The picture in 16.30 from early Devonian, painted by Z.Burian, was the first picture about paleozoic plants I have ever seen. It was in an old paleo book from the 1950s wich belonged my grandpa, but I loved it! Of course there were a lot of wrong things in this book, so all the Silurian and early Devonian plants were called by the same name "psilophytales". But there were many beautiful pictures from the Devonian and Carboniferous in this old book, and they made me getting interested in paleontology and paleobotanic. And the Carboniferous is still one of my most favourite periods in earth history, I would love to have some of the trees like sigillaria or lepidodendron in my garden. And also some Devonian plants, like Asteroxylon or archeosigillaria....😊 I would also like to know more about the Evolution of the angiosperms in the mesozoic, but there are still a lot of unclear things I guess... Best wishes to you all from Germany, and I hope to see more of your videos!
That was fascinating! Just one point of critique; To have the Eric Fusilier visible in a box at the margin of the slides would make it easier to follow the presentation. As I am a typical member of the ape family, eye contact helps me to focus my concentration. Anyway, thanks and greetings from Munich, Germany.
Hello i have an urgent question: When the plant life exploded in the carbonferous and the CO2 was reduced drasticly from the atmosphere, why did the temperatures not change? Only untill ~50 millions later with the Karoo ice age? At 18:40 it is said that the CO2 reduction is caused by the few cambrian plants and this lead to the Andean-Saharan glaciation. That is not only uncertain but unlikely in it's drastic effect and not in line with the jurassic CO2 decline with temperature rise for example. The cold itself is the major reductor of CO2 due to the absorbing oceans. The real reason for these drsatic temperature changes is the continetal distribution. When Antarctica left the south pole in the permian, the hot mesozoic began and when Antarctica turned back to the pole, our ice age began. Snow can not accumulate to large ice shields on the open seas.
There are many different factors that contribute to temperature changes globally, with the continents affecting ocean currents being only one of many. The main factors are usually atmospheric composition and milankovitch cycles, but there’s always nuance to every natural phenomenon.
@@ethannelson8592 Ok. But if one tries to find out what is the most dominant factor with an ockham razor atempt, i think it is clear that the continental distribution comes first. The Karoo ice age ends with Antarctica moving north, eventually losing it`s ice, which peaks in cretaceous maximum seal level. Then Antacrtica moves back to the pole and our current ice age began. The Milankovic cycles are on the smaller scale, responsible for the interglacials within such ice age period.
@@nyoodmono4681 These same massive climatic changes happen more frequently than significant tectonic change, so no, I’d disagree. It plays a big part in some cases, but not even remotely close to the majority of the time.
@@ethannelson8592 You disagree but where? There is a warm Cambrium followed by the Andean Saharan glaciation, a warm devonian, followed by the Karoo ice age, then the warm mesozoic, followed by our pleistocene. It is either hothouse (norm) or ice age (exception). The changes within our holocene are not "massiv" including our recent warming.
Why not build a “Time Machine” that transports you to an alternate universe in which earth was still in the Jurassic. That way you’ll have the real deal XD
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Thank you for such an exhaustive presentation! Here I mark some episodes just for ease.
01:17 The floor is given to Eric Fuselier.
01:58 Geological units of time.
03:03 Archean eon, Beginning of Life on Earth. Stromatolites.
05:05 Photosynthesis: cyanobacteria, purple sulfur bacteria.
07:03 Proterozoic eon, Great oxidation event.
08:32 Eukaryotes, Primary endosymbiosis.
10:11 Green algae. Charophyta. Proterocladus antiquus.
11:38 Phanerozoic eon. Paleozoic era.
12:49 Cambrian period.
14:26 Girvanella fossil (porostromate cyanobacteria).
15:16 Ordovician period.
16:30 First land plants were sporophytes. Spores typical of Bryophytes.
18:20 Late Ordovician mass extinction.
19:06 Silurian period.
20:36 Appearence of vascular plants. Tracheaphytes: Cooksonia, Salopella.
24:58 Devonian period.
27:15 Aglaophyton. Rhyniophyta. Trimerophytes: Psilophyton.
29:55 First trees: Progymnosperms, Cladoxylopsida, Wattieza, Archaeopteris, Callixylon.
36:04 Polypodiophyta (ferns).
37:26 Developing roots. Late Devonian extinction as a consequence.
38:24 Carboniferous period.
40:54 Equisetidae. Calamites.
43:49 Lepidodendrales: Lepidodendron, Lepidofloios, Sigillaria.
49:06 Seed plants (spermatophytes): Seed ferns (pteridospermatophyta), Alethopteris.
51:40 Mid carboniferous.
52:34 Gymnosperms: Conifers (Walchia).
53:57 Permian period.
55:57 Ginkgos. Cycads. Gnetophytes. Glossopteridales. Conifers: Voltzealeans.
58:58 Extinction of Progymnosperms. Mass extinction at the Permian-Triassic transition.
1:00:00 Mezozoic era, age of Cycads.
1:00:44 Triassic period. Permian extinction consequences and recovering.
1:02:11 Bennettitales: Williamsoniaceae. Conifers. Tree ferns.
1:03:32 Jurassic period.
1:05:35 Conifers: Araucariaceae, Cephalotaxacea, Pinaceae, Podocarpacea, Taxaceae, Taxodiaxeae.
1:07:43 Probably the earliest Angiosperm found: Nanjinganthus.
1:08:57 Cretaceous period.
1:10:30 Gnetophyta. Angiosperms: Magnoliophyta, Archaefructus, Operculifructus lopezii.
1:13:07 Amber.
1:14:43 Ferns: Tempskya (tree), modern ones.
1:16:16 Trees: Magnolias, Sycamores, Sycads (decline), Conifers (decline): Metasequoia.
1:17:44 Cenozoic era. Cretaceous-Paleogene extinction event. Age of savannas starts.
1:20:55 Paleogene period.
1:21:31 Paleocene: Acer, Zizyphoides flabellum. Eocene: desiduous forests and grasses. Oligocene: modern terrestrial ecosystems are forming.
1:26:53 Neogene period.
1:27:56 Modern seed plants. Grasses spreading. Fossils: Pinus, Podogonium knorri, Zelkova zelkovifolia, Taxodium dubium.
1:31:58 Quaternary period (Antropogen). Age of flowers.
1:32:59 Modern gymnosperms. Modern Tree ferns. Gnetophyta.
1:33:47 Supplemental reading.
1:35:37 Questions.
Thank you so much! We've added this information to the video caption.
The picture in 16.30 from early Devonian, painted by Z.Burian, was the first picture about paleozoic plants I have ever seen.
It was in an old paleo book from the 1950s wich belonged my grandpa, but I loved it! Of course there were a lot of wrong things in this book, so all the Silurian and early Devonian plants were called by the same name "psilophytales". But there were many beautiful pictures from the Devonian and Carboniferous in this old book, and they made me getting interested in paleontology and paleobotanic.
And the Carboniferous is still one of my most favourite periods in earth history, I would love to have some of the trees like sigillaria or lepidodendron in my garden.
And also some Devonian plants, like Asteroxylon or archeosigillaria....😊
I would also like to know more about the Evolution of the angiosperms in the mesozoic, but there are still a lot of unclear things I guess...
Best wishes to you all from Germany, and I hope to see more of your videos!
Great lecture! Thx
Thank you so much, Eric et al. I learned a lot. 🙏
Thank you sir.For this informative video..Respect from Bangladesh...❤
Lecture catering to my current interest. I was specially interested of Devonian plants. Carboniferous had also fascinating shapes.
I just love listening to these kinds of videos
Really great paleobotany presentation. Also, I had not heard of the fungal infestation defence of warm blooded animals before.
Well done, interesting. Thank you, I will save it for reference.
That was fascinating! Just one point of critique; To have the Eric Fusilier visible in a box at the margin of the slides would make it easier to follow the presentation. As I am a typical member of the ape family, eye contact helps me to focus my concentration. Anyway, thanks and greetings from Munich, Germany.
The universe seems to have provided everything needed for the development of life on all levels.
He's tricky like that, that Jesus.
So interesting ! Thank you.
Hello i have an urgent question: When the plant life exploded in the carbonferous and the CO2 was reduced drasticly from the atmosphere, why did the temperatures not change? Only untill ~50 millions later with the Karoo ice age? At 18:40 it is said that the CO2 reduction is caused by the few cambrian plants and this lead to the Andean-Saharan glaciation. That is not only uncertain but unlikely in it's drastic effect and not in line with the jurassic CO2 decline with temperature rise for example. The cold itself is the major reductor of CO2 due to the absorbing oceans. The real reason for these drsatic temperature changes is the continetal distribution. When Antarctica left the south pole in the permian, the hot mesozoic began and when Antarctica turned back to the pole, our ice age began. Snow can not accumulate to large ice shields on the open seas.
There are many different factors that contribute to temperature changes globally, with the continents affecting ocean currents being only one of many. The main factors are usually atmospheric composition and milankovitch cycles, but there’s always nuance to every natural phenomenon.
@@ethannelson8592 Ok. But if one tries to find out what is the most dominant factor with an ockham razor atempt, i think it is clear that the continental distribution comes first. The Karoo ice age ends with Antarctica moving north, eventually losing it`s ice, which peaks in cretaceous maximum seal level. Then Antacrtica moves back to the pole and our current ice age began. The Milankovic cycles are on the smaller scale, responsible for the interglacials within such ice age period.
@@nyoodmono4681 These same massive climatic changes happen more frequently than significant tectonic change, so no, I’d disagree. It plays a big part in some cases, but not even remotely close to the majority of the time.
@@ethannelson8592 You disagree but where? There is a warm Cambrium followed by the Andean Saharan glaciation, a warm devonian, followed by the Karoo ice age, then the warm mesozoic, followed by our pleistocene. It is either hothouse (norm) or ice age (exception). The changes within our holocene are not "massiv" including our recent warming.
@@nyoodmono4681 You skipped a few dozen other warming and cooling events, as well as the intermediate periods😂😂
Imagine rummaging through boxes and boxes of plant fossils, and helping yourself to whichever one you fancy.
Why not build a “Time Machine” that transports you to an alternate universe in which earth was still in the Jurassic. That way you’ll have the real deal XD
@thejdmguru621 All life exists at the same time, yet dimensions aren't hindered by such.......but, the real question is, Honda? Lol.
👍⭐⭐⭐⭐⭐
Geeks lecture better than the professionals🤔
Didn't even talk about the plants of the ediacarin period