From: owner-ammf-digest@smoe.org (alt.music.moxy-fruvous digest) To: ammf-digest@smoe.org Subject: alt.music.moxy-fruvous digest V14 #9172 Reply-To: ammf@fruvous.com Sender: owner-ammf-digest@smoe.org Errors-To: owner-ammf-digest@smoe.org Precedence: bulk alt.music.moxy-fruvous digest Friday, June 24 2022 Volume 14 : Number 9172 Today's Subjects: ----------------- Shopper, You can qualify to get a $90 Moderna gift card! ["Moderna Shoppe] What Happened When I Stopped Using Skin Care Products ["Skin Rejuvenation] The Fungal Nuker Secret Is Here ["Anti-Fungal Medication" Subject: Shopper, You can qualify to get a $90 Moderna gift card! Shopper, You can qualify to get a $90 Moderna gift card! http://originato.za.com/scLjKdBzjWlBDu3tscbdfIxY2vzdXujQ__VZ17UoAvxHjLQqmg http://originato.za.com/EMtEQEUSVWF27pXJgV43hEuZ00w4ICkzR0ObVOjfEsXbXUtnpA ough they differ from Viridiplantae in the pigments which are used in photosynthesis and so are different in colour. These groups also differ from green plants in that the storage polysaccharide is floridean starch and is stored in the cytoplasm rather than in the plastids. They appear to have had a common origin with Viridiplantae and the three groups form the clade Archaeplastida, whose name implies that their chloroplasts were derived from a single ancient endosymbiotic event. This is the broadest modern definition of the term 'plant'. In contrast, most other algae (e.g. brown algae/diatoms, haptophytes, dinoflagellates, and euglenids) not only have different pigments but also have chloroplasts with three or four surrounding membranes. They are not close relatives of the Archaeplastida, presumably having acquired chloroplasts separately from ingested or symbiotic green and red algae. They are thus not included in even the broadest modern definition of the plant kingdom, although they were in the past. The green plants or Viridiplantae were traditionally divided into the green algae (including the stoneworts) and the land plants. However, it is now known that the land plants evolved from within a group of green algae, so that the green algae by themselves are a ------------------------------ Date: Thu, 23 Jun 2022 09:38:45 -0400 From: "Skin Rejuvenation" Subject: What Happened When I Stopped Using Skin Care Products What Happened When I Stopped Using Skin Care Products http://instituto.za.com/fdpW9UYpHgFtzcRC9oEA9CxJlziJIQ1ZeX9JactvdCTSLxR-uw http://instituto.za.com/4HaGQd2C5q27pEAnxU2TFYGf37vtNNfoLvLk9iSYTgAjYnTrNw into increasingly more arid places, notably the vascular tissues xylem and phloem, that transport water and food throughout the organism. Root systems capable of obtaining soil water and nutrients also evolved during the Devonian. In modern vascular plants, the sporophyte is typically large, branched, nutritionally independent and long-lived, but there is increasing evidence that Paleozoic gametophytes were just as complex as the sporophytes. The gametophytes of all vascular plant groups evolved to become reduced in size and prominence in the life cycle. In seed plants, the microgametophyte is reduced from a multicellular free-living organism to a few cells in a pollen grain and the miniaturised megagametophyte remains inside the megasporangium, attached to and dependent on the parent plant. A megasporangium enclosed in a protective layer called an integument is known as an ovule. After fertilisation by means of sperm produced by pollen grains, an embryo sporophyte develops inside the ovule. The integument becomes a seed coat, and the ovule develops into a seed. Seed plants can survive and reproduce in extremely arid conditions, because they are not dependent on free water for the movement of sperm, or the development of free living gametophytes. The first seed plants, pteridosperms (seed ferns), now extinct, appeared in the Devonian and diversified through the Carboniferous. They were the ancestors of modern gymnosperms, of which four surviving groups are widespread today, particula ------------------------------ Date: Thu, 23 Jun 2022 09:18:26 -0400 From: "Anti-Fungal Medication" Subject: The Fungal Nuker Secret Is Here The Fungal Nuker Secret Is Here http://unterbal.ru.com/qbNDBE4bGKhw2djw3ZJa2KePqVmB1PoSVgkxm5altQqoo2bb http://unterbal.ru.com/_F8J8L8KNtLKLxPWY77UT4qMNjJkDs1Kx5j3AbIsnvkINwHIZw 50% solids (45% mineral and 5% organic matter), and 50% voids (or pores) of which half is occupied by water and half by gas. The percent soil mineral and organic content can be treated as a constant (in the short term), while the percent soil water and gas content is considered highly variable whereby a rise in one is simultaneously balanced by a reduction in the other. The pore space allows for the infiltration and movement of air and water, both of which are critical for life existing in soil. Compaction, a common problem with soils, reduces this space, preventing air and water from reaching plant roots and soil organisms. Given sufficient time, an undifferentiated soil will evolve a soil profile which consists of two or more layers, referred to as soil horizons. These differ in one or more properties such as in their texture, structure, density, porosity, consistency, temperature, color, and reactivity. The horizons differ greatly in thickness and generally lack sharp boundaries; their development is dependent on the type of parent material, the processes that modify those parent materials, and the soil-forming factors that influence those processes. The biological influences on soil properties are strongest near the surface, though the geochemical in ------------------------------ Date: Thu, 23 Jun 2022 05:20:33 -0400 From: "Family Savings" Subject: Walmart Knows Rewards! Get your $90 Here! Walmart Knows Rewards! Get your $90 Here! http://originato.za.com/ZbsAO8MiKbQ5tymRbSAF39duv8F19SsTwbG_NOTEAT1Ty_9aGg http://originato.za.com/MInhtU-BAZlia-fk21U5usKJT7jc8Z6WuEvawEvUmPOJp0Fuow hings were traditionally placed into one of two groups, plants and animals. This classification may date from Aristotle (384 BC b 322 BC), who made the distinction between plants, which generally do not move, and animals, which often are mobile to catch their food. Much later, when Linnaeus (1707b1778) created the basis of the modern system of scientific classification, these two groups became the kingdoms Vegetabilia (later Metaphyta or Plantae) and Animalia (also called Metazoa). Since then, it has become clear that the plant kingdom as originally defined included several unrelated groups, and the fungi and several groups of algae were removed to new kingdoms. However, these organisms are still sometimes considered plants, particularly in informal contexts.[citation needed] The term "plant" generally implies the possession of the following traits: multicellularity, possession of cell walls containing cellulose, and the ability to carry out photosynthesis with primary chloroplasts ------------------------------ Date: Thu, 23 Jun 2022 07:04:38 -0400 From: "Word Of Mouth" Subject: Whatâs your address? (amazing new device for you) Whatbs your address? (amazing new device for you) http://expatrong.ru.com/f0H52x2wWfs2twjDotymodEYWjZjbsYtJYCCLPskxYS4azRj8A http://expatrong.ru.com/IGh9-kY-vYlhICXlKMqiwRsg8B2PbOR3MkY6fgvIB2w8c3VOrw m formed on the land 1,200 million years ago, but it was not until the Ordovician Period, around 450 million years ago, that land plants appeared. However, new evidence from the study of carbon isotope ratios in Precambrian rocks has suggested that complex photosynthetic plants developed on the earth over 1000 m.y.a. For more than a century it has been assumed that the ancestors of land plants evolved in aquatic environments and then adapted to a life on land, an idea usually credited to botanist Frederick Orpen Bower in his 1908 book The Origin of a Land Flora. A recent alternative view, supported by genetic evidence, is that they evolved from terrestrial single-celled algae, and that even the common ancestor of red and green algae, and the unicellular freshwater algae glaucophytes, originated in a terrestrial environment in freshwater biofilms or microbial mats. Primitive land plants began to diversify in the late Silurian Period, around 420 million years ago, and the results of their diversification are displayed in remarkable detail in an early Devonian fossil assemblage from the Rhynie chert. This chert preserved early plants in cellular detail, petrified in volcanic springs. By the middle of the Devonian Period most of the features recognised in plants today are present, including roots, leaves and secondary wood, and by late Devonian times seeds had evolved. Late Devonian plants had thereby reached a degree of sophistication that allowed them to form forests of tall trees. Evolutionary innovation continued in the Carboniferous and later geological periods and is ongoing today. Most plant groups were relatively unscathed by the Permo-Triassic extinction event, although the structures of communities changed. This may have set the scene for the evolution of flowering plants in the Triassic (~200 million years ago), which exploded in the Cretaceous and Tertiary. The latest major group of plants to evolve were the grasses, which became important in the mid Tertiary, from around ------------------------------ Date: Thu, 23 Jun 2022 10:32:57 -0400 From: "Work From Home Job Quiz" Subject: $1,000/week YouTube job match $1,000/week YouTube job match http://seroy.za.com/-vTzWg574p1thM7e8d-JefUzSCHyX375JS9qkvPMHHFDU4eldg http://seroy.za.com/Q-OSPNKbdOUyvBn7q3k1kBz9bbJna3VJqh73ruwmd-K6ODl-5Q ar plant Cooksonia in mid-Silurian and the much larger and more complex lycophyte Baragwanathia longifolia in late Silurian. From the early Devonian Rhynie chert, detailed fossils of lycophytes and rhyniophytes have been found that show details of the individual cells within the plant organs and the symbiotic association of these plants with fungi of the order Glomales. The Devonian period also saw the evolution of leaves and roots, and the first modern tree, Archaeopteris. This tree with fern-like foliage and a trunk with conifer-like wood was heterosporous producing spores of two different sizes, an early step in the evolution of seeds. The Coal measures are a major source of Paleozoic plant fossils, with many groups of plants in existence at this time. The spoil heaps of coal mines are the best places to collect; coal itself is the remains of fossilised plants, though structural detail of the plant fossils is rarely visible in coal. In the Fossil Grove at Victoria Park in Glasgow, Scotland, the stumps of Lepidodendron trees are found in their original growth positions. The fossilized remains of conifer and angiosperm roots, stems and branches may be locally abundant in lake and inshore sedimentary rocks from the Mesozoic and Cenozoic eras. Sequoia and its allies, magn ------------------------------ End of alt.music.moxy-fruvous digest V14 #9172 **********************************************