Aarle-Rixtel is a village in the Dutch municipality of Laarbeek in North Brabant . It lies about 4 km north of Helmond . Since the municipal reorganization of 1968 the castle Croy is part of Aarle-Rixtel.
117-568: Aarle was first mentioned in 1249 as Arleh, and means "open forest with maple trees". Rixtel was first mentioned in 1179 as Ricstelle. The etymology is unknown. The villages developed in the Middle Ages along the Aa River . The two villages merged into a single entity. Aarle used to be a site of pilgrimage, and had a church, guesthouse, monastery and an inn . The Chapel of Our Lady in the Sand
234-483: A "nutlet" attached to a flattened wing of fibrous, papery tissue. They are shaped to spin as they fall and to carry the seeds a considerable distance on the wind. People often call them "helicopters" due to the way that they spin as they fall. During World War II, the US Army developed a special airdrop supply carrier that could carry up to 65 pounds (29 kg) of supplies and was based on the maple seed. Seed maturation
351-735: A climate similar to the Pacific Northwest . On the Alaska North Slope , Metasequoia was the dominant conifer. Much of the diversity represented migrants from nearer the equator. Deciduousness was dominant, probably to conserve energy by retroactively shedding leaves and retaining some energy rather than having them die from frostbite. In south-central Alaska, the Chickaloon Formation preserves peat-forming swamps dominated by taxodiaceous conifers and clastic floodplains occupied by angiosperm–conifer forests. At
468-537: A defined deep-water thermocline (a warmer mass of water closer to the surface sitting on top of a colder mass nearer the bottom) persisting throughout the epoch. The Atlantic foraminifera indicate a general warming of sea surface temperature–with tropical taxa present in higher latitude areas–until the Late Paleocene when the thermocline became steeper and tropical foraminifera retreated back to lower latitudes. Early Paleocene atmospheric CO 2 levels at what
585-622: A depth of about 1,000 m (3,300 ft). The Danian deposits are sequestered into the Aitzgorri Limestone Formation , and the Selandian and early Thanetian into the Itzurun Formation . The Itzurun Formation is divided into groups A and B corresponding to the two stages respectively. The two stages were ratified in 2008, and this area was chosen because of its completion, low risk of erosion, proximity to
702-600: A fossil record extending back to the middle Paleocene in North America. The oldest known fossils of Acer are from the late Paleocene of Northeast Asia and northern North America, around 60 million years old. The oldest fossils of Acer in Europe are from Svalbard , dating to the late Eocene ( Priabonian ~38–34 million years ago). Most maples or acers are trees growing to a height of 10–45 m (33–148 ft). Others are shrubs less than 10 meters tall with
819-662: A higher rate than deciduous angiosperms as deciduous plants can become dormant in harsh conditions. In the Gulf Coast, angiosperms experienced another extinction event during the PETM, which they recovered quickly from in the Eocene through immigration from the Caribbean and Europe. During this time, the climate became warmer and wetter, and it is possible that angiosperms evolved to become stenotopic by this time, able to inhabit
936-1035: A lobe, one of which is central or apical. A small number of species differ in having palmate compound, pinnate compound, pinnate veined or unlobed leaves. Several species, including Acer griseum (paperbark maple), Acer mandshuricum (Manchurian maple), Acer maximowiczianum (Nikko maple) and Acer triflorum (three-flowered maple), have trifoliate leaves. One species, Acer negundo (box-elder or Manitoba maple), has pinnately compound leaves that may be simply trifoliate or may have five, seven, or rarely nine leaflets. A few, such as Acer laevigatum (Nepal maple) and Acer carpinifolium (hornbeam maple), have pinnately veined simple leaves. Maple species, such as Acer rubrum , may be monoecious , dioecious or polygamodioecious . The flowers are regular, pentamerous , and borne in racemes , corymbs , or umbels . They have four or five sepals , four or five petals about 1–6 mm long (absent in some species), four to ten stamens about 6–10 mm long, and two pistils or
1053-441: A narrow range of temperature and moisture; or, since the dominant floral ecosystem was a highly integrated and complex closed-canopy rainforest by the middle Paleocene, the plant ecosystems were more vulnerable to climate change . There is some evidence that, in the Gulf Coast, there was an extinction event in the late Paleocene preceding the PETM, which may have been due to the aforementioned vulnerability of complex rainforests, and
1170-477: A number of small trunks originating at about ground level. Most species are deciduous , and many are renowned for their autumn leaf colours , but a few in southern Asia and the Mediterranean region are mostly evergreen . Most are shade-tolerant when young and are often riparian, understory, or pioneer species rather than climax overstory trees. There are a few exceptions such as sugar maple . Many of
1287-724: A pistil with two styles. The ovary is superior and has two carpels , whose wings elongate the flowers, making it easy to tell which flowers are female. Maples flower in late winter or early spring , in most species with or just after the appearance of the leaves, but in some before the trees leaf out. Maple flowers are green, yellow, orange or red. Though individually small, the effect of an entire tree in flower can be striking in several species. Some maples are an early spring source of pollen and nectar for bees . The distinctive fruits are called samaras , "maple keys", "helicopters", "whirlybirds" or "polynoses". These seeds occur in distinctive pairs each containing one seed enclosed in
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#17327824515791404-792: A problem for mowing lawns. Particularly popular are Norway maple (although it is considered invasive in North America), silver maple , Japanese maple , and red maple . The vine maple is also occasionally used as an ornamental tree. Other maples, especially smaller or more unusual species, are popular as specimen trees. Numerous maple cultivars that have been selected for particular characteristics can be propagated only by asexual reproduction such as cuttings, tissue culture , budding or grafting . Acer palmatum (Japanese maple) alone has over 1,000 cultivars, most selected in Japan, and many of them no longer propagated or not in cultivation in
1521-424: A short time frame. The freezing temperatures probably reversed after three years and returned to normal within decades, sulfuric acid aerosols causing acid rain probably dissipated after 10 years, and dust from the impact blocking out sunlight and inhibiting photosynthesis would have lasted up to a year though potential global wildfires raging for several years would have released more particulates into
1638-778: A single formation (a stratotype ) identifying the lower boundary of the stage. In 1989, the ICS decided to split the Paleocene into three stages: the Danian, Selandian, and Thanetian. The Danian was first defined in 1847 by German-Swiss geologist Pierre Jean Édouard Desor based on the Danish chalks at Stevns Klint and Faxse , and was part of the Cretaceous, succeeded by the Tertiary Montian Stage. In 1982, after it
1755-841: Is a geological epoch that lasted from about 66 to 56 million years ago (mya). It is the first epoch of the Paleogene Period in the modern Cenozoic Era . The name is a combination of the Ancient Greek παλαιός palaiós meaning "old" and the Eocene Epoch (which succeeds the Paleocene), translating to "the old part of the Eocene". The epoch is bracketed by two major events in Earth's history. The K–Pg extinction event , brought on by an asteroid impact ( Chicxulub impact ) and possibly volcanism ( Deccan Traps ), marked
1872-688: Is a major producer of maple syrup, an industry worth about 500 million Canadian dollars annually. Also, as these trees are a major source of pollen in early spring before many other plants have flowered, maple flowers are a source of foraging for honeybees that play a commercially important role in general agriculture and in natural habitats. Maple is used as pulpwood . The fibers have relatively thick walls that prevent collapsing upon drying. This gives good bulk and opacity in paper . Maple also gives paper good printing properties. Many maples have bright autumn foliage , and many countries have leaf-watching traditions. The sugar maple ( Acer saccharum )
1989-400: Is a pilgrimage site which was built around 1500. It was rebuilt in 1597. In 1846, it was converted into town hall, but became a chapel again in 1853. In 1969, it was restored and made symmetrical again. There is a little 16th-century Mary statue inside in the chapel which allegedly has performed miracles. The Our Lady Presentation Church was built between 1844 and 1846 in neoclassic style and
2106-437: Is also evidence this occurred again 300,000 years later in the early Thanetian dubbed MPBE-2. Respectively, about 83 and 132 gigatons of methane-derived carbon were ejected into the atmosphere, which suggests a 2–3 °C (3.6–5.4 °F) rise in temperature, and likely caused heightened seasonality and less stable environmental conditions. It may have also caused an increase of grass in some areas. From 59.7 to 58.1 Ma, during
2223-537: Is controversial, but most likely about 2,500 years. This carbon also interfered with the carbon cycle and caused ocean acidification, and potentially altered and slowed down ocean currents, the latter leading to the expansion of oxygen minimum zones (OMZs) in the deep sea. In surface water, OMZs could have also been caused from the formation of strong thermoclines preventing oxygen inflow, and higher temperatures equated to higher productivity leading to higher oxygen usurpation. Further, expanding OMZs could have caused
2340-435: Is now Castle Rock , Colorado, were calculated to be between 352 and 1,110 parts per million (ppm), with a median of 616 ppm. Based on this and estimated plant-gas exchange rates and global surface temperatures, the climate sensitivity was calculated to be +3 °C when CO 2 levels doubled, compared to 7 °C following the formation of ice at the poles. CO 2 levels alone may have been insufficient in maintaining
2457-556: Is now the Mediterranean Sea tropical. South-central North America had a humid, monsoonal climate along its coastal plain, but conditions were drier to the west and at higher altitudes. Svalbard was temperate, having a mean temperature of 19.2 ± 2.49 °C during its warmest month and 1.7 ± 3.24 °С during its coldest. Global deep water temperatures in the Paleocene likely ranged from 8–12 °C (46–54 °F), compared to 0–3 °C (32–37 °F) in modern day. Based on
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#17327824515792574-500: Is often used for the smoking of food. Charcoal from maples is an integral part of the Lincoln County Process used to make Tennessee whiskey . They are also cultivated as ornamental plants and have benefits for tourism and agriculture . Some of the larger maple species have valuable timber , particularly Sugar maple in North America and Sycamore maple in Europe. Sugar maple wood—often known as "hard maple"—is
2691-478: Is one of the finest examples of a so-called waterstaatskerk [ nl ] , churches built by the Rijkswaterstaat (Department of Public Works). It was remodelled between 1896 and 1897 by Joseph Cuypers . Croy Castle was built in the 15th century as a summer residence. The gate with the two towers date from 1500 and were restored in 1790. The last residence was Constance van der Bruggen who left
2808-400: Is placed in the subfamily Hippocastanoideae . The genus is subdivided by its morphology into a multitude of sections and subsections. Molecular studies incorporating DNA sequence data from both chloroplast and nuclear genomes, aiming to resolve the internal relationships and reconstruct the evolutionairy history of the group, suggest a Late Paleocene origin for the group, appearing first in
2925-458: Is sought for fine woodworking. Some maple wood has a highly decorative wood grain , known as flame maple , quilt maple , birdseye maple and burl wood . This condition occurs randomly in individual trees of several species and often cannot be detected until the wood has been sawn, though it is sometimes visible in the standing tree as a rippled pattern in the bark. These select decorative wood pieces also have subcategories that further filter
3042-670: Is the primary contributor to fall " foliage season " in north-eastern North America . In Japan , the custom of viewing the changing colour of maples in the autumn is called momijigari . Nikkō and Kyoto are particularly favoured destinations for this activity. In Korea, the same viewing activity is called danpung-nori and the Seoraksan and Naejang-san mountains are among the best-known destinations. Paleocene The Paleocene ( IPA : / ˈ p æ l i . ə s iː n , - i . oʊ -, ˈ p eɪ l i -/ PAL -ee-ə-seen, -ee-oh-, PAY -lee- ), or Palaeocene ,
3159-481: Is the standard maple bat most in use by professional baseball. Maple is also commonly used in archery as the core material in the limbs of a recurve bow due to its stiffness and strength. Maple wood is often graded based on physical and aesthetic characteristics. The most common terminology includes the grading scale from common #2; which is unselected and often used for craft woods; common #1, used for commercial and residential buildings; clear; and select grade, which
3276-654: Is used in numerous musical instruments . Maple is harder and has a brighter sound than mahogany , which is another major tonewood used in instrument manufacturing. The back, sides, and neck of most violins , violas , cellos , and double basses are made from maple. Electric guitar necks are commonly made from maple, having good dimensional stability. The necks of the Fender Stratocaster and Telecaster were originally an entirely maple one piece neck, but later were also available with rosewood fingerboards. Les Paul desired an all maple guitar, but due to
3393-425: Is usually in a few weeks to six months after flowering, with seed dispersal shortly after maturity. However, one tree can release hundreds of thousands of seeds at a time. Depending on the species, the seeds can be small and green to orange and big with thicker seed pods. The green seeds are released in pairs, sometimes with the stems still connected. The yellow seeds are released individually and almost always without
3510-548: Is why the GSSP was moved to Zumaia. Today, the beginning of the Selandian is marked by the appearances of the nannofossils Fasciculithus tympaniformis , Neochiastozygus perfectus , and Chiasmolithus edentulus , though some foraminifera are used by various authors. The Thanetian was first proposed by Swiss geologist Eugène Renevier , in 1873; he included the south England Thanet , Woolwich , and Reading formations. In 1880, French geologist Gustave Frédéric Dollfus narrowed
3627-820: The Antarctic Peninsula . In the Paleocene, the waterways between the Arctic Ocean and the North Atlantic were somewhat restricted, so North Atlantic Deep Water (NADW) and the Atlantic Meridional Overturning Circulation (AMOC)—which circulates cold water from the Arctic towards the equator—had not yet formed, and so deep water formation probably did not occur in the North Atlantic. The Arctic and Atlantic would not be connected by sufficiently deep waters until
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3744-826: The Caribbean Plate ), which had formed from the Galápagos hotspot in the Pacific in the latest Cretaceous, was moving eastward as the North American and South American plates were getting pushed in the opposite direction due to the opening of the Atlantic ( strike-slip tectonics ). This motion would eventually uplift the Isthmus of Panama by 2.6 mya. The Caribbean Plate continued moving until about 50 mya when it reached its current position. The components of
3861-826: The Cretaceous Period and the Mesozoic Era , and initiated the Cenozoic Era and the Paleogene Period. It is divided into three ages : the Danian spanning 66 to 61.6 million years ago (mya), the Selandian spanning 61.6 to 59.2 mya, and the Thanetian spanning 59.2 to 56 mya. It is succeeded by the Eocene. The K–Pg boundary is clearly defined in the fossil record in numerous places around
3978-549: The Holarctic region (comprising most of the Northern Hemisphere) was mainly early members of Ginkgo , Metasequoia , Glyptostrobus , Macginitiea , Platanus , Carya , Ampelopsis , and Cercidiphyllum . Patterns in plant recovery varied significantly with latitude , climate, and altitude. For example, what is now Castle Rock, Colorado featured a rich rainforest only 1.4 million years after
4095-536: The Paleocene–Eocene thermal maximum , a short period of intense warming and ocean acidification brought about by the release of carbon en masse into the atmosphere and ocean systems, which led to a mass extinction of 30–50% of benthic foraminifera –planktonic species which are used as bioindicators of the health of a marine ecosystem—one of the largest in the Cenozoic. This event happened around 55.8 mya, and
4212-809: The Quaternary from the Tertiary in 1829; and Scottish geologist Charles Lyell (ignoring the Quaternary) had divided the Tertiary Epoch into the Eocene , Miocene , Pliocene , and New Pliocene ( Holocene ) Periods in 1833. British geologist John Phillips had proposed the Cenozoic in 1840 in place of the Tertiary, and Austrian paleontologist Moritz Hörnes had introduced the Paleogene for
4329-520: The Southern Hemisphere . The type species of the genus is the sycamore maple Acer pseudoplatanus , one of the most common maple species in Europe. Most maples usually have easily identifiable palmate leaves (with a few exceptions, such as Acer carpinifolium , Acer laurinum , and Acer negundo ) and all share distinctive winged fruits . The closest relative of the maples is the small east Asian genus Dipteronia , followed by
4446-530: The Transantarctic Mountains . The poles probably had a cool temperate climate; northern Antarctica, Australia, the southern tip of South America, what is now the US and Canada, eastern Siberia, and Europe warm temperate; middle South America, southern and northern Africa, South India, Middle America, and China arid; and northern South America, central Africa, North India, middle Siberia, and what
4563-647: The Western world . Some delicate cultivars are usually grown in pots and rarely reach heights of more than 50–100 cm. Maples are a popular choice for the art of bonsai . Japanese maple ( Acer palmatum ), trident maple ( A. buergerianum ), Amur maple ( A. ginnala ), field maple ( A. campestre ) and Montpellier maple ( A. monspessulanum ) are popular choices and respond well to techniques that encourage leaf reduction and ramification , but most species can be used. Maple collections, sometimes called aceretums , occupy space in many gardens and arboreta around
4680-847: The opening of the North Atlantic Ocean and seafloor spreading , the divergence of the Greenland Plate from the North American Plate , and, climatically, the PETM by dissociating methane clathrate crystals on the seafloor resulting in the mass release of carbon. North and South America remained separated by the Central American Seaway , though an island arc (the South Central American Arc) had already formed about 73 mya. The Caribbean Large Igneous Province (now
4797-401: The root systems are typically dense and fibrous, inhibiting the growth of other vegetation underneath them. A few species, notably Acer cappadocicum , frequently produce root sprouts , which can develop into clonal colonies . Maples are distinguished by opposite leaf arrangement. The leaves in most species are palmate veined and lobed, with 3 to 9 (rarely to 13) veins each leading to
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4914-496: The water column . Though the temperature in the latest Danian varied at about the same magnitude, this event coincides with an increase of carbon. About 60.5 mya at the Danian/Selandian boundary, there is evidence of anoxia spreading out into coastal waters, and a drop in sea levels which is most likely explained as an increase in temperature and evaporation, as there was no ice at the poles to lock up water. During
5031-584: The Østerrende Clay . The beginning of this stage was defined by the end of carbonate rock deposition from an open ocean environment in the North Sea region (which had been going on for the previous 40 million years). The Selandian deposits in this area are directly overlain by the Eocene Fur Formation —the Thanetian was not represented here—and this discontinuity in the deposition record
5148-437: The 1970s to the 1990s, maple drum kits were a vast majority of all drum kits made, but in recent years, birch has become popular for drums once again. Some of the best drum-building companies use maple extensively throughout their mid-pro range. Maple drums are favored for their bright resonant sound. Certain types of drum sticks are also made from maple. During late winter to early spring in northeastern North America , when
5265-831: The Canadian ice hockey team, the Toronto Maple Leafs . The first attested use of the word was in 1260 as "mapole", and it also appears a century later in Geoffrey Chaucer 's Canterbury Tales , spelled as "mapul". The maple is also a symbol of Hiroshima , ubiquitous in the local meibutsu . The maple leaf appears in the coat of arms of Sammatti , a former municipality of Uusimaa , Finland . Some species of maple are extensively planted as ornamental trees by homeowners, businesses, and municipalities due to their fall colour, relatively fast growth, ease of transplanting, and lack of hard seeds that would pose
5382-534: The Cretaceous, had receded. Between about 60.5 and 54.5 mya, there was heightened volcanic activity in the North Atlantic region—the third largest magmatic event in the last 150 million years—creating the North Atlantic Igneous Province . The proto- Iceland hotspot is sometimes cited as being responsible for the initial volcanism, though rifting and resulting volcanism have also contributed. This volcanism may have contributed to
5499-439: The Cretaceous, tropical or subtropical , and the poles were temperate , with an average global temperature of roughly 24–25 °C (75–77 °F). For comparison, the average global temperature for the period between 1951 and 1980 was 14 °C (57 °F). The latitudinal temperature gradient was approximately 0.24 °C per degree of latitude. The poles also lacked ice caps, though some alpine glaciation did occur in
5616-635: The Eocene and Neogene for the Miocene and Pliocene in 1853. After decades of inconsistent usage, the newly formed International Commission on Stratigraphy (ICS), in 1969, standardized stratigraphy based on the prevailing opinions in Europe: the Cenozoic Era subdivided into the Tertiary and Quaternary sub-eras, and the Tertiary subdivided into the Paleogene and Neogene Periods. In 1978, the Paleogene
5733-473: The Eocene". The Eocene, in turn, is derived from Ancient Greek eo— eos ἠώς meaning "dawn", and—cene kainos καινός meaning "new" or "recent", as the epoch saw the dawn of recent, or modern, life. Paleocene did not come into broad usage until around 1920. In North America and mainland Europe, the standard spelling is "Paleocene", whereas it is "Palaeocene" in the UK. Geologist T. C. R. Pulvertaft has argued that
5850-723: The K–Pg boundary, the largest the Mexican Chicxulub crater whose impact was a major precipitator of the K–Pg extinction, and also the Ukrainian Boltysh crater , dated to 65.4 mya the Canadian Eagle Butte crater (though it may be younger), the Vista Alegre crater (though this may date to about 115 mya ). Silicate glass spherules along the Atlantic coast of the U.S. indicate a meteor impact in
5967-542: The Late Cretaceous became dominant trees in Patagonia, before going extinct. Some plant communities, such as those in eastern North America, were already experiencing an extinction event in the late Maastrichtian, particularly in the 1 million years before the K–Pg extinction event. The "disaster plants" that refilled the emptied landscape crowded out many Cretaceous plants, and resultantly, many went extinct by
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#17327824515796084-533: The Miocene about 24–17 mya. There is evidence that some plants and animals could migrate between India and Asia during the Paleocene, possibly via intermediary island arcs. In the modern thermohaline circulation , warm tropical water becomes colder and saltier at the poles and sinks ( downwelling or deep water formation) that occurs at the North Atlantic near the North Pole and the Southern Ocean near
6201-728: The Northern Component Waters by Greenland in the Eocene—the predecessor of the AMOC—may have caused an intense warming in the North Hemisphere and cooling in the Southern, as well as an increase in deep water temperatures. In the PETM, it is possible deep water formation occurred in saltier tropical waters and moved polewards, which would increase global surface temperatures by warming the poles. Also, Antarctica
6318-412: The Paleocene, especially at the end, in tandem with the increasing global temperature. At the North Pole, woody angiosperms had become the dominant plants, a reversal from the Cretaceous where herbs proliferated. The Iceberg Bay Formation on Ellesmere Island , Nunavut (latitude 75 – 80 ° N) shows remains of a late Paleocene dawn redwood forest, the canopy reaching around 32 m (105 ft), and
6435-473: The Paleocene, with a global average temperature of about 24–25 °C (75–77 °F), compared to 14 °C (57 °F) in more recent times, the Earth had a greenhouse climate without permanent ice sheets at the poles, like the preceding Mesozoic . As such, there were forests worldwide—including at the poles—but they had low species richness in regards to plant life, and were populated by mainly small creatures that were rapidly evolving to take advantage of
6552-413: The South Pole, due to the increasing isolation of Antarctica, many plant taxa were endemic to the continent instead of migrating down. Patagonian flora may have originated in Antarctica. The climate was much cooler than in the Late Cretaceous, though frost probably was not common in at least coastal areas. East Antarctica was likely warm and humid. Because of this, evergreen forests could proliferate as, in
6669-429: The Thanetian is best correlated with the C26r/C26n reversal. Several economically important coal deposits formed during the Paleocene, such as the sub-bituminous Fort Union Formation in the Powder River Basin of Wyoming and Montana, which produces 43% of American coal; the Wilcox Group in Texas, the richest deposits of the Gulf Coastal Plain ; and the Cerrejón mine in Colombia, the largest open-pit mine in
6786-427: The Turgai route connecting Europe with Asia (which were otherwise separated by the Turgai Strait at this time). The Laramide orogeny , which began in the Late Cretaceous, continued to uplift the Rocky Mountains ; it ended at the end of the Paleocene. Because of this and a drop in sea levels resulting from tectonic activity, the Western Interior Seaway , which had divided the continent of North America for much of
6903-649: The United States and Ontario, Canada. Maples are affected by a number of fungal diseases. Several are susceptible to Verticillium wilt caused by Verticillium species, which can cause significant local mortality. Sooty bark disease , caused by Cryptostroma species, can kill trees that are under stress due to drought . Death of maples can rarely be caused by Phytophthora root rot and Ganoderma root decay. Maple leaves in late summer and autumn are commonly disfigured by "tar spot" caused by Rhytisma species and mildew caused by Uncinula species, though these diseases do not usually have an adverse effect on
7020-438: The absence of frost and a low probability of leaves dying, it was more energy efficient to retain leaves than to regrow them every year. One possibility is that the interior of the continent favored deciduous trees, though prevailing continental climates may have produced winters warm enough to support evergreen forests. As in the Cretaceous, podocarpaceous conifers, Nothofagus , and Proteaceae angiosperms were common. In
7137-409: The aesthetic looks. Crotch wood, bees wing, cats paw, old growth and mottled are some terms used to describe the look of these decorative woods. Maples have a long history of use for furniture production in the United States. The Cherokee people would produce a purple dye from maple bark, which they used to dye cloth. Maple is considered a tonewood , or a wood that carries sound waves well, and
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#17327824515797254-422: The algae Discoaster and a diversification of Heliolithus , though the best correlation is in terms of paleomagnetism . A chron is the occurrence of a geomagnetic reversal —when the North and South poles switch polarities . Chron 1 (C1n) is defined as modern day to about 780,000 years ago, and the n denotes "normal" as in the polarity of today, and an r "reverse" for the opposite polarity. The beginning of
7371-507: The atmosphere. For the following half million years, the carbon isotope gradient—a difference in the C / C ratio between surface and deep ocean water, causing carbon to cycle into the deep sea—may have shut down. This, termed a "Strangelove ocean", indicates low oceanic productivity ; resultant decreased phytoplankton activity may have led to a reduction in cloud seeds and, thus, marine cloud brightening , causing global temperatures to increase by 6 °C ( CLAW hypothesis ). Following
7488-399: The beginning of the Paleocene and killed off 75% of species, most famously the non-avian dinosaurs. The end of the epoch was marked by the Paleocene–Eocene Thermal Maximum (PETM), which was a major climatic event wherein about 2,500–4,500 gigatons of carbon were released into the atmosphere and ocean systems, causing a spike in global temperatures and ocean acidification . In the Paleocene,
7605-418: The boundary; for example, in the Williston Basin of North Dakota, an estimated 1/3 to 3/5 of plant species went extinct. The K–Pg extinction event ushered in a floral turnover; for example, the once commonplace Araucariaceae conifers were almost fully replaced by Podocarpaceae conifers, and the Cheirolepidiaceae , a group of conifers that had dominated during most of the Mesozoic but had become rare during
7722-424: The continents of the Northern Hemisphere were still connected via some land bridges ; and South America, Antarctica, and Australia had not completely separated yet. The Rocky Mountains were being uplifted, the Americas had not yet joined, the Indian Plate had begun its collision with Asia, and the North Atlantic Igneous Province was forming in the third-largest magmatic event of the last 150 million years. In
7839-409: The country, with at least one in each province. Although the idea of the tree as a national symbol originally hailed from the province of Quebec where the sugar maple is significant, today's arboreal emblem of Canada rather refers to a generic maple. The design on the flag is an eleven-point stylization modeled after a sugar maple leaf (which normally bears 23 points). It is also in the name of
7956-559: The country. Paleocene coal has been mined extensively in Svalbard , Norway, since near the beginning of the 20th century, and late Paleocene and early Eocene coal is widely distributed across the Canadian Arctic Archipelago and northern Siberia. In the North Sea, Paleocene-derived natural gas reserves, when they were discovered, totaled approximately 2.23 trillion m (7.89 trillion ft ), and oil in place 13.54 billion barrels. Important phosphate deposits—predominantly of francolite —near Métlaoui , Tunisia were formed from
8073-404: The dark forest floor, and epiphytism where a plant grows on another plant in response to less space on the forest floor. Despite increasing density—which could act as fuel—wildfires decreased in frequency from the Cretaceous to the early Eocene as the atmospheric oxygen levels decreased to modern day levels, though they may have been more intense. There was a major die-off of plant species over
8190-405: The definition to just the Thanet Formation. The Thanetian begins a little after the mid-Paleocene biotic event —a short-lived climatic event caused by an increase in methane —recorded at Itzurun as a dark 1 m (3.3 ft) interval from a reduction of calcium carbonate . At Itzurun, it begins about 29 m (95 ft) above the base of the Selandian, and is marked by the first appearance of
8307-411: The early to middle Eocene. There is evidence of deep water formation in the North Pacific to at least a depth of about 2,900 m (9,500 ft). The elevated global deep water temperatures in the Paleocene may have been too warm for thermohaline circulation to be predominately heat driven. It is possible that the greenhouse climate shifted precipitation patterns, such that the Southern Hemisphere
8424-529: The ecosystem may have been disrupted by only a small change in climate. The warm Paleocene climate, much like that of the Cretaceous , allowed for diverse polar forests. Whereas precipitation is a major factor in plant diversity nearer the equator, polar plants had to adapt to varying light availability ( polar nights and midnight suns ) and temperatures. Because of this, plants from both poles independently evolved some similar characteristics, such as broad leaves. Plant diversity at both poles increased throughout
8541-403: The estate to the poor of Stiphout . A retirement home was established in the castle until 1977. In 1988, it became an office building. In 1840, Aarle was home to 701 people and Rixtel was home to 154 people. The former town hall was built in 1855 and consists of three blocks: a school, the town hall and the residence for the school teacher. Until the municipal reorganization of 1997, Aarle-Rixtel
8658-486: The event, probably due to a rain shadow effect causing regular monsoon seasons. Conversely, low plant diversity and a lack of specialization in insects in the Colombian Cerrejón Formation , dated to 58 mya, indicates the ecosystem was still recovering from the K–Pg extinction event 7 million years later. Flowering plants ( angiosperms ), which had become dominant among forest taxa by
8775-539: The extreme disruptions in the aftermath of the K-Pg extinction event, the relatively cool, though still greenhouse, conditions of the Late Cretaceous–Early Palaeogene Cool Interval (LKEPCI) that began in the Late Cretaceous continued. The Dan –C2 Event 65.2 mya in the early Danian spanned about 100,000 years, and was characterized by an increase in carbon, particularly in the deep sea. Since
8892-606: The former southern supercontinent Gondwanaland in the Southern Hemisphere continued to drift apart, but Antarctica was still connected to South America and Australia. Africa was heading north towards Europe, and the Indian subcontinent towards Asia, which would eventually close the Tethys Ocean . The Indian and Eurasian Plates began colliding in the Paleocene, with uplift (and a land connection) beginning in
9009-453: The greenhouse climate, and some positive feedbacks must have been active, such as some combination of cloud, aerosol, or vegetation related processes. A 2019 study identified changes in orbital eccentricity as the dominant drivers of climate between the late Cretaceous and the early Eocene. The effects of the meteor impact and volcanism 66 mya and the climate across the K–Pg boundary were likely fleeting, and climate reverted to normal in
9126-591: The greenstriped mapleworm ( Dryocampa rubicunda ), can feed on the leaves so much that they cause temporary defoliation of host maple trees. Aphids are also very common sap-feeders on maples. In horticultural applications a dimethoate spray will solve this. Infestations of the Asian long-horned beetle ( Anoplophora glabripennis ) have resulted in the destruction of thousands of maples and other tree species in Illinois, Massachusetts, New Jersey, New York, and Ohio in
9243-533: The last remaining Dutch bell foundry. Maple See either species grouped by sections alphabetical list of species Acer is a genus of trees and shrubs commonly known as maples . The genus is placed in the soapberry family Sapindaceae . There are approximately 132 species , most of which are native to Asia , with a number also appearing in Europe , northern Africa , and North America . Only one species, Acer laurinum , extends to
9360-482: The late Danian, there was a warming event and evidence of ocean acidification associated with an increase in carbon; at this time, there was major seafloor spreading in the Atlantic and volcanic activity along the southeast margin of Greenland. The Latest Danian Event, also known as the Top Chron C27n Event, lasted about 200,000 years and resulted in a 1.6–2.8 °C increase in temperatures throughout
9477-871: The late Paleocene to the early Eocene. Impact craters formed in the Paleocene include: the Connolly Basin crater in Western Australia less than 60 mya, the Texan Marquez crater 58 mya, the Greenlandic Hiawatha Glacier crater 58 mya, and possibly the Jordan Jabel Waqf as Suwwan crater which dates to between 56 and 37 mya. Vanadium -rich osbornite from the Isle of Skye , Scotland, dating to 60 mya may be impact ejecta . Craters were also formed near
9594-491: The late Selandian and early Thanetian, organic carbon burial resulted in a period of climatic cooling, sea level fall and transient ice growth. This interval saw the highest δ O values of the epoch. The Paleocene–Eocene Thermal Maximum was an approximately 200,000-year-long event where the global average temperature rose by some 5 to 8 °C (9 to 14 °F), and mid-latitude and polar areas may have exceeded modern tropical temperatures of 24–29 °C (75–84 °F). This
9711-478: The latter spelling is incorrect because this would imply either a translation of "old recent" or a derivation from "pala" and "Eocene", which would be incorrect because the prefix palæo- uses the ligature æ instead of "a" and "e" individually, so only both characters or neither should be dropped, not just one. The Paleocene Epoch is the 10 million year time interval directly after the K–Pg extinction event , which ended
9828-562: The mid- Maastrichtian , more and more carbon had been sequestered in the deep sea possibly due to a global cooling trend and increased circulation into the deep sea. The Dan–C2 event may represent a release of this carbon after deep sea temperatures rose to a certain threshold, as warmer water can dissolve less carbon. Alternatively, the cause of the Dan-C2 event may have been a pulse of Deccan Traps volcanism. Savanna may have temporarily displaced forestland in this interval. Around 62.2 mya in
9945-573: The mid-Palaeocene biotic event (MPBE), also known as the Early Late Palaeocene Event (ELPE), around 59 Ma (roughly 50,000 years before the Selandian/Thanetian boundary), the temperature spiked probably due to a mass release of the deep sea methane hydrate into the atmosphere and ocean systems. Carbon was probably output for 10–11,000 years, and the aftereffects likely subsided around 52–53,000 years later. There
10062-399: The middle Cretaceous 110–90 mya, continued to develop and proliferate, more so to take advantage of the recently emptied niches and an increase in rainfall. Along with them coevolved the insects that fed on these plants and pollinated them. Predation by insects was especially high during the PETM. Many fruit-bearing plants appeared in the Paleocene in particular, probably to take advantage of
10179-432: The middle Paleocene. The strata immediately overlaying the K–Pg extinction event are especially rich in fern fossils. Ferns are often the first species to colonize areas damaged by forest fires , so this " fern spike " may mark the recovery of the biosphere following the impact (which caused blazing fires worldwide). The diversifying herb flora of the early Paleocene either represent pioneer species which re-colonized
10296-563: The more widespread genus Aesculus (buckeyes and horse-chestnuts). Maple syrup is made from the sap of some maple species. It is one of the most common genera of trees in Asia. Many maple species are grown in gardens where they are valued for their autumn colour and often decorative foliage, some also for their attractive flowers, fruit, or bark. The closest relative of Acer is Dipteronia , which only has two living species in China, but has
10413-604: The newly evolving birds and mammals for seed dispersal . In what is now the Gulf Coast , angiosperm diversity increased slowly in the early Paleocene, and more rapidly in the middle and late Paleocene. This may have been because the effects of the K–Pg extinction event were still to some extent felt in the early Paleocene, the early Paleocene may not have had as many open niches, early angiosperms may not have been able to evolve at such an accelerated rate as later angiosperms, low diversity equates to lower evolution rates, or there
10530-599: The night-to-day temperatures change from freezing to thawing, maple trees may be tapped for sap to manufacture maple syrup . The sap is sent via tubing to a sugar house where it is boiled to produce syrup or made into maple sugar or maple taffy . It takes about 40 litres (42 US qt) of sugar maple sap to make 1 litre (1.1 US qt) of syrup. While any Acer species may be tapped for syrup, many do not have sufficient quantities of sugar to be commercially useful, whereas sugar maples ( A. saccharum ) are most commonly used to produce maple syrup. Québec, Canada
10647-619: The northeastern Palearctic. Rapid lineage divergence was followed by several independent dispersals to the Nearctic and Western Palearctic regions. Fifty-four species of maples meet the International Union for Conservation of Nature criteria for being under threat of extinction in their native habitat. The leaves are used as a food plant for the larvae of a number of the order Lepidoptera (see List of Lepidoptera that feed on maples). In high concentrations, caterpillars, like
10764-474: The oceans, the thermohaline circulation probably was much different from what it is today, with downwellings occurring in the North Pacific rather than the North Atlantic, and water density mainly being controlled by salinity rather than temperature. The K–Pg extinction event caused a floral and faunal turnover of species, with previously abundant species being replaced by previously uncommon ones. In
10881-434: The original areas the stages were defined, accessibility, and the protected status of the area due to its geological significance. The Selandian was first proposed by Danish geologist Alfred Rosenkrantz in 1924 based on a section of fossil-rich glauconitic marls overlain by gray clay which unconformably overlies Danian chalk and limestone . The area is now subdivided into the Æbelø Formation , Holmehus Formation , and
10998-444: The proliferation of sulfate-reducing microorganisms which create highly toxic hydrogen sulfide H 2 S as a waste product. During the event, the volume of sulfidic water may have been 10–20% of total ocean volume, in comparison to today's 1%. This may have also caused chemocline upwellings along continents and the dispersal of H 2 S into the atmosphere. During the PETM there was a temporary dwarfing of mammals apparently caused by
11115-610: The proposal was officially published in 2006. The Selandian and Thanetian are both defined in Itzurun beach by the Basque town of Zumaia , 43°18′02″N 2°15′34″W / 43.3006°N 2.2594°W / 43.3006; -2.2594 , as the area is a continuous early Santonian to early Eocene sea cliff outcrop . The Paleocene section is an essentially complete, exposed record 165 m (541 ft) thick, mainly composed of alternating hemipelagic sediments deposited at
11232-461: The recently emptied Earth. Though some animals attained great size, most remained rather small. The forests grew quite dense in the general absence of large herbivores. Mammals proliferated in the Paleocene, and the earliest placental and marsupial mammals are recorded from this time, but most Paleocene taxa have ambiguous affinities . In the seas, ray-finned fish rose to dominate open ocean and recovering reef ecosystems. The word "Paleocene"
11349-404: The recently emptied landscape, or a response to the increased amount of shade provided in a forested landscape. Lycopods , ferns, and angiosperm shrubs may have been important components of the Paleocene understory . In general, the forests of the Paleocene were species-poor, and diversity did not fully recover until the end of the Paleocene. For example, the floral diversity of what is now
11466-675: The region at the PETM. During the Paleocene, the continents continued to drift toward their present positions. In the Northern Hemisphere, the former components of Laurasia (North America and Eurasia) were, at times, connected via land bridges: Beringia (at 65.5 and 58 mya) between North America and East Asia, the De Geer route (from 71 to 63 mya) between Greenland and Scandinavia , the Thulean route (at 57 and 55.8 mya) between North America and Western Europe via Greenland, and
11583-823: The same is true in the North Dakotan Almont/Beicegel Creek —such as Ochnaceae , Cyclocarya , and Ginkgo cranei —indicating the same floral families have characterized South American rainforests and the American Western Interior since the Paleocene. The extinction of large herbivorous dinosaurs may have allowed the forests to grow quite dense, and there is little evidence of wide open plains. Plants evolved several techniques to cope with high plant density, such as buttressing to better absorb nutrients and compete with other plants, increased height to reach sunlight, larger diaspore in seeds to provide added nutrition on
11700-708: The stems. Most species require stratification in order to germinate , and some seeds can remain dormant in the soil for several years before germinating. The genus Acer , together with genus Dipteronia , were formerly often classified in a family of their own, the Aceraceae , but recent botanical consensus, including the Angiosperm Phylogeny Group system, includes them in the family Sapindaceae ; their exclusion from Sapindaceae would leave that family paraphyletic . Within Sapindaceae, Acer
11817-483: The trees' long-term health. A maple leaf is on the coat of arms of Canada , and is on the Canadian flag . The maple is a common symbol of strength and endurance and has been chosen as the national tree of Canada. Maple leaves are traditionally an important part of Canadian Forces military regalia, for example, the military rank insignia for generals use maple leaf symbols. There are 10 species naturally growing in
11934-471: The upper limit, average sea surface temperatures (SSTs) at 60° N and S would have been the same as deep sea temperatures, at 30° N and S about 23 °C (73 °F), and at the equator about 28 °C (82 °F). In the Danish Palaeocene sea, SSTs were cooler than those of the preceding Late Cretaceous and the succeeding Eocene. The Paleocene foraminifera assemblage globally indicates
12051-498: The upward excursion in temperature. The warm, wet climate supported tropical and subtropical forests worldwide, mainly populated by conifers and broad-leafed trees. In Patagonia, the landscape supported tropical rainforests , cloud rainforests , mangrove forests , swamp forests , savannas , and sclerophyllous forests. In the Colombian Cerrejón Formation , fossil flora belong to the same families as modern day flora—such as palm trees , legumes , aroids , and malvales —and
12168-422: The weight of maple, only the tops of Gibson 's Les Paul guitars are made from carved maple, often using quilted or flamed maple tops. Due to its weight, very few solid body guitars are made entirely from maple, but many guitars have maple necks, tops or veneers. Maple is also often used to make bassoons and sometimes for other woodwind instruments like maple recorders. Many drums are made from maple. From
12285-406: The wood of choice for bowling pins, bowling alley lanes, pool and snooker cue shafts , and butcher's blocks . Maple wood is also used for the manufacture of wooden baseball bats , though less often than ash or hickory due to the tendency of maple bats to shatter if they do break. The maple bat was introduced to Major League Baseball (MLB) in 1998 by Sam Bat founder Sam Holman. Today it
12402-599: The world by a high- iridium band, as well as discontinuities with fossil flora and fauna. It is generally thought that a 10 to 15 km (6 to 9 mi) wide asteroid impact, forming the Chicxulub Crater in the Yucatán Peninsula in the Gulf of Mexico , and Deccan Trap volcanism caused a cataclysmic event at the boundary resulting in the extinction of 75% of all species. The Paleocene ended with
12519-806: The world including the "five great W's" in England : Wakehurst Place Garden , Westonbirt Arboretum , Windsor Great Park , Winkworth Arboretum and Wisley Garden . In the United States , the aceretum at the Harvard -owned Arnold Arboretum in Boston is especially notable. In the number of species and cultivars, the Esveld Aceretum in Boskoop, Netherlands , is the largest in the world. Maples are important as sources of syrup and wood. Dried wood
12636-488: Was a separate municipality. In 1997, it became part of Laarbeek . The spoken language is Peellands (an East Brabantian dialect, which is very similar to Standard Dutch ). Since many decades, the village has been an important location for textile production. Petit & Fritsen was a bell foundry that was located in Aarle-Rixtel until 2014. In that year, the company was acquired by a competitor who became thereby
12753-455: Was due to an ejection of 2,500–4,500 gigatons of carbon into the atmosphere, most commonly explained as the perturbation and release of methane clathrate deposits in the North Atlantic from tectonic activity and resultant increase in bottom water temperatures. Other proposed hypotheses include methane release from the heating of organic matter at the seafloor rather than methane clathrates, or melting permafrost . The duration of carbon output
12870-463: Was first used by French paleobotanist and geologist Wilhelm Philipp Schimper in 1874 while describing deposits near Paris (spelled "Paléocène" in his treatise). By this time, Italian geologist Giovanni Arduino had divided the history of life on Earth into the Primary ( Paleozoic ), Secondary ( Mesozoic ), and Tertiary in 1759; French geologist Jules Desnoyers had proposed splitting off
12987-530: Was not a major contributor to the greenhouse climate, and deep water temperatures more likely change as a response to global temperature change rather than affecting it. In the Arctic, coastal upwelling may have been largely temperature and wind-driven. In summer, the land surface temperature was probably higher than oceanic temperature, and the opposite was true in the winter, which is consistent with monsoon seasons in Asia. Open-ocean upwelling may have also been possible. The Paleocene climate was, much like in
13104-429: Was not much angiosperm migration into the region in the early Paleocene. Over the K–Pg extinction event, angiosperms had a higher extinction rate than gymnosperms (which include conifers, cycads , and relatives) and pteridophytes (ferns, horsetails , and relatives); zoophilous angiosperms (those that relied on animals for pollination) had a higher rate than anemophilous angiosperms; and evergreen angiosperms had
13221-558: Was officially defined as the Paleocene, Eocene, and Oligocene Epochs; and the Neogene as the Miocene and Pliocene Epochs. In 1989, Tertiary and Quaternary were removed from the time scale due to the arbitrary nature of their boundary, but Quaternary was reinstated in 2009. The term "Paleocene" is a portmanteau combination of the Ancient Greek palaios παλαιός meaning "old", and the word "Eocene", and so means "the old part of
13338-439: Was one of the most significant periods of global change during the Cenozoic. Geologists divide the rocks of the Paleocene into a stratigraphic set of smaller rock units called stages , each formed during corresponding time intervals called ages. Stages can be defined globally or regionally. For global stratigraphic correlation, the ICS ratify global stages based on a Global Boundary Stratotype Section and Point (GSSP) from
13455-540: Was shown that the Danian and the Montian are the same, the ICS decided to define the Danian as starting with the K–Pg boundary, thus ending the practice of including the Danian in the Cretaceous. In 1991, the GSSP was defined as a well-preserved section in the El Haria Formation near El Kef , Tunisia, 36°09′13″N 8°38′55″E / 36.1537°N 8.6486°E / 36.1537; 8.6486 , and
13572-508: Was still connected to South America and Australia, and, because of this, the Antarctic Circumpolar Current —which traps cold water around the continent and prevents warm equatorial water from entering—had not yet formed. Its formation may have been related in the freezing of the continent. Warm coastal upwellings at the poles would have inhibited permanent ice cover. Conversely, it is possible deep water circulation
13689-556: Was wetter than the Northern, or the Southern experienced less evaporation than the Northern. In either case, this would have made the Northern more saline than the Southern, creating a density difference and a downwelling in the North Pacific traveling southward. Deep water formation may have also occurred in the South Atlantic. It is largely unknown how global currents could have affected global temperature. The formation of
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