Earth and Planetary Science - Open Access Policy Deposits
Parent: Department of Earth and Planetary Science
eScholarship stats: Breakdown by Item for July through October, 2026
| Item | Title | Total requests | Download | View-only | %Dnld |
|---|---|---|---|---|---|
| 6sr7r702 | Contamination source modeling with SCRuB improves cancer phenotype prediction from microbiome data | 3,075 | 2,970 | 105 | 96.6% |
| 0qh5400s | Asgard archaea illuminate the origin of eukaryotic cellular complexity | 1,125 | 445 | 680 | 39.6% |
| 3428v1r6 | Observational determination of surface radiative forcing by CO2 from 2000 to 2010 | 745 | 282 | 463 | 37.9% |
| 5nn5k347 | Deccan volcanism at K-Pg time | 683 | 409 | 274 | 59.9% |
| 1n55m9r9 | Crystallization by particle attachment in synthetic, biogenic, and geologic environments | 664 | 234 | 430 | 35.2% |
| 9ks7v8nv | Unusual biology across a group comprising more than 15% of domain Bacteria | 540 | 260 | 280 | 48.1% |
| 8x03v7vf | Is a wet-bulb temperature of 35 ∘C the correct threshold for human survivability? | 529 | 140 | 389 | 26.5% |
| 9gn649wp | Chapter 4 The Precambrian paleogeography of Laurentia | 486 | 176 | 310 | 36.2% |
| 3bg1f0t3 | New CRISPR–Cas systems from uncultivated microbes | 471 | 263 | 208 | 55.8% |
| 881113j7 | Phillipsite and Al-tobermorite mineral cements produced through low-temperature water-rock reactions in Roman marine concrete | 465 | 239 | 226 | 51.4% |
| 9ft608qj | The Precambrian paleogeography of Laurentia | 459 | 304 | 155 | 66.2% |
| 127352f5 | Why the Forcing from Carbon Dioxide Scales as the Logarithm of Its Concentration | 453 | 53 | 400 | 11.7% |
| 0d72911v | Exact Expression for the Lifting Condensation Level | 436 | 125 | 311 | 28.7% |
| 4ww343m7 | Imaging the Meissner effect in hydride superconductors using quantum sensors | 430 | 238 | 192 | 55.3% |
| 5jd7x994 | The Fascinating and Complex Dynamics of Geyser Eruptions | 429 | 310 | 119 | 72.3% |
| 4g491916 | COBRA improves the completeness and contiguity of viral genomes assembled from metagenomes | 421 | 279 | 142 | 66.3% |
| 5xs3w45m | The geophysics, geology and mechanics of slow fault slip | 412 | 232 | 180 | 56.3% |
| 7h70k3r1 | Campanian Ignimbrite volcanism, climate, and the final decline of the Neanderthals | 409 | 190 | 219 | 46.5% |
| 4st880qz | Harnessing the GPS Data Explosion for Interdisciplinary Science | 407 | 191 | 216 | 46.9% |
| 0x75w0pj | Projected increase in lightning strikes in the United States due to global warming | 399 | 206 | 193 | 51.6% |
| 2qw922pr | New insights into Mn2+ and Mg2+ inhibition of calcite growth | 395 | 256 | 139 | 64.8% |
| 2xz601d0 | Predicting fatal heat and humidity using the heat index model | 390 | 291 | 99 | 74.6% |
| 65h6718x | A new view of the tree of life | 384 | 278 | 106 | 72.4% |
| 4dz5g9x3 | Biosynthetic capacity, metabolic variety and unusual biology in the CPR and DPANN radiations | 383 | 233 | 150 | 60.8% |
| 5146j96s | Earthquake transformer—an attentive deep-learning model for simultaneous earthquake detection and phase picking | 382 | 75 | 307 | 19.6% |
| 56g272dg | Revisiting short-term earthquake triggered volcanism | 382 | 182 | 200 | 47.6% |
| 71q1b4jn | A map of the rubisco biochemical landscape | 371 | 218 | 153 | 58.8% |
| 82x2055s | Tracking the weight of Hurricane Harvey’s stormwater using GPS data | 371 | 145 | 226 | 39.1% |
| 4k06c637 | Arc-continent collisions in the tropics set Earth’s climate state | 363 | 125 | 238 | 34.4% |
| 6tk816t9 | Fallout melt debris and aerodynamically-shaped glasses in beach sands of Hiroshima Bay, Japan | 357 | 137 | 220 | 38.4% |
| 3h42c90k | Mechanism of Ferric Oxalate Photolysis | 354 | 80 | 274 | 22.6% |
| 1fv2v6jd | The NASA Psyche Mission: The First up-Close Exploration of a Metal-Rich World | 352 | 306 | 46 | 86.9% |
| 0v05s7t5 | Clouds and Convective Self‐Aggregation in a Multimodel Ensemble of Radiative‐Convective Equilibrium Simulations | 345 | 276 | 69 | 80.0% |
| 3tp9t0w4 | Forecasting Tropical Annual Maximum Wet‐Bulb Temperatures Months in Advance From the Current State of ENSO | 341 | 302 | 39 | 88.6% |
| 2gq7t0cf | Shock compression of stishovite and melting of silica at planetary interior conditions | 331 | 55 | 276 | 16.6% |
| 0299z0z4 | Major New Microbial Groups Expand Diversity and Alter our Understanding of the Tree of Life | 329 | 64 | 265 | 19.5% |
| 7226f497 | Earthquake Early Warning: Advances, Scientific Challenges, and Societal Needs | 327 | 149 | 178 | 45.6% |
| 8sj8w1rf | The eruptive tempo of Deccan volcanism in relation to the Cretaceous-Paleogene boundary | 317 | 171 | 146 | 53.9% |
| 4bp114m5 | Biomineralization: Integrating mechanism and evolutionary history | 312 | 132 | 180 | 42.3% |
| 3q4714cg | Flood Basalts and Mass Extinctions | 310 | 102 | 208 | 32.9% |
| 1rd181nc | Leveraging Submarine DAS Arrays for Offshore Earthquake Early Warning: A Case Study in Monterey Bay, California | 307 | 171 | 136 | 55.7% |
| 2z2404tn | Failed rifting and fast drifting: Midcontinent Rift development, Laurentia’s rapid motion and the driver of Grenvillian orogenesis | 307 | 216 | 91 | 70.4% |
| 9rx7w6vm | Mineralogical, magnetic and geochemical data constrain the pathways and extent of weathering of mineralized sedimentary rocks | 307 | 169 | 138 | 55.0% |
| 537967ff | Electron Mobility and Trapping in Ferrihydrite Nanoparticles | 304 | 241 | 63 | 79.3% |
| 5fk799n8 | State shift in Deccan volcanism at the Cretaceous-Paleogene boundary, possibly induced by impact | 301 | 188 | 113 | 62.5% |
| 7dh443bf | The late Mesoproterozoic to early Neoproterozoic Grenvillian orogeny and the assembly of Rodinia: Turning point in the tectonic evolution of Laurentia | 301 | 159 | 142 | 52.8% |
| 3tj9z6tt | Monitoring natural gas storage using Synthetic Aperture Radar: are the residuals informative? | 299 | 248 | 51 | 82.9% |
| 400782gj | Genomic resolution of a cold subsurface aquifer community provides metabolic insights for novel microbes adapted to high CO2 concentrations | 296 | 210 | 86 | 70.9% |
| 5032h14q | Trapped bubbles keep pumice afloat and gas diffusion makes pumice sink | 292 | 158 | 134 | 54.1% |
| 2pc59445 | Floquet Prethermalization with Lifetime Exceeding 90 s in a Bulk Hyperpolarized Solid | 290 | 150 | 140 | 51.7% |
Note: Due to the evolving nature of web traffic, the data presented here should be considered approximate and subject to revision. Learn more.