OOIR: Observatory of International Research

Papers

(The H4-Index of Global and Planetary Change is 31. The table below lists those papers that are above that threshold based on CrossRef citation counts [max. 250 papers]. The publications cover those that have been published in the past four years, i.e., from 2021-12-01 to 2025-12-01.)

Article	Citations
Editorial Board	73
Ichnology, sedimentology, and orbital cycles in the hemipelagic Early Jurassic Laurasian Seaway (Pliensbachian, Cardigan Bay Basin, UK)	72
Mid-Piacenzian and future changes in South Asian precipitation under global warming	63
The Central Paratethys Sea – Part of the tropical eastern Atlantic rather than gate into the Indian Ocean	59
Exploring the impact of the Great Green Wall on Atlantic Tropical Cyclone activity	58
ITCZ precipitation and cloud cover excursions control Cedrela nebulosa tree-ring oxygen and carbon isotopes in the northwestern Amazon	54
Population migration with improved productivity caused a heterogeneity pattern of Holocene vegetation succession in typical areas of the lower Yangtze region	48
Benzo[ghi]fluoranthene and benz[a]anthracene as potentially useful wildfire temperature indicators	46
A link between the paleoenvironment and PETM via trace element proxies in Southwest Atlantic sediments	45
Orbital eccentricity and inclination metronomes in Middle Miocene lacustrine mudstones of Jiuxi Basin, Tibet: Closing an astrochronology time gap and calibrating global cooling events	44
Local sulfur sources control the development of Mississippi Valley-type Pb-Zn deposits worldwide	43
Assessment of Indian Ocean upwelling changes and its relationship with the Indian monsoon	42
Editorial Board	42
Reconciling inconsistent trends of geochemical and environmental magnetic records from East Asian sediments based on modern calibration	41
Regional landscape change triggered by Andean uplift: The extinction of Sparassodonta (Mammalia, Metatheria) in South America	40
A strong influence of the precession and northern high latitudinal climate on the monsoon seasonality and productivity in the Andaman Sea	39
Climate or tectonics? What controls the spatial-temporal variations in erosion rates across the Eastern Cordillera of Colombia? [Global and planetary change, volume 203, August 2021, 103,541]: Comment	37
Nature of Devonian anoxic events based on multiproxy records from Panthalassa, NW Canada	37
Temperature variability revealed by lacustrine brGDGTs in northeastern China since the Last Glacial Maximum	36
Constraints on Earth-Moon dynamical parameters from Eocene cyclostratigraphy	36
Permafrost controls the displacement rates of large unstable rock-slopes in subarctic environments	36
Geodynamic evolution of the Paleo-Asian Ocean: Sr–Nd–Pb–Hf isotopic evidence from Paleozoic ophiolites and arc igneous rocks in the Central Tianshan, Northwest China	35
Cenozoic mountain building of the West Qinling and its correlation with formation of the earliest eolian red clays in the Chinese Loess Plateau	34
Warming and drying increased the interspecies consistency of tree-ring lignin methoxy δ2H variability at the alpine treeline	34
Change of global land extreme temperature in the future	33

Monsoon variability and high latitude climate signals in the central Mediterranean at the Pliocene – Pleistocene transition: the Gelasian stratotype section (Monte San Nicola, Sicily)	33
Tracking magmatism and oceanic change through the early Aptian Anoxic Event (OAE 1a) to the late Aptian: Insights from osmium isotopes from the westernmost Tethys (SE Spain) Cau Core	33
Anaerobic oxidation of methane and greigite formation: Evidence of isotopically heavy pyrite in Pleistocene coastal sediments from the South Yellow Sea	33
Spatio-temporal characteristics and driving factors of flash drought in northern China from 1978 to 2020	32
Coupled feedback between the tropics and subtropics of the Indian Ocean with emphasis on the coupled interaction between IOD and SIOD	31
Dual carbon isotopes constrain the sources and age variations of terrestrial organic carbon in the middle Okinawa Trough since the last deglaciation	31