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A number of acronyms in this essay are not commonly used and at least one is unique to my work.

The path to developing FE technology for public use outlined above I believe work, but there are also other ways that the Fifth Epochal Event can manifest. If I had to bet on how it will manifest, I would put my money on the struggle between the , and on their beginning to release some of their sequestered technologies. The reason why their organized suppression efforts have been so successful is that they know if of it makes it to the public, it will only be a matter of time before the dam breaks, which would probably include ETs openly interacting with humanity. The GCs know that if any of that happens, their days of ruling humanity will quickly end. That is partly why this hump has been so hard to get over. But I am not going to wait for something to happen at that level to save us all, and what I am attempting will also help form a nucleus of awareness that can greatly help with an enlightened and harmless implementation of FE. If FE makes its appearance, its implementation will need to be led by as many enlightened and informed people as possible. Some need to be ahead of the curve to lead the way, if only by promoting an enlightened awareness. Once people can see FE with their own eyes, preferably by having it delivered to their home (anything less, and ; they will not be talked into an abundance-based mentality; they must experience it), the should be pretty rapid, especially if there is already a choir singing the song of abundance.

For several years before writing this essay, I have stated that the only inventor-oriented approach with a prayer is for an inventor with the goods (a viable prototype undoubtedly generating FE) to give it to a worthy group so that they can take it the rest of the way, past humanity’s inertia and any organized suppression activities that might be inflicted on the effort. I have never heard of the inventor with the goods willing to give it away, and that worthy group does not yet exist; my efforts could be seen as trying to help form it. Criticizing the inventor with the goods who is unwilling to give it away, when there is nobody worth giving it to, is unproductive.

After I first published this essay in September 2014, I read Paul Boyer's , which surveyed the reactions of Americans to dropping atom bombs on Japan. I read it in relation to my studies regarding the , but what struck me was how similar the reactions to the bombs were to how people view FE today. The primary difference, of course, is that everybody acknowledges that nuclear bombs exist and have been used, while almost nobody acknowledges today that FE technology exists, through , , or . Another obvious difference is that the first use of atomic energy was vaporizing a couple of cities. While the initial American reaction was celebratory and euphoric, it quickly became evident that the USA would not hold a monopoly on nuclear weapons forever, and fears of nuclear attack became part of the fabric of American consciousness, and by 1946, nearly half of Americans were amenable to the idea of a world government that could prevent a nuclear holocaust.

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From their , monkeys , and between 35 and 29 mya, according to molecular clock studies, some African monkeys , and , a controversial transitional fruit-eating monkey, appeared about 25 mya. most famous find was a skull in 1948. The primary differences between apes and monkeys are that apes are larger, lost their tails (not having as much need for balancing on tree limbs), and they have a stiffer spine and larger brain. Apes began the descent from canopy to ground. Simians will eat fruit if they can, but some developed thicker tooth enamel. That change meant that they no longer subsisted on soft fruit and leaves, but were eating coarser vegetation, which was a consequence of living in a cooler, dryer world. No Miocene apes were as adapted to leaf eating as today’s apes and leaf-eating monkeys. As with , a prominent speculation today is that those monkeys/apes changed their diets and left the trees as they lost the competitive game with other canopy-dwellers. split from the line that became great apes about 22 mya and became masters of tree-living, with their swinging mode of locomotion.

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From their through their and in the Eocene, primates continued evolving. About 35 mya, and monkeys, called (also called simians or anthropoids), split. Simians seem to have split from a group also ancestral to . Today’s prosimians include , , , and . During the , Africa and Southeast Asia became primate refugia. Tarsiers have , and the live on islands near Southeast Asia. Primate history in the late Eocene and Oligocene is controversial today. The fate of an from primates’ is debated, but they seem at least cousins to ancestors of , if not ancestral to them.

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But the African Oligocene event of most interest to most humans was African primate evolution. By the Eocene’s end, primates were extinct in Europe and North America, and largely gone in Asia. Africa became the Oligocene's refuge for primates as they lived in the remaining rainforest. The first animals that evolved in the late Eocene, and what appears to be a appeared in Africa at the Oligocene’s beginning, about 35-33 mya. But ancestral to that creature was one that also led to those that migrated to South America, probably via vegetation rafts (with perhaps a land bridge helping), around the same time. Those South American monkeys are known as today and they evolved in isolation for more than 30 million years. For those that stayed behind in Africa, first appeared around the same time as those New World monkeys migrated; they diverged from . Scientists today think that somewhere between about 35 mya and 29 mya the splits between those three lineages happened. Old World and New World monkeys have not changed much in the intervening years, but apes sure have.

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The appeared in North America in the late Eocene and early Oligocene, and in Europe in the late Oligocene. It might be amusing to consider, but cats and dogs are close cousins and . in the early Oligocene in North America about 34 mya, and in the late Oligocene about 25 mya. in the late Eocene and early Oligocene, and the in the Oligocene. The common ancestor of today’s sloths lived in the late Eocene; South American appeared in the late Oligocene. The may have begun in the Oligocene. The . By the late Eocene, the had appeared, and squirrels had appeared in North America.


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For several million years, life in the Eocene was halcyonic, and at 50 mya, the state had prevailed ever since the 250 mya. But just as , Earth began cooling off. The ultimate reason was atmospheric carbon dioxide levels that had been steadily declining for tens of millions of years. The intense volcanism of the previous 200 million years waned and the inexorably sequestered carbon into Earth’s crust and mantle. While falling carbon dioxide levels were the ultimate cause, the first proximate cause was probably the isolation of Antarctica at the South Pole and changes in global ocean currents. During the early Eocene, the global ocean floor’s water temperature was about 13oC (55oF), warm enough to swim in, which was a far cry from today’s near-freezing and below-freezing temperatures. The North Sea was warm as bathwater. Radical , warming the ocean floor, and . Whatever the causes were, the oceans were warm from top to bottom, from pole to pole. But between 50 to 45 mya, Australia made its final split from Antarctica and moved northward, India began crashing into Asia and cut off the Tethys Ocean and the global tropical circulation, and South America also moved northward, away from Antarctica. Although the debate is still fierce over the cooling’s exact causes, the evidence (much is from ) is that the oceans cooled off over the next 12 million years, very consistently, although a brief small reversal transpired at about 40 mya. By 37-38 mya, the 200-million-year-plus Greenhouse Earth phase ended and the transition to today’s ice age was underway. In the late Eocene, as the trend toward conditions began, such as the .

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The Oligocene Epoch (c. 34 to 23 mya) was relatively cold. In the 1960s, a , the recovered nearly 20,000 cores from Earth’s oceans, and scientists had paradigm-shift learning experiences from studying those cores. One finding was that Antarctica developed its ice sheets far earlier than previously supposed, and the cores pushed back the initial ice sheet formation by 20 million years, ; the first Antarctic glaciers formed as early as 49 mya. The evidence included in sediments, which meant icebergs. The event that led to Antarctic ice sheets was the formation of the , which began to form about 40 mya and was firmly established by 34 mya, when the Antarctic ice sheets grew in earnest. The current’s formation was caused by Antarctica’s increasing isolation from Australia and South America, which gradually allowed an uninterrupted current to form that circled Antarctica and isolated it so that it no longer received tropical currents. That situation eventually turned Antarctica into the big sheet of ice that it is today. It also radically changed global oceanic currents. formed, which cooled the oceans as well as oxygenated its depths, and it comprises more than half of the water in today’s oceans. began forming around the same time.