The song was inspired, in part, by https://en.wikipedia.org/wiki/The_B...

Thing is

When you're posting on your mobile ..

Itz like a straight jacket ...

You can only say

Fook you to certain zzzzz boring posters on here loike ...

Just saying .

"Namacalathus and Namapoika are the first metazoans to form reefs, especially Cloudina with its weakly calcified shells, documented in the Nama Group of Southern Africa and elsewhere. Cloudina lived at a time when the oceans may have had salinity similar to those of today because of the formation of the rare “saline giants” around 540-550 million years ago, which formed major salt deposits globally. Thus low salinity combined with the rapid degradation of a lengthy mountain chain spanning much of Rodinia (Squire et al., 2006) may have supersaturated the global oceans with both oxygen and the building blocks of hard parts [ Me: “This would be on Earth with a highly stable gyroscopic like daily cycle through of about 21 hours” ]. Higher temperatures, too, would have favored the deposition of calcite. So, both ocean chemistry and temperature may have played a role in the origin and expansion of the metazoans and the first development of shells in the “ocean playgrounds of summer” (Kanuth, 2005; Vickers-Rich, 2006,2007)."

- The Rise of Animals, Mikhail A fedonkin, James G. Gehling, Kathleen Grey, Guy M. Narbonne, Patricia Vickers-Rich

“These were not the first of the Precambrian glacials, which
date back into the Archean. But these younger glacials and
global refrigeration may have given significant advantages to
eukaryotic organisms, which could have developed before in
isolated cold areas near the poles when the Earth was warmer
(Fedonkin’s [1996] “cold cradles”). Another possibility, or even \a “parallel-possibility,” for such “cradles” of metazoans could
have been in fresh waters or in less saline environments, the \interface between fresh waters and the “salty,” open marine
conditions, which could have had twice the concentration of
salt of modern seas (Kanuth, 2005). Both cold and less saline estuarine or fresh waters would have had another advantage,
with their higher oxygen supply (Kanuth, 2005; Vickers-Rich,
2006, 2007).
Between 610 and 605 million years ago massive \ accumulations of salts were laid down globally, preserved
today in Australia, Oman, Saudi Arabia, Iran and Pakistan
(Kanuth, 2005). Before this rather dramatic removal of NaCl
from the oceans, salinity could have been as high as 1.6 to 2
times what it is today - a problem for most living metazoans,
but certainly not an issue for cyanobacteria (Kanuth, 2005).
Increased salinity also rudeness oxygen solubility, and so with
decreased salinity, oxygen levels would have risen in the
global oceans. Further enhancing oxygenation may have been
a marked change in weathering styles, highlighted by Kennedy
and colleagues (2006). With a greater input of weathered
clays, enhanced perhaps by the development and expansion
of an early terrestrial biota, greater volumes of carbon would
have been sequestered, bumping up free oxygen levels in
the environment. This terrestrial input could also have been
increased by tectonic activity at this time that generated a
lengthy mountain range, forcing the burial of organic carbon
that occurred in the late Neoproterozoic (Des Marais et al.,
1992; Squire et al., 2006).
Then, with Earth-wide refrigeration, which lowered ocean
salinity and increased oxygen content (both because of the
cold and the lower salinity), the isolated “cradles” could have
provided the sources of metazoan biodiversity. Metazoans
could have expanded into ore inviting, less saline, well-
oxygenated environments - the “cold playgrounds” of the
global oceans (Vickers-Rich, 2006, 2007) and new ecospace
that provided the chance to construct the new niches that
Douglas Erwin (2005) termed the inventions that let to
innovation - of body plans and diversity. This could explain
why the Ediacaran fauna appeared rather abruptly and long
after genetic studies predict that metazoan body plans should
have arisen (Blair & Hedges, [Me: I only read people theorizing, lining up interesting measurements, but I am interested in the idea of a global clock] ). Condon and Bowring
(2005) also note that there was a major perturbation in the
global carbon cycle (the Shura anomaly) at around 560 to
551 million years, unrelated to glaciation, but “consistent with
progressive oxidation and re-mineralization of the organic
carbon reservoir.” They note that this coincides with the
appearance of such macro-Ediacarans as Kimberella.
These early macro-metazoans are preserved in the
siliciclastics laid down in marine waters, reflected by the
sediments in the White Sea region of Russia, the Flinders
Ranges of South Australia and the Avalon Peninsula of
Newfoundland, suggestive of cool waters. Even in the
carbonate-rich, siliciclastic deposits of southern Namibia,
Ediacara-type microfossils are preserved in the quartzites
that may have been deposited during relatively cool
episodes. In contrast, in the carbonates of Namibia, Cloudina,“

I've written a poem

Itz called

Boss

Black eyes
Stare at me
Wondering
Why>

<https://www.youtube.com/watch?v=rEy...>

https://www.youtube.com/watch?v=M65...

https://www.youtube.com/watch?v=xqB...

<"Then after exhausting every other possibility, <Harry> begin to think. The strain was terrific. And impossible though it seemed, he got an idea">

<https://www.youtube.com/watch?v=INX...>

Smokey Robinson "They said they grew up listening to BLACK music!"

<https://www.youtube.com/watch?v=BOv...>

City punters should not have been paid today. I say the owners withhold a game check, give it to charity.

<https://www.youtube.com/watch?v=2VD...>