For thousands of years, the olive tree has stood as a symbol of resilience and tradition in the Mediterranean. But a groundbreaking study reveals that this iconic plant is not just a product of nature—it is a living archive of human ambition, cultural exchange, and adaptation.
By analyzing ancient pollen, climate records, and archaeological findings, researchers have uncovered how Sicilian communities transformed their landscape through olive cultivation over 3,700 years.
This story, hidden in the mud of a coastal lake, challenges long-held assumptions about the origins of Mediterranean agriculture and offers urgent lessons for today’s climate challenges.
How Sicily’s Olive Trees Shaped Mediterranean History
The study centered on Pantano Grande, a salt marsh near Sicily’s Strait of Messina. Salt marshes are coastal wetlands flooded by tides, known for preserving organic material like pollen in their oxygen-poor sediments. This strategic location, a crossroads for ancient traders, preserved layers of sediment dating back to 1800 BCE.
Scientists extracted cores of mud, each layer acting like a time capsule. Within these layers, pollen grains told a vivid story: olive trees dominated the landscape during three key periods—the Bronze Age, Roman times, and the modern era.
To distinguish human influence from natural growth, researchers developed the Olea Index, a tool comparing olive pollen to wild shrubs and oaks. The Olea Index uses two metrics:
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Olea Index MED: Compares olive pollen to Mediterranean shrubs like Pistacia (a genus of flowering plants) and Phillyrea (evergreen shrubs).
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Olea Index OAK: Compares olive pollen to evergreen oaks (Quercus ilex).
When olive levels outpace these plants (values >0), it signals human intervention rather than natural growth.
Radiocarbon dating, a method that measures the decay of carbon-14 isotopes in organic material, and volcanic ash layers (tephra) provided precise timelines. For example, ash from Mount Etna’s FL eruption around 1100 BCE helped correlate Sicilian data with other Mediterranean records.
Climate proxies, such as oxygen isotopes (δ¹⁸O) in lake carbonates, revealed wet or dry phases. Oxygen isotopes are atoms of oxygen with different molecular weights; higher δ¹⁸O values indicate drier conditions.
Meanwhile, archaeological evidence—olive pits (stone seeds inside olives), wood fragments, and oil lamps—confirmed that people were actively using olives long before previously assumed.
Bronze Age Origins of Olive Cultivation in Sicily
The oldest evidence of olive exploitation in Sicily dates to the Early-Middle Bronze Age (1800–1100 BCE). The Bronze Age marks a period when humans first widely used bronze tools, revolutionizing agriculture and trade.
During this period, olive pollen accounted for 35% of all plant remains in Pantano Grande, peaking at 50% in some layers.
This surge coincided with the rise of the Thapsos-Milazzese culture, a Sicilian society known for its fortified settlements and trade ties to Mycenaean Greece and Cyprus.
Mycenaean pottery (ceramics from ancient Greece) and Cypriot copper ingots (metal trade bars) found in Sicilian tombs suggest a bustling exchange network. Olives likely traveled these routes as luxury goods, with oil used for cooking, lighting, and rituals.
But these early olives were not the cultivated varieties we know today. Instead, Bronze Age Sicilians practiced proto-domestication, a term describing early human management of wild plants without full genetic domestication. Proto-domestication involved protecting wild groves, pruning trees, and selectively harvesting fruit.
Wood from olive trees built homes and ships, while leaves fed livestock. Fruit was pressed into oil or preserved as food. This system required no formal farming—people simply encouraged wild groves to thrive.
Climate proxies played a supporting role. Oxygen isotopes from lake sediments indicate relatively wet conditions, with steady rainfall nurturing both wild and managed trees. However, this balance would soon collapse.
The Role of Human Intervention in Olive Tree Expansion
Around 1100 BCE, olive pollen levels plummeted to less than 5%. This sharp decline aligns with the Late Bronze Age Collapse, a period of societal disintegration across the Mediterranean caused by invasions, droughts, and trade breakdowns. In Sicily, the trigger was twofold.
- First, Mount Etna’s FL eruption (named for the Fornazzo-Linguaglossa region) blanketed the region in ash, blocking sunlight and damaging crops. Volcanic ash layers, called tephra, are critical for dating because they create precise time markers in sediment cores.
- Second, the collapse of Mycenaean Greece—a dominant Bronze Age civilization—severed trade networks. Without access to eastern markets, Sicilian communities abandoned coastal settlements and retreated inland.
Archaeological evidence paints a grim picture. Coastal villages like Thapsos were deserted, while fortified hilltop settlements emerged. Pollen records show grasses and weeds replacing olives, suggesting a return to subsistence farming (farming only for survival, not trade). Yet, even in this decline, the stage was set for future revival.
Roman Engineering and Sicily’s Ancient Olive Groves
Olive pollen surged again during Roman rule (138 BCE–235 CE), though never reaching Bronze Age peaks. At its height, olive levels hit 20–25%, alongside cereals like wheat and barley.
The Romans, masters of agricultural engineering, transformed Sicily into a breadbasket (a region producing surplus grain) and oil jar for their empire.
They introduced terracing (carving steps into hillsides to prevent soil erosion) and built irrigation channels to combat drier conditions, evident in rising oxygen isotope values.
Large estates called latifundia (industrial-scale Roman farms) mass-produced olive oil. Archaeological sites reveal olive presses (machines to extract oil) and amphorae (clay jars for storage). Amphorae stamped with Sicilian origins have been found as far as Britain, proving the island’s role in long-distance trade.
However, Roman olives were genetically distinct from Bronze Age varieties, imported from the eastern Mediterranean to meet imperial demand. This shift marked the beginning of a genetic bottleneck (reduced genetic diversity due to selective breeding), which still affects Sicilian groves today.
- After the Roman Empire fell, olive cultivation withered. Pollen levels dropped to 5–10% during the Arab invasions (827–1061 CE), as political instability and arid climates made large-scale farming untenable.
Abandoned groves were replaced by scrubland (land dominated by shrubs), with hardy plants like Pistacia and Phillyrea taking over. Yet, even in decline, olives persisted in small household gardens, a testament to their cultural staying power.
Modern Threats to Sicily’s Iconic Olive Landscapes
From the 18th century onward, olives returned with a vengeance. Pollen levels soared to 40%, but this revival came at a cost. Modern Sicilian groves rely heavily on imported Middle Eastern varieties, sidelining native wild olives.
Genetic studies show that 98% of today’s trees descend from just five ancient lineages, leaving them vulnerable to diseases like Xylella fastidiosa, a bacterial pathogen that blocks water flow in plants.
Since 2013, Xylella has destroyed over 1 million trees in Sicily, highlighting the risks of monoculture farming (cultivating a single crop species).
Industrial farming methods exacerbated soil degradation and water scarcity. Wild olive populations, once thriving in Bronze Age forests, have declined by 72%.
Despite these challenges, the study highlights a silver lining: Sicilian farmers are now reviving agroforestry (mixing trees with crops) and planting drought-resistant wild varieties, blending traditional knowledge with modern science.
Lessons from Sicily’s Olive-Driven Agricultural Past
The 3,700-year pollen record from Pantano Grande offers more than historical insight—it provides a roadmap for sustainable agriculture. First, it proves that olives thrived not because of ideal climates, but through human adaptability.
Bronze Age communities weathered volcanic winters by diversifying crops, while Romans engineered solutions to droughts. Second, it warns against over-reliance on monocultures. The genetic uniformity of modern groves mirrors mistakes made by the Romans, who prioritized yield over diversity.
Perhaps most importantly, the study redefines “natural” landscapes. What we see as timeless olive groves are, in fact, human creations—shaped by millennia of trial, error, and cultural exchange.
As climate change intensifies, this long-term perspective is vital. Farmers are already drawing inspiration from the past, reviving Bronze Age agroforestry techniques to build resilient groves.
The Future of Sicily’s Olive Trees Amid Climate Change
While groundbreaking, the study leaves gaps. Without ancient DNA analysis of olive pits (stone seeds), researchers cannot pinpoint domestication dates. Comparisons with North African sites are scarce, skewing the narrative toward European perspectives.
Future projects aim to sequence Bronze Age olive DNA and expand pollen studies to Sardinia and Malta, two islands with similar Mediterranean climates.
Another priority is understanding modern threats. Xylella fastidiosa, unknown in ancient times, requires urgent attention. By combining ancient data with climate models, scientists hope to predict how the disease will spread in a warming world.
Conclusion
The story of Sicily’s olive trees is a mirror reflecting humanity’s best and worst traits—ingenuity, resilience, but also shortsightedness.
From Bronze Age traders navigating the Strait of Messina to Roman engineers terracing hillsides, each generation left its mark on the land. Today, as we face unprecedented ecological crises, this history reminds us that solutions often lie in the past.
As lead researcher Jordan Palli notes, “Every olive grove is a dialogue between humans and nature. To protect them, we must listen to both voices.” By learning from 3,700 years of adaptation, we can ensure that Sicily’s olives—and the cultures they sustain—endure for millennia to come.
Power Terms
Palynology: The study of pollen grains and spores found in sediments, soil, or archaeological sites. It helps scientists understand past vegetation, climate, and human activities by analyzing the types and amounts of pollen preserved over time. For example, in this study, palynology was used to track changes in olive tree populations around Pantano Grande lake. Importance: It reveals how landscapes and human practices evolved. Use: Reconstructing historical plant communities and human impacts on ecosystems.
Pollen Zones (PZ): Divisions in sediment layers based on changes in pollen types and amounts. These zones help identify shifts in vegetation or climate over time. In the paper, three main pollen zones (PZ1, PZ2, PZ3) were identified, each representing different phases of olive tree dominance or decline. Importance: They provide a timeline of ecological changes. Example: PZ1 (1750–1150 BCE) showed high olive pollen, indicating olive tree expansion.
Olea Index: A tool to determine if olive pollen increases are natural or human-driven. Two formulas were used:
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Olea Index MED = (Olea% – Mediterranean shrubs%) / (Olea% + Mediterranean shrubs%)
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Olea Index OAK = (Olea% – Oak%) / (Olea% + Oak%)
Positive values suggest human influence. Importance: Helps distinguish wild olive growth from cultivation. Example: High values in the Bronze Age linked olive expansion to human activity.
Radiocarbon Dating: A method to estimate the age of organic materials by measuring radioactive carbon-14 decay. It was used to date sediment layers in Pantano Grande. Importance: Provides timelines for ecological and cultural changes. Example: Dating revealed olive pollen peaks around 3700 BP (Before Present).
Tephra Layers: Volcanic ash deposits in sediment cores. These act as time markers because they correspond to known eruptions. Importance: Helps synchronize timelines across regions. Example: The FL tephra layer from Mount Etna linked Pantano Grande’s sediment to other Sicilian sites.
δ¹⁸O (Oxygen Isotopes): A measure of oxygen isotopes in lake carbonates or ice cores, reflecting past climate conditions (wet/dry periods). In the study, δ¹⁸O data from Lago di Pergusa showed Sicily’s climate during olive expansion. Importance: Connects vegetation changes to climate. Example: Wet conditions in the Bronze Age supported olive growth.
Thermo-Mediterranean Subhumid Bioclimate: A warm, moderately rainy climate zone typical of coastal Mediterranean regions. The study area (Peloro Cape) falls under this category. Importance: Explains the natural habitat for wild olive trees. Example: Average 18°C temperature and 800 mm annual rainfall suit olive growth.
Anthropogenic Propagation: Human-driven spread of plants, either through cultivation or land management. The paper links olive expansion in Sicily to Bronze Age societies. Importance: Shows how humans shape ecosystems. Example: Early Sicilians likely promoted wild olives for food, wood, or trade.
Biocultural Heritage: Landscapes shaped by the interaction of nature and culture over time. Olive groves are iconic Mediterranean examples. Importance: Highlights the value of traditional practices. Example: Sicilian olive groves reflect 3700 years of human-nature collaboration.
Domestication: Adapting wild species for human use through selective breeding. Olive domestication began in the Near East ~7000 years ago. Importance: Explains genetic changes in crops. Example: Sicilian olives may have mixed wild and domesticated traits.
Molecular Analyses: Studying DNA to trace plant origins and relationships. The paper mentions genetic evidence linking modern olives to Eastern Mediterranean ancestors. Importance: Reveals migration and trade routes. Example: Most Italian olives share genes with ancient Levantine varieties.
Principal Component Analysis (PCA): A statistical method simplifying complex data into key trends. In the study, PCA showed how olive pollen dominated over other plants. Importance: Identifies major ecological shifts. Example: PC1 explained 44% of pollen variation, highlighting olive’s impact.
Microcharcoal: Tiny charcoal particles in sediments, indicating past fires. The study found microcharcoal peaks during olive expansion phases. Importance: Links fire events to human activity or climate. Example: High charcoal in PZ1 suggests fire use for land clearance.
Coprophilous Fungus: Fungi that grow on animal dung, like Sporormiella. Their spores in sediments indicate livestock presence. Importance: Tracks pastoralism. Example: Increased spores in PZ2b (850–250 BCE) signal farming activity near Pantano Grande.
Zygnematacean Algae: Freshwater algae (e.g., Pseudoschizaea) indicating wetland conditions. Their rise in PZ2b suggests soil erosion or marsh changes. Importance: Reflects local environmental shifts. Example: Algae peaks correlate with agricultural expansion.
Pollen Influx: The rate at which pollen accumulates in sediments (grains/cm²/year). High influx means nearby plant activity. Importance: Measures vegetation density. Example: Olive pollen influx peaked during Roman times, showing intensive cultivation.
Cultural Stages: Periods defined by societal changes, like the Bronze Age or Roman era. The paper ties olive trends to three stages: Bronze Age, Roman, and Kingdom of Sicily. Importance: Connects ecology to human history. Example: Olive declines in PZ2a (1150–850 BCE) match trade network collapses.
Trade Networks: Routes for exchanging goods (e.g., metals, olive oil). Sicily’s position in Mediterranean trade boosted olive spread. Importance: Explains crop diffusion. Example: Mycenaean pottery in Sicily hints at Bronze Age olive exchanges.
Wild vs. Cultivated Olive: Wild olives (Olea europaea var. sylvestris) are smaller and less oily than cultivated ones (Olea europaea var. europaea). The study debates their historical overlap. Importance: Differentiation affects domestication theories. Example: Pollen alone can’t confirm cultivation; seeds or wood are better evidence.
Sedimentation Rate: How quickly sediment layers form (e.g., cm/year). Pantano Grande’s rate (~5 years/cm) allowed high-resolution analysis. Importance: Affects timeline accuracy. Example: Slow rates provide detailed climate records.
Pollen Sum: Total pollen grains counted in a sample, used to calculate percentages. Aquatic plants were excluded to focus on land vegetation. Importance: Standardizes data for comparison. Example: A sum of 350 grains ensured statistical reliability.
Paleoclimate Proxies: Indirect climate indicators (e.g., pollen, isotopes). The study used δ¹⁸O and pollen to infer past rainfall. Importance: Reconstructs environments without direct measurements. Example: Wet phases in δ¹⁸O matched oak pollen increases.
Vegetation Dynamics: Changes in plant communities over time. The paper tracks shifts between olives, oaks, and grasses. Importance: Shows ecological responses to climate/humans. Example: Grass replaced olives after Bronze Age societal collapse.
Archaeobotanical Evidence: Plant remains (seeds, wood) from archaeological sites. The study cites olive stones in Sicilian Bronze Age villages. Importance: Direct proof of plant use. Example: Ustica Island olive wood shows early exploitation.
Rewilding: Natural return of ecosystems after human abandonment. Post-Roman declines in olive pollen suggest land recovery. Importance: Highlights human-environment resilience. Example: Shrublands replaced farms during medieval conflicts.
Reference:
Palli, J., Fiolna, S., Bini, M., Cappella, F., Izdebski, A., Masi, A., Mensing, S., Nigro, L., Piovesan, G., Sadori, L., & Zanchetta, G. (2025). The human-driven ecological success of olive trees over the last 3700 years in the Central Mediterranean. Quaternary Science Reviews, 356, 109313. https://doi.org/10.1016/j.quascirev.2025.109313