Paleoclimate & Environment
Understanding the landscapes, climates, and ecological settings hominins evolved in — from proxy records to geochronology.
Reconstructions of past environments combine multiple independent lines of evidence: pollen and plant macrofossils, faunal community composition, stable isotope ratios from teeth and sediments, and sedimentology (facies, lake levels, aeolian deposits). No single proxy tells the whole story; convergence across proxies strengthens interpretation.
Paleoenvironments map
Sites with coordinates and inferred habitat types from integrated proxy data.
Environment timeline
Records ordered by age (calendar years BP), bars span age_old_bp to age_young_bp, colored by habitat type.
Isotope analysis
Stable isotope measurements from hominin and comparative taxa; δ13C often reflects diet and canopy cover.
| Species | Site | Isotope system | Δ value | Sample material | Interpretation | Date (MYA) |
|---|---|---|---|---|---|---|
| Australopithecus afarensis | Hadar | δC13 | -10.5000 | enamel | Eastern African Pliocene hominins: heterogeneous C3/C4 mix by locale/taxon. | 3.200 |
| Australopithecus africanus | Sterkfontein | δC13 | -6.5000 | enamel | Sterkfontein Au. africanus: mixed C3/C4 browsing/grazing mosaic. | 2.800 |
| Australopithecus africanus | Sterkfontein | δC13 | -8.2000 | enamel | Lower end of Au. africanus δ13C distribution (South African sites). | 2.500 |
| Australopithecus africanus | Sterkfontein | δO18 | -4.2000 | enamel | Bioapatite carbonate oxygen (reporting conventions vary; illustrative site-level value). | 2.500 |
| Paranthropus boisei | — | δC13 | -2.0000 | enamel | Species mean near C4 endmember (East African basins). | 2.000 |
| Australopithecus sediba | Sterkfontein | δC13 | -9.0000 | enamel | Malapa: C3-biased signal in some individuals (environmental/diet heterogeneity). | 2.000 |
| Homo rudolfensis | Koobi Fora | δC13 | -8.8000 | enamel | KNM-ER 1470 early Homo: δ13C within early Homo “C3-heavy” spread. | 1.900 |
| Paranthropus robustus | Swartkrans | δC13 | -5.0000 | enamel | Swartkrans P. robustus: elevated C4 resources vs pure C3 feeders. | 1.800 |
| Paranthropus boisei | Olduvai Gorge | δC13 | -1.2000 | enamel | P. boisei: among most 13C-enriched hominin enamel measured (C4-dominated). | 1.800 |
| Paranthropus boisei | Olduvai Gorge | δO18 | -3.8000 | enamel | Olduvai paleolake hydrology influences δ18O in enamel carbonate. | 1.800 |
| Homo georgicus | Dmanisi | δC13 | -11.5000 | enamel | Dmanisi earliest Eurasian hominin ecosystem (Caucasus). | 1.800 |
| Homo habilis | Koobi Fora | δC13 | -8.0000 | enamel | Early Homo Koobi Fora: more negative δ13C than contemporary Paranthropus. | 1.600 |
| Homo ergaster | Koobi Fora | δC13 | -8.5000 | enamel | H. ergaster/early Homo: predominantly C3 ecosystems with mixed signatures. | 1.600 |
| Paranthropus robustus | Swartkrans | δC13 | -7.1000 | enamel | Spread across individuals/seasons; not a single dietary niche. | 1.500 |
| Paranthropus robustus | Swartkrans | Sr 87 86 | 0.7085 | enamel | Local Sr baseline vs possible non-local individuals (mobility studies). | 1.500 |
| Homo erectus | Wonderwerk Cave | δC13 | -9.5000 | enamel | Wonderwerk Cave: southern African savanna-woodland mix. | 1.000 |
| Homo antecessor | Gesher Benot Ya'aqov | δC13 | -12.0000 | bone apatite | GBY Acheulean occupation: Levantine ecosystem isotopic context. | 0.790 |
| Homo erectus | Zhoukoudian | δC13 | -18.0000 | enamel | Zhoukoudian: C3-dominated local biomass signal in enamel apatite studies. | 0.500 |
| Homo heidelbergensis | Atapuerca | δC13 | -11.0000 | bone collagen | Sima de los Huesos: Middle Pleistocene western European ecosystem. | 0.430 |
| Homo neanderthalensis | Qesem Cave | δN15 | 10.2000 | bone collagen | Qesem Cave: late Lower Palaeolithic meat-dominated protein signal (site studies). | 0.400 |
| Homo erectus | Olorgesailie | δC13 | -11.0000 | enamel | Olorgesailie Acheulean landscape: open grassland expansion in some intervals. | 0.320 |
| Homo sapiens | Jebel Irhoud | δC13 | -13.0000 | enamel | Jebel Irhoud: North African late Middle Pleistocene ecosystems. | 0.315 |
| Homo naledi | Rising Star Cave | δC13 | -10.0000 | enamel | Rising Star: illustrative mixed C3/C4 context for southern Africa (local ecology). | 0.300 |
| Homo neanderthalensis | Schoningen | δN15 | 10.8000 | bone collagen | European Middle Palaeolithic carnivory signal (site-specific). | 0.300 |
| Homo rhodesiensis | Sterkfontein | δC13 | -9.2000 | bone collagen | Kabwe/Broken Hill comparative Middle Pleistocene signal (material debated). | 0.300 |
| Homo sapiens | Omo Kibish | δC13 | -15.0000 | enamel | Omo Kibish: riverine/lacustrine resource δ13C heterogeneity. | 0.195 |
| Homo sapiens | Pinnacle Point | δC13 | -16.0000 | enamel | Pinnacle Point MSA coastal-inland mix (illustrative). | 0.164 |
| Homo sapiens | Klasies River Caves | δC13 | -17.0000 | bone collagen | Klasies River MSA: C3-dominated protein resources (terrestrial/coastal mix). | 0.100 |
| Homo sapiens | Klasies River Caves | δN15 | 11.0000 | bone collagen | MSA humans: high δ15N consistent with marine+terrestrial protein at coast. | 0.100 |
| Homo sapiens | Blombos Cave | δC13 | -12.5000 | bone apatite | Blombos coastal diet: marine influence shifts δ13C (material-dependent). | 0.077 |
| Homo floresiensis | Liang Bua | δC13 | -14.0000 | bone collagen | Flores: island resource δ13C (faunal/hominin comparative frameworks). | 0.060 |
| Homo neanderthalensis | — | δN15 | 10.5000 | bone collagen | Neanderthals: high δ15N consistent with high trophic level meat protein. | 0.050 |
| Homo neanderthalensis | — | δN15 | 9.1000 | bone collagen | Lower δ15N end of Neanderthal range (ecology/age effects). | 0.050 |
| Homo denisova | Denisova Cave | δC13 | -14.0000 | bone collagen | Denisova Cave ecological baseline via fauna comparators (hominin direct values rare). | 0.050 |
| Homo neanderthalensis | Shanidar Cave | δN15 | 11.2000 | bone collagen | Shanidar: elevated δ15N in some individuals (freshwater caveat in some regions). | 0.045 |
| Homo sapiens | Hohle Fels | δC13 | -21.0000 | bone collagen | Upper Palaeolithic Europe: strong C3 terrestrial signal (illustrative). | 0.040 |
δ13C vs. age (MYA)
Scatter of carbon isotope values through time; one color per species (δ13C rows only).
Dating methods
Chronometric and relative ages tied to sites and specimens.
| Site | Specimen | Method | Date (MYA) | Uncertainty | Dated material | Notes |
|---|---|---|---|---|---|---|
| Sterkfontein Member 2 | StW 573 | cosmogenic nuclide | 3.6700 | +0.16 MYA / −0.16 MYA | Quartz pebbles from cave infill surrounding skeleton | |
| Laetoli | — | Ar Ar | 3.6600 | +0.03 MYA / −0.03 MYA | Laetolil Beds tephra | Footprint surface bracketing ~3.66 Ma. |
| Hadar | — | Ar Ar | 3.2000 | +0.02 MYA / −0.02 MYA | Tuffs at Hadar (Kada Hadar Member) | Lucy horizon age cluster ~3.18–3.2 Ma (recalibrated over decades). |
| Sterkfontein | — | cosmogenic nuclide | 2.8000 | +0.3 MYA / −0.3 MYA | Member 4 breccia (surface exposure models) | Sterkfontein Member 4 age debates; multiple methods. |
| Middle Awash | Taung 1 | U Pb | 2.8000 | +0.05 MYA / −0.05 MYA | Flowstone (Taung) | Taung Child age debates; U-Pb flowstone models. |
| Sterkfontein | Stw 573 | U Pb | 2.6700 | +0.15 MYA / −0.15 MYA | Flowstone (Little Foot) | StW 573 flowstone bracketing (published ranges). |
| West Turkana | — | Ar Ar | 2.5000 | +0.05 MYA / −0.05 MYA | Tuffs West Turkana | Black Skull / Nachukui Formation ages. |
| Kromdraai | — | biostratigraphy | 2.0000 | +0.2 MYA / −0.2 MYA | Faunal assemblage | Kromdraai relative dating via biozones (illustrative). |
| Lomekwi | — | U Pb | 1.9770 | +0.003 MYA / −0.003 MYA | Flowstone Malapa | Au. sediba U-Pb flowstone ages ~1.977 Ma (Dirks et al.). |
| Olduvai Gorge | — | Ar Ar | 1.8000 | +0.02 MYA / −0.02 MYA | Tuff I Bed I (crystal separates) | Classic Ar/Ar chronology for Olduvai Bed I hominins/tools. |
| Swartkrans | — | ESR | 1.8000 | +0.2 MYA / −0.2 MYA | Tooth enamel (Swartkrans) | Swartkrans Member chronologies. |
| Gona | — | paleomagnetism | 1.8000 | +0.1 MYA / −0.1 MYA | Section (Drimolen) | South African cave breccia magnetostratigraphy (site-dependent). |
| Border Cave | — | Ar Ar | 1.8000 | +0.05 MYA / −0.05 MYA | Trinil section | Java Homo erectus classic age brackets. |
| Olduvai Gorge | OH 5 | K Ar | 1.7900 | +0.05 MYA / −0.05 MYA | Basalt below OH 5 | OH 5 approximate stratigraphic age (literature range). |
| Dmanisi | — | paleomagnetism | 1.7800 | +0.05 MYA / −0.05 MYA | Section through Dmanisi | Magnetostratigraphic alignment to global polarity timescale. |
| Dmanisi | D3444 | Ar Ar | 1.7700 | +0.02 MYA / −0.02 MYA | Basalt beneath hominin layers | Dmanisi hominins ~1.77–1.85 Ma (stratigraphic summaries). |
| Callao Cave | — | Ar Ar | 1.6600 | +0.03 MYA / −0.03 MYA | Sangiran tuffs | Sangiran H. erectus chronology. |
| Koobi Fora | KNM-WT 15000 | Ar Ar | 1.5600 | +0.02 MYA / −0.02 MYA | KBS Tuff (context) | Turkana Boy ~1.56 Ma (Turkana radioisotope framework). |
| Atapuerca | — | Ar Ar | 1.2000 | +0.05 MYA / −0.05 MYA | Atapuerca section tephras | Gran Dolina TD6 context (regional chronologies). |
| Wonderwerk Cave | — | OSL | 1.0700 | +0.1 MYA / −0.1 MYA | Cave sediments (Wonderwerk) | Early fire evidence layers (site publications). |
| Gesher Benot Ya'aqov | — | Ar Ar | 0.7900 | +0.05 MYA / −0.05 MYA | Basalt chronology (Levant) | GBY ~780 ka occupation (classic range). |
| Herto | — | Ar Ar | 0.6000 | +0.05 MYA / −0.05 MYA | Bodo volcanic context | Bodo cranium Middle Pleistocene East Africa. |
| Atapuerca | Cranium 5 | U series | 0.4300 | +0.02 MYA / −0.02 MYA | Speleothems / flowstone (Sima) | Sima de los Huesos minimum ages (U-series frameworks). |
| Zhoukoudian | Zhoukoudian III | U series | 0.4000 | +0.05 MYA / −0.05 MYA | Zhoukoudian speleothems / stratigraphy | Locality 1 chronology (complex). |
| Terra Amata | — | ESR | 0.4000 | +0.05 MYA / −0.05 MYA | Tooth enamel | Petralona cave chronologies (debated). |
| Qesem Cave | — | ESR | 0.4000 | +0.05 MYA / −0.05 MYA | Tooth enamel | Qesem Cave ages ~400 ka (range in literature). |
| Ceprano | Ceprano 1 | K Ar | 0.4000 | +0.05 MYA / −0.05 MYA | Volcanic sediment associated with calvaria | |
| Rising Star Cave | — | ESR | 0.3350 | +0.05 MYA / −0.05 MYA | Tooth enamel (H. naledi) | Dirks et al. 2017: H. naledi ages 236–335 ka. |
| Olorgesailie | — | Ar Ar | 0.3200 | +0.03 MYA / −0.03 MYA | Tephra correlations | Olorgesailie Acheulean chronology (southern Kenya). |
| Jebel Irhoud | Jebel Irhoud 1 | U series | 0.3150 | +0.03 MYA / −0.03 MYA | Flowstone Irhoud | Jebel Irhoud H. sapiens ~315 ka (multi-method). |
| Schoningen | — | U series | 0.3000 | +0.03 MYA / −0.03 MYA | Speleothem / peat (context) | Schöningen spears ~300 ka (site summaries). |
| Lazaret Cave | Kabwe 1 | U series | 0.3000 | +0.05 MYA / −0.05 MYA | U-series on bone (context) | Kabwe direct dating attempts (contested). |
| Penghu Channel | Penghu 1 | biostratigraphy | 0.3000 | +0.15 MYA / −0.15 MYA | Associated dredged fauna (Stegodon, Rhinoceros) | |
| Bouri Formation | — | ESR | 0.2600 | +0.04 MYA / −0.04 MYA | Enamel (Florisbad) | Late Middle Stone Age hominin contexts (illustrative). |
| Florisbad | Florisbad cranium | ESR | 0.2590 | +0.035 MYA / −0.035 MYA | Bovid tooth enamel from associated deposit | |
| Rising Star Cave | DH1 | U series | 0.2360 | +0.03 MYA / −0.03 MYA | Flowstone ages (Dinaledi) | Young end of naledi age distribution. |
| Omo Kibish | Omo 1 | Ar Ar | 0.1960 | +0.005 MYA / −0.005 MYA | KHS tephra Omo Kibish | Omo I KHS ~196 ka (radioisotope frameworks). |
| Pinnacle Point | — | OSL | 0.1640 | +0.02 MYA / −0.02 MYA | Coastal sediments | Pinnacle Point 5–164 ka MSA occupations. |
| Herto | BOU-VP-16/1 | Ar Ar | 0.1600 | +0.002 MYA / −0.002 MYA | Dacitic tuff underlying hominin-bearing horizon | |
| Nesher Ramla | NR-1 | U series | 0.1300 | +0.01 MYA / −0.01 MYA | Bovid tooth enamel from same stratum | |
| Klasies River Caves | — | OSL | 0.1150 | +0.015 MYA / −0.015 MYA | Coastal sediments | Klasies River MSA ages (site publications). |
| Blombos Cave | — | OSL | 0.0770 | +0.007 MYA / −0.007 MYA | Sediments (MSA) | Blombos Still Bay / MSA chronologies. |
| Liang Bua | LB1 | Ar Ar | 0.0600 | +0.01 MYA / −0.01 MYA | Jaramillo ash near Liang Bua | LB1 bracketing (Flores chronology). |
| Shanidar Cave | Shanidar 1 | radiocarbon C14 | 0.0500 | +0.005 MYA / −0.005 MYA | Charcoal (Neanderthal layers) | Shanidar MP/UP chronology (site-specific calibrations). |
| Denisova Cave | — | radiocarbon C14 | 0.0500 | +0.01 MYA / −0.01 MYA | Charcoal / bone (molecular age) | Denisova Cave stratigraphic chronology (multiple labs). |
| Hohle Fels | — | radiocarbon C14 | 0.0400 | +0.005 MYA / −0.005 MYA | Charcoal (Aurignacian contexts) | Hohle Fels Upper Palaeolithic ages. |