3.4 Origin of the microbial world: Part 4 - Jan Audun Rasmussen

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Do curso por University of Copenhagen

Origens - Formação do Universo, Sistema Solar, Terra e Vida

362 classificações

University of Copenhagen

Origens - Formação do Universo, Sistema Solar, Terra e Vida

362 classificações

O curso "Origens" traça a origem de todas as coisas - a partir do Big Bang até a origem do Sistema Solar e da Terra. O curso segue a Evolução da vida no nosso planeta desde os primórdios do tempo geológico até as formas de vida atuais.

Na lição

Origin of the microbial world / The Cambrian Explosion and Exceptional Preservation

In this module Jan Audun Rasmussen and Danny Eibye-Jacobsen will show you how life evolved during the first 4 billion years since the creation of the Earth. As you will see, it is very challenging to study the oldest life forms of our planet. During this enormous time span – which covers about 80% of the Earth’s history – microbial life slowly evolved to form a crucial component of the biosphere. Toward the end of the period the deepest foundations of the different groups of animals evolved. All of the life forms surrounding us today can be traced back to this time.

3.1 Origin of the microbial world: Part 1 - Jan Audun Rasmussen 16:55

3.2 Origin of the microbial world: Part 2 - Jan Audun Rasmussen12:53

3.3 Origin of the microbial world: Part 3 - Jan Audun Rasmussen13:01

3.4 Origin of the microbial world: Part 4 - Jan Audun Rasmussen 9:52

3.5 Origin of the Metazoans and evolution of life at small scale - Danny Eibye-Jacobsen15:37

3.6 The Cambrian Explosion and exceptional preservation: Part 1 - Danny Eibye-Jacobsen12:58

3.7 The Cambrian Explosion and exceptional preservation: Part 2 - Danny Eibye-Jacobsen12:29

3.8 The Cambrian Explosion and exceptional preservation: Part 3 - Danny Eibye-Jacobsen6:35

Conheça os instrutores

Henning Haack
Associate Professor
Natural History Museum
James Connelly
Professor
Natural History Museum of Denmark
Vivi Vajda
Professor
Department of Geology, Lund University
Jon Fjeldså
Professor, Curator
Thomas Gilbert
Professor
Michael Houmark-Nielsen
Associate Professor
Natural History Museum of Denmark
Bent Erik Kramer Lindow
Curator
Natural History Museum of Denmark
Gilles Guy Roger Cuny
Associate Professor
Natural History Museum of Denmark
Ole Seberg
Associate Professor
Natural History Museum of Denmark
Gitte Petersen
Associate Professor
Natural History Museum of Denmark
Tais Wittchen Dahl
Assistant Professor of Geobiology
Arne Thorshøj Nielsen
Associate Professor
Natural History Museum of Copenhagen
Martin Vinther Sørensen
Associate Professor, Curator
Natural History Museum of Denmark
Svend Stouge
Associate Professor
Natural History Museum of Denmark
Danny Eibye Jacobsen
Associate Professor, Curator
Natural History Museum of Denmark
Jan Audun Rasmussen
Associate Professor
Natural History Museum of Denmark
Emily Catherine Pope
Assistant professor
Natural History Museum of Denmark

[MUSIC]

We will now move forward to the Neoproterozoic era

that started about a thousand million years ago.

Organic microfossils from the Neoproterozoic are not unusual.

But it was shown in 2010, by an American research team,

that the highest diversity occurred between 800 million and 700 million years

and again somewhere after 580 million years.

Also, the morphological disparity among microscopic eukaryotes, which may

be explained as morphological variation, increased during the Neoproterozoic.

The rising acritarch diversification in the early Neoproterozoic

has been related to the evolution of

sexual reproduction in the late Mesoprotozoic,

and the British research group led by Timothy Lenton showed in 2014

that the so-called cyanobacteria-dominated biological pump in the oceans

was replaced by the eukaryote-dominated pump starting before the Cryogenian glaciations.

Some of the important Eukaryotes that evolved just before the glaciations

include testate amoebae, and very small 10 to 30 microns phosphatic,

eukaryrotic scales preserved in about 800 million years old rocks from Canada.

It is not certain what has driven this pre-glacial Neoproterozoic

diversification among the eukaryotes.

But it was suggested by Susanna Porter in 2011 that predation among

uni-cellular organisms may have had an influence on the rising diversity.

It is possible that also the oceanic increase in oxygen and

nitrogen have had an effect.

The Cryogenian Period spans an interval from 850 to 635 million years.

It includes two major glaciations called the Sturtian and Marinoan glaciations

and a smaller named the Gaskiers glaciation.

This Cryogenian glacial event is sometimes called the Second Snowball Earth

not to be confused with the Paleoproterozoic Snowball Earth event.

The name Snowball Earth is related to the hypothesis that the cold

period resulted in very extensive glaciations.

Perhaps causing that the ocean bottom at

times was frozen solid even at low latitudes.

Some scientists are sceptical to this and suggest that it only reached a

so-called "slush-ball" stage.

No matter what is true, it is clear that the glacial period

influenced negatively on the evolution and diversification of life,

as it has been shown that the diversification of

eukaryotes was significantly lowered during the glacial events.

The Rodinia Supercontinent did form some 900 million years ago and

broke up again at about 750 million years.

The Cryogenian glaciations occurred just after the break up,

between 720 and 580 million years.

An international research team published in 2009 in

Nature the oldest evidence of Metazoa.

More precisely they detected biomarkers indicating the occurrence of

the group of sponges called Demospongia

from 635 million years old rocks from the end of the Cryogenian.

The living natural bath-sponges, which some of you

may know to also belong to the Demospongia.

Demospongia are benthic organisms living on the sea floor

both in marine environments and lakes.

An intriguing hypothesis was published by Lenton and

co-workers in 2014 in Nature Geoscience.

They suggested that both the shift from cyanobacteria to

eukaryotic algae as primary oxygen producers

and the appearance of filter-feeding benthic animals like the sponges,

had a significant influence on both ventilation of the shelf seas and

the removal of phosphorous.

As a consequence, they hypothesized that the amount of phosphate and

global oxygen demand in the sea, decreased during the Neoproterozoic

without requiring an increase in the atmospheric oxygen.

The result was more oxygenated sea-water and

diversification of higher- oxygen-demanding animals.

After a long and relatively stable period that lasted from the

mid-Mesoprotozoic, to approximately 600 million years,

atmospheric oxygen levels began to rise again,

especially in the late Neoproterozoic, just after the end of the glacial period.

Analysis of the iron content of deep-sea sediments from Newfoundland,

shows that the deep ocean was anoxic and ferruginous, that is rich in iron-2,

before and during the last of the Neoproterozoic glaciations around 580

million years ago that is called the Gaskiers glaciation.

Don Canfield and co-workers have shown, however, that the oxygen content of

the deep sea rose significantly just after the last Neoproterozoic glacial period.

The first convincing Metazoan fossils were found in the Ediacarian, nearly

575 million years ago in old phosphoritic sediments

from the Yangtze platform, southeast China.

This very unique Lagerstatte has been named the Doushantuo Formation Lagerstatte.

The exceptional fossils

include both putative metazoan embryos, larvae, and microfossils;

unnamed, mature, possible Cnidaria which possibly are Hydrozoans and

tubular fossils that probably belong to Cnidaria,

which is the phylum where also corals belong.

The Doushantuo biota was succeeded by the Ediacara biota, consisting of several

different macroscopic and microscopic ecosystems recognized globally.

The Ediacara biota consists of very special organisms

representing puzzling tubular and frond shaped, mostly sessile organisms,

which lived during the Ediacaran period from 635

million years ago to 541 million years ago.

The Ediacara biota radiated about 575 millions years ago,

just after the end of the Cryogenian period's extensive glaciations.

The biota didn't survive the Precambrian/Cambrian boundary at 541

million years.

The taxonomical classification of most of the organisms is currently unsolved.

Fossil of both sponges, that is Porifera, and more advanced animals called

Bilateria have been found from the period just before the Cambrian,

but the Ediacaran period was mainly characterized by

experimental life forms without secure ties to the living organism groups,

and they had only a very short temporal extent, geologically speaking.

It was suggested by Buss and Seilacher of Yale University that several taxa

were so special that they were transferred to a new kingdom called Vendobionta.

Originally, in 1994,

Seilacher interpreted them as a possible sister group of the Eumetazoa,

but nine years later, he and co-workers suggested the quite controversial idea

that they may instead be giant protozoans.

Perhaps related to Foraminifera.

But perhaps we are now a little bit closer to understand these extraordinary fossils.

In 2014, Danish scientists from the Natural History Museum of Denmark

discovered and described a new living non-bilaterian genus, called Dendrogramma

originating from between 400 and 1,000 meters depth offshore Tasmania.

It has been suggested that Dendrogramma perhaps may be

related to representatives of the Ediacara biota.

At the entrance to the Cambrian the development of life began to

take a serious hold among multi-cellular organisms,

particularly among the metazoans.

Many new features were invented such as hard skeletons and hard teeth.

The oxygen content increased also in the deep part of the oceans,

and organisms developed new feeding strategies and

occupied new niches and habitats.

The resulting explosive rise in

biodiversity has been called the Cambrian explosion.

[MUSIC]

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