Charles C. Mann, "Bio-blender Earth"

This lecture was presented as part of The Long Now Foundation’s monthly Seminars About Long-term Thinking.

Living in the Homogenocene: The First 500 Years

Monday April 23, 02012 – San Francisco

Video is up on the Mann Seminar page for Members.

*********************

Audio is up on the Mann Seminar page, or you can subscribe to our podcast.

*********************

Bio-blender Earth – a summary by Stewart Brand

Tumultuous effects resulted and continue to result from the massive mixing of the world’s biota when European ships reconnected the American continent to the rest of the world. Mann traced several of the cascading consequences of “the biggest ecological convulsion since the death of the dinosaurs.”

The first momentous change came from microbial exchange—20 lethal diseases came from Europe to the Americas while only one (syphilis) went the other way. North America, which had been largely cleared by natives with fire and agriculture, reforested when two-thirds to 95% of the native inhabitants died from European diseases—“the greatest demographic catastrophe in human history.” That huge reforesting drew down atmospheric carbon dioxide and Europe’s “Little Ice Age” (1550-1800) apparently resulted.

Meanwhile the mountain of silver at Potosí, Bolivia, vastly enriched Europe, which “went shopping” worldwide. Trading ships coursed the world’s oceans. One artifact picked up from Peru was the potato—a single variety of the 6,000 available. When potatoes in Europe turned out to provide four times the amount of food per acre as wheat, the previously routine famines came to an end, population soared, governments became more stable, and they began building global empires. After 1843 guano shipped by the ton from coastal Peru for fertilizer introduced high-input agriculture. In Ireland 40% of the exploding population ate only potatoes. Around 1844 a potato blight arrived from Mexico, and a million Irish died in the Great Famine and a million more emigrated.

In China, which has no large lakes and only two major rivers, agriculture had been limited to two wet regions where rice could be grown. Two imports from America—maize and sweet potato—could be farmed in dry lands. As in Europe, population went up. Vast areas were terraced as Han farmers pushed westward as far as the Mongolian desert. In heavy rains the terraces melted into the streams, and silt built up in the lowlands, elevating the rivers as much as 40 feet above the surrounding terrain, so when they flooded, millions died. “A Katrina per month for 100 years,” as one Chinese meteorologist described it. The constant calamities weakened the government, and China became ripe for foreign colonial takeover.

In America two imported diseases—malaria and yellow fever—were selective in who they killed. Europeans died in huge numbers, but Africans were one-tenth as susceptible, and so slavery replaced traditional indentured servitude in all the warm regions that favored mosquito-borne diseases. As one result, four times as many Africans as Europeans crossed the Atlantic and began mixing with the remaining native Americans, giving rise to an endless variety of racial blends and accompanying vitality throughout the Americas.

During the Q & A, Mann described a potential fresh eco-convulsion-in-waiting. “There is an area in southeast Asia roughly the size of Great Britain that is a single giant rubber plantation.” Where rubber trees originally came from in the Amazon there is now a rubber tree leaf-blight that is starting to spread in Asia. “You could lose all the rubber trees in three to six months. It would be the biggest deforestation in a long time.” The entire auto industry, he added, depends on just-in-time delivery of rubber.

Subscribe to our Seminar email list for updates and summaries.

Share on Facebook Share on Twitter

More from Announcements

What is the long now?

The Long Now Foundation is a nonprofit established in 01996 to foster long-term thinking. Our work encourages imagination at the timescale of civilization — the next and last 10,000 years — a timespan we call the long now.

Learn more

Join our newsletter for the latest in long-term thinking

Long Now's website is changing...