134 citations as recorded by crossref.

1. Carbon isotope constraints on glacial Atlantic meridional overturning: Strength vs depth J. Muglia & A. Schmittner 10.1016/j.quascirev.2021.106844
2. Description of a global marine particulate organic carbon-13 isotope data set M. Verwega et al. 10.5194/essd-13-4861-2021
3. A global estimate of the full oceanic 13C Suess effect since the preindustrial M. Eide et al. 10.1002/2016GB005472
4. Carbon isotope excursions during the late Miocene recorded by lipids of marine Thaumarchaeota, Piedmont Basin, Mediterranean Sea M. Sabino et al. 10.1130/G49360.1
5. Stable Carbon Isotopes Suggest Large Terrestrial Carbon Inputs to the Global Ocean E. Kwon et al. 10.1029/2020GB006684
6. Competition between ocean carbon pumps in simulations with varying Southern Hemisphere westerly wind forcing W. Huiskamp et al. 10.1007/s00382-015-2781-0
7. Planktonic foraminifera organic carbon isotopes as archives of upper ocean carbon cycling B. Hoogakker et al. 10.1038/s41467-022-32480-0
8. Using ocean models to predict spatial and temporal variation in marine carbon isotopes S. Magozzi et al. 10.1002/ecs2.1763
9. Constraints on natural global atmospheric CO2 fluxes from 1860 to 2010 using a simplified explicit forward model H. Hellevang & P. Aagaard 10.1038/srep17352
10. Carbon stable isotope record in the coral species Siderastrea stellata: A link to the Suess Effect in the tropical South Atlantic Ocean N. Pereira et al. 10.1016/j.palaeo.2018.02.007
11. Simulating stable carbon isotopes in the ocean component of the FAMOUS general circulation model with MOSES1 (XOAVI) J. Dentith et al. 10.5194/gmd-13-3529-2020
12. Revisiting the relationship between the pore water carbon isotope gradient and bottom water oxygen concentrations H. Bradbury et al. 10.1016/j.gca.2023.12.011
13. Atlantic Meridional Overturning Circulation and δ13C Variability During the Last Interglacial A. Kessler et al. 10.1029/2019PA003818
14. Impacts of geography, taxonomy and functional group on inorganic carbon use patterns in marine macrophytes C. Stepien & A. Austin 10.1111/1365-2745.12451
15. Stable carbon isotopes of dissolved inorganic carbon for a zonal transect across the subpolar North Atlantic Ocean in summer 2014 M. Humphreys et al. 10.5194/essd-8-221-2016
16. Impact of oceanic circulation changes on atmospheric δ13CO2 L. Menviel et al. 10.1002/2015GB005207
17. The Southern Ocean during the ice ages: A review of the Antarctic surface isolation hypothesis, with comparison to the North Pacific D. Sigman et al. 10.1016/j.quascirev.2020.106732
18. Reversible scavenging and advection – Resolving the neodymium paradox in the South Atlantic R. Wang et al. 10.1016/j.gca.2021.09.015
19. Millennial changes in North Atlantic oxygen concentrations B. Hoogakker et al. 10.5194/bg-13-211-2016
20. The atmospheric bridge communicated the <i>δ</i><sup>13</sup>C decline during the last deglaciation to the global upper ocean J. Shao et al. 10.5194/cp-17-1507-2021
21. An internally consistent dataset of <i>δ</i><sup>13</sup>C-DIC in the North Atlantic Ocean – NAC13v1 M. Becker et al. 10.5194/essd-8-559-2016
22. The anthropogenic perturbation of the marine nitrogen cycle by atmospheric deposition: Nitrogen cycle feedbacks and the 15N Haber‐Bosch effect S. Yang & N. Gruber 10.1002/2016GB005421
23. Calibration of temperature-dependent ocean microbial processes in the cGENIE.muffin (v0.9.13) Earth system model K. Crichton et al. 10.5194/gmd-14-125-2021
24. A baseline for the vertical distribution of the stable carbon isotopes of dissolved inorganic carbon (δ13CDIC) in the Arctic Ocean D. Bauch et al. 10.1007/s41063-015-0001-0
25. Re-assessing the influence of particle-hosted sulphide precipitation on the marine cadmium cycle G. de Souza et al. 10.1016/j.gca.2022.02.009
26. Deconvolving the controls on the deep ocean's silicon stable isotope distribution G. de Souza et al. 10.1016/j.epsl.2014.04.040
27. Reduced oxygenation at intermediate depths of the southwest Pacific during the last glacial maximum A. Durand et al. 10.1016/j.epsl.2018.03.036
28. Less Remineralized Carbon in the Intermediate‐Depth South Atlantic During Heinrich Stadial 1 M. Lacerra et al. 10.1029/2018PA003537
29. Carbon Cycle Responses to Changes in Weathering and the Long‐Term Fate of Stable Carbon Isotopes A. Jeltsch‐Thömmes & F. Joos 10.1029/2022PA004577
30. Global patterns and inferences of tuna movements and trophodynamics from stable isotope analysis J. Logan et al. 10.1016/j.dsr2.2020.104775
31. Identifying physiological and environmental influences on otolith chemistry in a coastal fishery species J. Martino et al. 10.1071/MF20196
32. The large-scale evolution of neodymium isotopic composition in the global modern and Holocene ocean revealed from seawater and archive data K. Tachikawa et al. 10.1016/j.chemgeo.2017.03.018
33. Sources of dissolved inorganic carbon to the Canada Basin halocline: A multitracer study K. Brown et al. 10.1002/2015JC011535
34. Stable carbon isotope ratios of intact GDGTs indicate heterogeneous sources to marine sediments A. Pearson et al. 10.1016/j.gca.2016.02.034
35. Southwest Pacific deep water carbonate chemistry linked to high southern latitude climate and atmospheric CO2 during the Last Glacial Termination K. Allen et al. 10.1016/j.quascirev.2015.05.007
36. Coupling of oceanic carbon and nitrogen facilitates spatially resolved quantitative reconstruction of nitrate inventories N. Glock et al. 10.1038/s41467-018-03647-5
37. Ocean carbon and nitrogen isotopes in CSIRO Mk3L-COAL version 1.0: a tool for palaeoceanographic research P. Buchanan et al. 10.5194/gmd-12-1491-2019
38. Stable carbon isotopes of dissolved inorganic carbon in the Western North Pacific Ocean: Proxy for water mixing and dynamics T. Ge et al. 10.3389/fmars.2022.998437
39. Spatiotemporal variability and drivers of <i>p</i>CO<sub>2</sub> and air–sea CO<sub>2</sub> fluxes in the California Current System: an eddy-resolving modeling study G. Turi et al. 10.5194/bg-11-671-2014
40. Carbon storage in the mid‐depth Atlantic during millennial‐scale climate events M. Lacerra et al. 10.1002/2016PA003081
41. Glacial expansion of carbon-rich deep waters into the Southwestern Indian Ocean over the last 630 kyr J. Pérez-Asensio et al. 10.1016/j.gloplacha.2023.104283
42. Evaluating the Glacial‐Deglacial Carbon Respiration and Ventilation Change Hypothesis as a Mechanism for Changing Atmospheric CO2 L. Stott et al. 10.1029/2020GL091296
43. Integrating machine learning with otolith isoscapes: Reconstructing connectivity of a marine fish over four decades K. Arai et al. 10.1371/journal.pone.0285702
44. A monthly resolved coral δ13C and δ18O record of changes in the Kuroshio Current into the South China Sea via the Luzon Strait X. Li et al. 10.1016/j.palaeo.2023.111468
45. Including an ocean carbon cycle model into <i>i</i>LOVECLIM (v1.0) N. Bouttes et al. 10.5194/gmd-8-1563-2015
46. Rapid Loss of CO2 From the South Pacific Ocean During the Last Glacial Termination K. Allen et al. 10.1029/2019PA003766
47. Southern Ocean influence on the eastern tropical North Pacific's intermediate-depth circulation during the Last Glacial Maximum J. Carriquiry et al. 10.1002/2014PA002766
48. Source‐Labeled Anthropogenic Carbon Reveals a Large Shift of Preindustrial Carbon From the Ocean to the Atmosphere M. Holzer & T. DeVries 10.1029/2022GB007405
49. Latest Pliocene Northern Hemisphere glaciation amplified by intensified Atlantic meridional overturning circulation T. Hayashi et al. 10.1038/s43247-020-00023-4
50. Future Changes in δ13C of Dissolved Inorganic Carbon in the Ocean H. Graven et al. 10.1029/2021EF002173
51. The smoking gun for Atlantic circulation changes A. Schmittner 10.1126/science.aag3156
52. Carbon 13 Isotopes Reveal Limited Ocean Circulation Changes Between Interglacials of the Last 800 ka N. Bouttes et al. 10.1029/2019PA003776
53. Constraining the Variability of the Atlantic Meridional Overturning Circulation During the Holocene J. Lippold et al. 10.1029/2019GL084988
54. No detectable influence of the carbonate ion effect on changes in stable carbon isotope ratios (δ13C) of shallow dwelling planktic foraminifera over the past 160 kyr P. Köhler & S. Mulitza 10.5194/cp-20-991-2024
55. Effects of eustatic sea-level change, ocean dynamics, and nutrient utilization on atmospheric <i>p</i>CO<sub>2</sub> and seawater composition over the last 130 000 years: a model study K. Wallmann et al. 10.5194/cp-12-339-2016
56. Processes Driving Global Interior Ocean pH Distribution S. Lauvset et al. 10.1029/2019GB006229
57. Response of atmospheric CO2 changes to the Abyssal Pacific overturning during the last glacial cycle Y. Zhang et al. 10.1016/j.gloplacha.2024.104636
58. Using the Suess effect on the stable carbon isotope to distinguish the future from the past in radiocarbon P. Köhler 10.1088/1748-9326/11/12/124016
59. Enhanced δ13C and δ18O Differences Between the South Atlantic and South Pacific During the Last Glaciation: The Deep Gateway Hypothesis E. Sikes et al. 10.1002/2017PA003118
60. North Atlantic ocean circulation and abrupt climate change during the last glaciation L. Henry et al. 10.1126/science.aaf5529
61. Temperature-dependent ocean–atmosphere equilibration of carbon isotopes in surface and intermediate waters over the deglaciation J. Lynch-Stieglitz et al. 10.1016/j.epsl.2018.11.024
62. 20th century changes in carbon isotopes and water-use efficiency: tree-ring-based evaluation of the CLM4.5 and LPX-Bern models K. Keller et al. 10.5194/bg-14-2641-2017
63. Stable isotopic signature of Southern Ocean deep water CO2 ventilation K. Prasanna et al. 10.1016/j.dsr2.2015.04.009
64. Carbon Cycling in Marine Particles Based on Inorganic and Organic Stable Isotopes S. Dong et al. 10.1016/j.gca.2024.10.005
65. Holocene North Atlantic Overturning in an atmosphere‐ocean‐sea ice model compared to proxy‐based reconstructions M. Blaschek et al. 10.1002/2015PA002828
66. Evaluation of Paleocene‐Eocene Thermal Maximum Carbon Isotope Record Completeness—An Illustration of the Potential of Dynamic Time Warping in Aligning Paleo‐Proxy Records S. Ajayi et al. 10.1029/2019GC008620
67. Stable carbon isotopic composition of particulate organic matter in the Cosmonaut and Cooperation Seas in summer J. Kang et al. 10.1016/j.pocean.2024.103363
68. Data Constraints on Glacial Atlantic Water Mass Geometry and Properties D. Oppo et al. 10.1029/2018PA003408
69. Southern Ocean controls of the vertical marine <i>δ</i><sup>13</sup>C gradient – a modelling study A. Morée et al. 10.5194/bg-15-7205-2018
70. Trophic Structure of Neuston Across Tropical and Subtropical Oceanic Provinces Assessed With Stable Isotopes R. Albuquerque et al. 10.3389/fmars.2020.606088
71. The first global deep-sea stable isotope assessment reveals the unique trophic ecology of Vampire Squid Vampyroteuthis infernalis (Cephalopoda) A. Golikov et al. 10.1038/s41598-019-55719-1
72. Measurements of the stable carbon isotope composition of dissolved inorganic carbon in the northeastern Atlantic and Nordic Seas during summer 2012 M. Humphreys et al. 10.5194/essd-7-127-2015
73. Insights on long-term ecosystem changes from stable isotopes in historical squid beaks A. Golikov et al. 10.1186/s12862-024-02274-7
74. Modern, Preindustrial, and Past (Last 25 ka) Carbon Isotopic (δ13C) Variability in the Surface Waters of the Southwest Pacific C. Maxson et al. 10.1029/2018PA003441
75. Overturning circulation, nutrient limitation, and warming in the Glacial North Pacific J. Rae et al. 10.1126/sciadv.abd1654
76. Complementary constraints from carbon (13C) and nitrogen (15N) isotopes on the glacial ocean's soft‐tissue biological pump A. Schmittner & C. Somes 10.1002/2015PA002905
77. Variable carbon isotope fractionation of photosynthetic communities over depth in an open-ocean euphotic zone L. Henderson et al. 10.1073/pnas.2304613121
78. The [simple carbon project] model v1.0 C. O'Neill et al. 10.5194/gmd-12-1541-2019
79. Global deepwater circulation between 2.4 and 1.7 Ma and its connection to the onset of Northern Hemisphere Glaciation J. Du et al. 10.1002/2015PA002906
80. Incorporating the stable carbon isotope <sup>13</sup>C in the ocean biogeochemical component of the Max Planck Institute Earth System Model B. Liu et al. 10.5194/bg-18-4389-2021
81. Projected reversal of oceanic stable carbon isotope ratio depth gradient with continued anthropogenic carbon emissions E. Kwon et al. 10.1038/s43247-022-00388-8
82. Multidecadal accumulation of anthropogenic and remineralized dissolved inorganic carbon along the Extended Ellett Line in the northeast Atlantic Ocean M. Humphreys et al. 10.1002/2015GB005246
83. Evidence for a biological pump driver of atmospheric CO2 rise during Heinrich Stadial 1 J. Hertzberg et al. 10.1002/2016GL070723
84. A late Jurassic carbon-isotope record from the Qiangtang Basin (Tibet), eastern Tethys, and its palaeoceanographic implications G. Li et al. 10.1016/j.gloplacha.2020.103349
85. Sensitivity of ocean circulation to warming during the Early Eocene greenhouse S. Kirtland Turner et al. 10.1073/pnas.2311980121
86. Compiled records of carbon isotopes in atmospheric CO<sub>2</sub> for historical simulations in CMIP6 H. Graven et al. 10.5194/gmd-10-4405-2017
87. Carbon isotopes in the marine biogeochemistry model FESOM2.1-REcoM3 M. Butzin et al. 10.5194/gmd-17-1709-2024
88. Rapid shift and millennial-scale variations in Holocene North Pacific Intermediate Water ventilation L. Lembke-Jene et al. 10.1073/pnas.1714754115
89. Weak overturning circulation and high Southern Ocean nutrient utilization maximized glacial ocean carbon J. Muglia et al. 10.1016/j.epsl.2018.05.038
90. Atlantic circulation changes across a stadial–interstadial transition C. Waelbroeck et al. 10.5194/cp-19-901-2023
91. Oceanography and community structure drive zooplankton carbon and nitrogen dynamics in the eastern Bering Sea E. Hertz et al. 10.3354/meps12647
92. Macroevolutionary and macroecological response of Iberian rodents to late Neogene climatic oscillations and events J. van Dam et al. 10.1016/j.gloplacha.2023.104153
93. Temperature-dependent remineralization and carbon cycling in the warm Eocene oceans E. John et al. 10.1016/j.palaeo.2014.05.019
94. Development of a novel empirical framework for interpreting geological carbon isotope excursions, with implications for the rate of carbon injection across the PETM S. Kirtland Turner & A. Ridgwell 10.1016/j.epsl.2015.11.027
95. Alternating Influence of Northern Versus Southern‐Sourced Water Masses on the Equatorial Pacific Subthermocline During the Past 240 ka N. Rippert et al. 10.1002/2017PA003133
96. The lateral transport of zooplankton explains trophic and taxonomic similarities over the zonal gradient of central Chile C. González et al. 10.1016/j.jmarsys.2022.103840
97. How old is too old? Implications of averaging 14C-Based estimates of ventilation age to assess the Pacific Ocean's role in sequestering CO2 in the past L. Stott 10.1016/j.quascirev.2023.108122
98. Coupled biostratigraphy and chemostratigraphy at Lanna, Sweden: A key section for the Floian–lower Darriwilian interval (Lower–Middle Ordovician) A. Lindskog et al. 10.1016/j.palaeo.2023.111446
99. Biogeochemical protocols and diagnostics for the CMIP6 Ocean Model Intercomparison Project (OMIP) J. Orr et al. 10.5194/gmd-10-2169-2017
100. Temporal and spatial trends in marine carbon isotopes in the Arctic Ocean and implications for food web studies C. de la Vega et al. 10.1111/gcb.14832
101. Calibration of the carbon isotope composition (δ13C) of benthic foraminifera A. Schmittner et al. 10.1002/2016PA003072
102. Lower oceanic <i>δ</i><sup>13</sup>C during the last interglacial period compared to the Holocene S. Bengtson et al. 10.5194/cp-17-507-2021
103. Dissolved Inorganic Carbon ([DIC], δ13С(DIC)) in Waters of the Eastern East Siberian Sea E. Dubinina et al. 10.1134/S0016702920080054
104. Open-Ocean Minima in δ13C Values of Particulate Organic Carbon in the Lower Euphotic Zone H. Close & L. Henderson 10.3389/fmars.2020.540165
105. Water column distribution of stable isotopes and carbonate properties in the South-eastern Levantine basin (Eastern Mediterranean): Vertical and temporal change G. Sisma-Ventura et al. 10.1016/j.jmarsys.2016.01.012
106. Assessment of C, N, and Si Isotopes as Tracers of Past Ocean Nutrient and Carbon Cycling J. Farmer et al. 10.1029/2020GB006775
107. A global ocean climatology of preindustrial and modern ocean δ13C M. Eide et al. 10.1002/2016GB005473
108. Experimental support towards a metabolic proxy in fish using otolith carbon isotopes J. Martino et al. 10.1242/jeb.217091
109. A Next Generation Ocean Carbon Isotope Model for Climate Studies I: Steady State Controls on Ocean 13C M. Claret et al. 10.1029/2020GB006757
110. Controls on Alkenone Carbon Isotope Fractionation in the Modern Ocean S. Phelps et al. 10.1029/2021GC009658
111. Strong middepth warming and weak radiocarbon imprints in the equatorial Atlantic during Heinrich 1 and Younger Dryas S. Weldeab et al. 10.1002/2016PA002957
112. Otolith δ13C values as a metabolic proxy: approaches and mechanical underpinnings M. Chung et al. 10.1071/MF18317
113. Carbon isotopes in the ocean model of the Community Earth System Model (CESM1) A. Jahn et al. 10.5194/gmd-8-2419-2015
114. Early deglacial Atlantic overturning decline and its role in atmospheric CO<sub>2</sub> rise inferred from carbon isotopes (δ<sup>13</sup>C) A. Schmittner & D. Lund 10.5194/cp-11-135-2015
115. Application of Stable Carbon Isotopes in a Subtropical North Atlantic MesocosmStudy: A New Approach to Assess CO2 Effects on the Marine Carbon Cycle M. Esposito et al. 10.3389/fmars.2019.00616
116. Incorporating otolith-isotope inferred field metabolic rate into conservation strategies V. de Groot et al. 10.1093/conphys/coae013
117. Strong geochemical anomalies following active submarine eruption offshore Mayotte M. Mastin et al. 10.1016/j.chemgeo.2023.121739
118. Carbon and carbon-13 in the preindustrial and glacial ocean A. Schmittner et al. 10.1371/journal.pclm.0000434
119. The mineralization and early diagenesis of deep-sea coral Madrepora oculata M. Wang et al. 10.1016/j.chemgeo.2022.120966
120. Assessing transient changes in the ocean carbon cycle during the last deglaciation through carbon isotope modeling H. Kobayashi et al. 10.5194/cp-20-769-2024
121. Ocean gateways and circulation dynamics: Unveiling the deep water-mass properties in the western equatorial Pacific since the Middle Miocene H. Bali & A. Gupta 10.1016/j.marmicro.2024.102420
122. Evaluating the Extent of North Atlantic Deep Water and the Mean Atlantic δ13C From Statistical Reconstructions S. Bengtson et al. 10.1029/2019PA003589
123. The Biological Pump During the Last Glacial Maximum E. Galbraith & L. Skinner 10.1146/annurev-marine-010419-010906
124. An international intercomparison of stable carbon isotope composition measurements of dissolved inorganic carbon in seawater L. Cheng et al. 10.1002/lom3.10300
125. Ocean biogeochemistry in the Norwegian Earth System Model version 2 (NorESM2) J. Tjiputra et al. 10.5194/gmd-13-2393-2020
126. Deglacial whole-ocean δ13C change estimated from 480 benthic foraminiferal records C. Peterson et al. 10.1002/2013PA002552
127. Oxygen and carbon isotope records of Upper Cretaceous foraminifera from Poland: vital and microhabitat effects Z. Dubicka et al. 10.1016/j.palaeo.2018.03.029
128. Eastern Atlantic deep-water circulation and carbon storage inferred from neodymium and carbon isotopic compositions over the past 1.1 million years K. Tachikawa et al. 10.1016/j.quascirev.2020.106752
129. Evaluating the biological pump efficiency of the Last Glacial Maximum ocean using <i>δ</i><sup>13</sup>C A. Morée et al. 10.5194/cp-17-753-2021
130. How much did Glacial North Atlantic Water shoal? G. Gebbie 10.1002/2013PA002557
131. The impact of atmospheric pCO2 on carbon isotope ratios of the atmosphere and ocean E. Galbraith et al. 10.1002/2014GB004929
132. Global-mean marine δ13C and its uncertainty in a glacial state estimate G. Gebbie et al. 10.1016/j.quascirev.2015.08.010
133. How well would modern‐day oceanic property distributions be known with paleoceanographic‐like observations? G. Gebbie et al. 10.1002/2015PA002917
134. Deglacial weakening of the oceanic soft tissue pump: global constraints from sedimentary nitrogen isotopes and oxygenation proxies E. Galbraith & S. Jaccard 10.1016/j.quascirev.2014.11.012