. The highlighted bar marks where J.S. Sinninghe Damsté sits on this spectrum.

38–42 publications: 1 scientists 43–47 publications: 0 scientists 48–52 publications: 3 scientists 53–57 publications: 8 scientists 58–62 publications: 11 scientists 63–67 publications: 16 scientists 68–72 publications: 24 scientists 73–77 publications: 31 scientists 78–82 publications: 49 scientists 83–87 publications: 77 scientists 88–92 publications: 86 scientists 93–97 publications: 88 scientists 98–102 publications: 92 scientists 103–107 publications: 84 scientists 108–112 publications: 102 scientists 113–117 publications: 108 scientists 118–122 publications: 117 scientists 123–127 publications: 126 scientists 128–132 publications: 146 scientists 133–137 publications: 114 scientists 138–142 publications: 102 scientists 143–147 publications: 127 scientists 148–152 publications: 102 scientists 153–157 publications: 112 scientists 158–162 publications: 102 scientists 163–167 publications: 127 scientists 168–172 publications: 121 scientists 173–177 publications: 112 scientists 178–182 publications: 109 scientists 183–187 publications: 98 scientists 188–192 publications: 92 scientists 193–197 publications: 105 scientists 198–202 publications: 77 scientists 203–207 publications: 80 scientists 208–212 publications: 89 scientists 213–217 publications: 70 scientists 218–222 publications: 74 scientists 223–227 publications: 74 scientists 228–232 publications: 70 scientists 233–237 publications: 67 scientists 238–242 publications: 59 scientists 243–247 publications: 67 scientists 248–252 publications: 51 scientists 253–257 publications: 46 scientists 258–262 publications: 41 scientists 263–267 publications: 39 scientists 268–272 publications: 34 scientists 273–277 publications: 39 scientists 278–282 publications: 35 scientists 283–287 publications: 36 scientists 288–292 publications: 35 scientists 293–297 publications: 29 scientists 298–302 publications: 23 scientists 303–307 publications: 39 scientists 308–312 publications: 34 scientists 313–317 publications: 23 scientists 318–322 publications: 18 scientists 323–327 publications: 18 scientists 328–332 publications: 21 scientists 333–337 publications: 20 scientists 338–342 publications: 15 scientists 343–347 publications: 13 scientists 348–352 publications: 24 scientists 353–357 publications: 25 scientists 358–362 publications: 10 scientists 363–367 publications: 20 scientists 368–372 publications: 17 scientists 373–377 publications: 18 scientists 378–382 publications: 15 scientists 383–387 publications: 7 scientists 388–392 publications: 22 scientists 393–397 publications: 9 scientists 398–402 publications: 11 scientists 403–407 publications: 16 scientists 408–412 publications: 4 scientists 413–417 publications: 5 scientists 418–422 publications: 14 scientists 423–427 publications: 8 scientists 428–432 publications: 7 scientists 433–437 publications: 7 scientists 438–442 publications: 10 scientists 443–447 publications: 10 scientists 448–452 publications: 3 scientists 453–457 publications: 9 scientists 458–462 publications: 11 scientists 463–467 publications: 4 scientists 468–472 publications: 6 scientists 473–477 publications: 11 scientists 478–482 publications: 8 scientists 483–487 publications: 2 scientists 488–492 publications: 3 scientists 493–497 publications: 4 scientists 498–502 publications: 4 scientists 503–507 publications: 4 scientists 508–509 publications: 4 scientists 510+ publications: 100 scientists
38 publications 510+

The last bar groups every scientist with 510 publications or more.

J.S. Sinninghe Damsté D-index placement in Earth Science in 2026

The chart shows the D-index (discipline H-index) distribution of Earth Science scientists ranked by Research.com in 2026. The highlighted bar marks where J.S. Sinninghe Damsté sits on this spectrum.

30 D-Index: 15 scientists 31 D-Index: 42 scientists 32 D-Index: 60 scientists 33 D-Index: 90 scientists 34 D-Index: 103 scientists 35 D-Index: 108 scientists 36 D-Index: 142 scientists 37 D-Index: 147 scientists 38 D-Index: 147 scientists 39 D-Index: 152 scientists 40 D-Index: 143 scientists 41 D-Index: 157 scientists 42 D-Index: 141 scientists 43 D-Index: 151 scientists 44 D-Index: 140 scientists 45 D-Index: 135 scientists 46 D-Index: 121 scientists 47 D-Index: 108 scientists 48 D-Index: 128 scientists 49 D-Index: 111 scientists 50 D-Index: 106 scientists 51 D-Index: 112 scientists 52 D-Index: 102 scientists 53 D-Index: 103 scientists 54 D-Index: 94 scientists 55 D-Index: 61 scientists 56 D-Index: 101 scientists 57 D-Index: 71 scientists 58 D-Index: 65 scientists 59 D-Index: 78 scientists 60 D-Index: 93 scientists 61 D-Index: 56 scientists 62 D-Index: 58 scientists 63 D-Index: 52 scientists 64 D-Index: 63 scientists 65 D-Index: 49 scientists 66 D-Index: 53 scientists 67 D-Index: 57 scientists 68 D-Index: 50 scientists 69 D-Index: 44 scientists 70 D-Index: 44 scientists 71 D-Index: 31 scientists 72 D-Index: 33 scientists 73 D-Index: 33 scientists 74 D-Index: 23 scientists 75 D-Index: 32 scientists 76 D-Index: 24 scientists 77 D-Index: 17 scientists 78 D-Index: 19 scientists 79 D-Index: 9 scientists 80 D-Index: 21 scientists 81 D-Index: 20 scientists 82 D-Index: 17 scientists 83 D-Index: 19 scientists 84 D-Index: 19 scientists 85 D-Index: 14 scientists 86 D-Index: 6 scientists 87 D-Index: 14 scientists 88 D-Index: 17 scientists 89 D-Index: 10 scientists 90 D-Index: 8 scientists 91 D-Index: 8 scientists 92 D-Index: 9 scientists 93 D-Index: 6 scientists 94+ D-Index: 98 scientists
30 D-Index 94+

The last bar groups every scientist with 94 D-Index or more.

Research.com Recognitions

  • 2026 - Research.com Earth Science in Netherlands Leader Award
  • 2025 - Research.com Earth Science in Netherlands Leader Award
  • 2005 - Royal Netherlands Academy of Arts and Sciences
  • 2004 - Spinoza Prize, Dutch Research Council

Overview

What is he best known for?

The fields of study he is best known for:

  • Ecology
  • Organic chemistry
  • Bacteria

J.S. Sinninghe Damsté mainly investigates Oceanography, Total organic carbon, Paleontology, Photic zone and Archaea. His research brings together the fields of Sedimentary rock and Oceanography. The concepts of his Total organic carbon study are interwoven with issues in Organic matter, Kerogen, Algaenan, Geochemistry and Nannochloropsis sp..

His Photic zone research includes elements of Sterane, Hopanoids, Isotopes of carbon and Anoxic waters. His Archaea study incorporates themes from Environmental chemistry, Anaerobic oxidation of methane, Methane and Glycerol. The study incorporates disciplines such as Glacial period and Vegetation in addition to Holocene.

His most cited work include:

  • Evidence for gammacerane as an indicator of water column stratification (626 citations)
  • Revised calibration of the MBT–CBT paleotemperature proxy based on branched tetraether membrane lipids in surface soils (276 citations)
  • Application of biological markers in the recognition of palaeohypersaline environments (235 citations)

What are the main themes of his work throughout his whole career to date?

J.S. Sinninghe Damsté focuses on Oceanography, Sediment, Environmental chemistry, Paleontology and Ecology. His studies deal with areas such as Sedimentary rock and Organic matter as well as Oceanography. His Organic matter research is multidisciplinary, relying on both Total organic carbon and Terrigenous sediment.

His Environmental chemistry study integrates concerns from other disciplines, such as Sulfur, Isotopes of carbon, Archaea, Mineralogy and Methane. His Archaea research integrates issues from Carbonate and Cold seep. His research investigates the link between Paleontology and topics such as Geochemistry that cross with problems in Anaerobic oxidation of methane.

He most often published in these fields:

  • Oceanography (42.71%)
  • Sediment (14.06%)
  • Environmental chemistry (13.02%)

What were the highlights of his more recent work (between 2013-2021)?

  • Oceanography (42.71%)
  • Sediment (14.06%)
  • Holocene (11.98%)

In recent papers he was focusing on the following fields of study:

J.S. Sinninghe Damsté spends much of his time researching Oceanography, Sediment, Holocene, Sea surface temperature and Sedimentary rock. The concepts of his Oceanography study are interwoven with issues in Organic matter and Particulates. His study looks at the relationship between Sediment and topics such as Environmental chemistry, which overlap with Methanotroph, Petroleum seep, Hydrogen and Oxygen minimum zone.

His work on Last Glacial Maximum as part of general Holocene research is often related to Distribution, thus linking different fields of science. His Sea surface temperature study combines topics in areas such as Continental shelf and Upwelling. His Sedimentary rock research is multidisciplinary, incorporating elements of Proxy and Provenance.

Between 2013 and 2021, his most popular works were:

  • Spatial heterogeneity of sources of branched tetraethers in shelf systems : The geochemistry of tetraethers in the Berau River delta (Kalimantan, Indonesia) (83 citations)
  • Climate variability and ocean fertility during the Aptian Stage (61 citations)
  • A perturbed hydrological cycle during Oceanic Anoxic Event 2 (57 citations)

In his most recent research, the most cited papers focused on:

  • Ecology
  • Organic chemistry
  • Bacteria

His primary areas of investigation include Oceanography, TEX86, Sediment, Sea surface temperature and Organic matter. The study incorporates disciplines such as Soil water and Seasonality in addition to Oceanography. His TEX86 research is multidisciplinary, incorporating perspectives in Volcano, Stage, Paleontology and Anoxic waters.

His Sea surface temperature study integrates concerns from other disciplines, such as Ocean gyre, Last Glacial Maximum, Holocene and Mediterranean climate, Mediterranean sea. His study in Organic matter is interdisciplinary in nature, drawing from both Structural basin, Total organic carbon, Pleistocene, Sedimentary rock and Provenance. His Total organic carbon study is concerned with the field of Environmental chemistry as a whole.

Best Publications

  • A microbial consortium couples anaerobic methane oxidation to denitrification

    Ashna A. Raghoebarsing;Arjan Pol;Katinka T. van de Pas-Schoonen;Alfons J. P. Smolders

  • Distributional variations in marine crenarchaeotal membrane lipids: a new tool for reconstructing ancient sea water temperatures?

    Stefan Schouten;Ellen C. Hopmans;Enno Schefuß;Jaap S. Sinninghe Damsté

  • A novel proxy for terrestrial organic matter in sediments based on branched and isoprenoid tetraether lipids

    Ellen C Hopmans;Johan W.H Weijers;Enno Schefuß;Lydie Herfort

  • Evidence for gammacerane as an indicator of water column stratification

    J.S. Sinninghe Damsté;F. Kenig;M.P. Koopmans;J. Koster

  • The organic geochemistry of glycerol dialkyl glycerol tetraether lipids: A review

    Stefan Schouten;Ellen C. Hopmans;Jaap S. Sinninghe Damsté

  • Environmental controls on bacterial tetraether membrane lipid distribution in soils

    Johan W.H. Weijers;Stefan Schouten;Jurgen C. van den Donker;Ellen C. Hopmans

  • Restricted utility of the pristane/phytane ratio as a palaeoenvironmental indicator

    H. L. ten Haven;J. W. de Leeuw;J. Rullkötter;J. S. Sinninghe Damsté

  • New indices and calibrations derived from the distribution of crenarchaeal isoprenoid tetraether lipids: Implications for past sea surface temperature reconstructions

    Jung-Hyun Kim;Jaap van der Meer;Stefan Schouten;Peer Helmke

  • Subtropical Arctic Ocean temperatures during the Palaeocene/Eocene thermal maximum

    Appy Sluijs;Stefan Schouten;Mark Pagani;Martijn Woltering

  • Occurrence and distribution of tetraether membrane lipids in soils : Implications for the use of the TEX86 proxy and the BIT index

    Johan W.H. Weijers;Stefan Schouten;Otto C. Spaargaren;Jaap S. Sinninghe Damsté

  • Crenarchaeol: the characteristic core glycerol dibiphytanyl glycerol tetraether membrane lipid of cosmopolitan pelagic crenarchaeota.

    Jaap S Sinninghe Damsté;Stefan Schouten;Ellen C Hopmans;Adri C T van Duin

  • Northern Hemisphere Controls on Tropical Southeast African Climate During the Past 60,000 Years

    Jessica E. Tierney;James M. Russell;Yongsong Huang;Jaap S. Sinninghe Damsté

  • The effect of improved chromatography on GDGT-based palaeoproxies

    Ellen C. Hopmans;Stefan Schouten;Jaap S. Sinninghe Damsté

  • An improved method to determine the absolute abundance of glycerol dibiphytanyl glycerol tetraether lipids

    Carme Huguet;Ellen C. Hopmans;Wilma Febo-Ayala;David H. Thompson

  • Analysis, structure and geochemical significance of organically-bound sulphur in the geosphere : state of the art and future research

    Jaap S. Sinninghe Damste;Jan W. De Leeuw

  • Occurrence and abundance of 6-methyl branched glycerol dialkyl glycerol tetraethers in soils : Implications for palaeoclimate reconstruction

    Cindy De Jonge;Ellen C. Hopmans;Claudia I. Zell;Jung Hyun Kim

  • Cretaceous sea-surface temperature evolution: Constraints from TEX86 and planktonic foraminiferal oxygen isotopes

    Charlotte L. O'Brien;Stuart A. Robinson;Richard D. Pancost;Jaap S. Sinninghe Damsté

  • Arctic hydrology during global warming at the Palaeocene/Eocene thermal maximum

    Mark Pagani;Nikolai Pedentchouk;Matthew Huber;Appy Sluijs

  • Analytical methodology for TEX86 paleothermometry by high-performance liquid chromatography/atmospheric pressure chemical ionization-mass spectrometry.

    Stefan Schouten;Carme Huguet;Ellen C Hopmans;Michiel V M Kienhuis

  • Revised calibration of the MBT–CBT paleotemperature proxy based on branched tetraether membrane lipids in surface soils

    F. Peterse;J. van der Meer;S. Schouten;J.W.H. Weijers

  • Diagenetic and catagenetic products of isorenieratene: Molecular indicators for photic zone anoxia

    Martin P. Koopmans;Jürgen Köster;Heidy M.E. Van Kaam-Peters;Fabien Kenig

  • Global sediment core-top calibration of the TEX86 paleothermometer in the ocean

    Jung-Hyun Kim;Stefan Schouten;Ellen C. Hopmans;Barbara Donner

  • Application of biological markers in the recognition of palaeohypersaline environments

    H. L. ten Haven;J. W. de Leeuw;J. S. Sinninghe Damsté;P. A. Schenck

Frequent Co-Authors

Ellen C. Hopmans
Ellen C. Hopmans Royal Netherlands Institute for Sea Research
J.W. de Leeuw
J.W. de Leeuw Delft University of Technology
Stefan Schouten
Stefan Schouten Utrecht University
Marianne Baas
Marianne Baas Delft University of Technology
Gert-Jan Reichart
Gert-Jan Reichart Utrecht University
Francien Peterse
Francien Peterse Utrecht University
Dirk Verschuren
Dirk Verschuren Ghent University
Henk Brinkhuis
Henk Brinkhuis Utrecht University
John M. Hayes
John M. Hayes Woods Hole Oceanographic Institution
Johan W.H. Weijers
Johan W.H. Weijers Shell (Netherlands)

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