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دراسة الأحداث البيولوجية

من ويكيبيديا، الموسوعة الحرة
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الفينولوجيا، هو علم دراسة النباتات الدورية وأحداث دورة حياة الحيوان وكيفية تأثّرها بالتغيرات الموسمية وتغيرات المناخ عبر السنين، إضافة لعوامل الموائل (كالارتفاع). اشتق الاسم من اللغة اليونانية، وهو مكون من كلمة φαίνω وتعني عرض أو إلقاء الضوء على[1] وكلمة λόγος وتعني دراسة أو علم[2]، يشير المصطلح إلى أن الفينولوجيا عني أساساً بتواريخ الأحداث البيولوجية الأولى من دورات الحياة السنوية. ومن الأمثلة على ذلك، تاريخ أول حدث لهجرة الطيور، تاريخ ظهور أوراق الأشجار والأزهار الأولى، أول رحلة طيران للفراشات، تاريخ تلوّن أوراق الأشجار وتساقطها في الأشجار غير دائمة الخضرة، وتواريخ وضع الطيور والحشرات للبيوض لأول مرة، أو مواقيت دورات التنمية لمستعمرات نحلة العسل في مناطق المناخ المعتدل. في الأدبيات العلمية المتعلقة بعلم البيئة، يستخدم هذا المصطلح بشكل عام للدلالة على الإطار الزمني لأي من الظواهر البيولوجية الموسمية، بما في ذلك تواريخ آخر ظهور (على سبيل المثال، قد تكون الفينولوجيا الموسمية لبعض الأنواع من نيسان وحتى أيلول). نظراً لأن العديد من هذه الظواهر حساسة جداً لتغيرات المناخ، خصوصاً درجات الحرارة، فقد تكون السجلات الفينولوجية وثائق مفيدة للحرارة في علم المناخ التاريخي، خاصة لدراسة تغير المناخ والاحترار العالمي. على سبيل المثال، تستخدم سجلات حصاد العنب في أوروبا لإعادة بناء سجلات درجات الحرارة الموسمية المتزايدة في الصيف حتى 500 سنة خلت[3][4] In addition to providing a longer historical baseline than instrumental measurements, phenological observations provide high temporal resolution of ongoing changes related to احترار عالمي.[5][6] The concept of Growing-degree day contributes to our understanding of phenology.

السجلات القديمة[عدل]

Observations of phenological events have provided indications of the progress of the natural calendar since ancient agricultural times. Many cultures have traditional phenological proverbs and sayings which indicate a time for action: "When the sloe tree is white as a sheet, sow your barley whether it be dry or wet" or attempt to forecast future climate: "If oak's before ash, you're in for a splash. If ash before oak, you're in for a soak". But the indications can be pretty unreliable, as an alternative version of the rhyme shows: "If the oak is out before the مران عالي, 'Twill be a summer of wet and splash; If the ash is out before the oak,'Twill be a summer of fire and smoke." Theoretically, though, these are not mutually exclusive, as one forecasts immediate conditions and one forecasts future conditions.

The North American Bird Phenology Program at USGS Patuxent Wildlife Research Center (PWRC) is in possession of a collection of millions of bird arrival and departure date records for over 870 species across North America, dating between 1880 and 1970. This program, originally started by Wells W. Cooke, involved over 3,000 observers including many notable naturalists of the time. The program ran for 90 years and came to a close in 1970 when other programs starting up at PWRC took precedent. The program was again started in 2009 to digitize the collection of records and now with the help of citizens worldwide, each record is being transcribed into a database which will be publicly accessible for use.

The English naturalists Gilbert White and William Markwick reported the seasonal events of more than 400 plant and animal species, Gilbert White in Selborne, Hampshire and William Markwick in Battle, Sussex over a 25-year period between 1768 and 1793. The data, reported in White's Natural History and Antiquities of Selborne[7] are reported as the earliest and latest dates for each event over 25 years; so annual changes cannot therefore be determined.

In Japan and China the time of blossoming of cherry and peach trees is associated with ancient festivals and some of these dates can be traced back to the eighth century. Such historical records may, in principle, be capable of providing estimates of climate at dates before instrumental records became available. For example, records of the harvest dates of the pinot noir عنب in منطقة بورغندي have been used in an attempt to reconstruct spring–summer temperatures from 1370 to 2003;[8][9] the reconstructed values during 1787–2000 have a correlation with Paris instrumental data of about 0.75.

السجلات الحديثة[عدل]

Robert Marsham is the founding father of modern phenological recording. Marsham was a wealthy landowner who kept systematic records of "Indications of spring" on his estate at Stratton Strawless, نورفولك, from 1736. These were in the form of dates of the first occurrence of events such as flowering, bud burst, emergence or flight of an insect. Consistent records of the same events or "phenophases" were maintained by generations of the same family over unprecedentedly long periods of time, eventually ending with the death of Mary Marsham in 1958, so that trends can be observed and related to long-term climate records. The data show significant variation in dates which broadly correspond with warm and cold years. Between 1850 and 1950 a long-term trend of gradual climate warming is observable, and during this same period the Marsham record of oak leafing dates tended to become earlier.[10]

After 1960 the rate of warming accelerated, and this is mirrored by increasing earliness of oak leafing, recorded in the data collected by Jean Combes in Surrey. Over the past 250 years, the first leafing date of oak appears to have advanced by about 8 days, corresponding to overall warming on the order of 1.5 °C in the same period.

Towards the end of the 19th century the recording of the appearance and development of plants and animals became a national pastime, and between 1891 and 1948 a programme of phenological recording was organised across the British Isles by the Royal Meteorological Society (RMS). Up to 600 observers submitted returns in some years, with numbers averaging a few hundred. During this period 11 main plant phenophases were consistently recorded over the 58 years from 1891–1948, and a further 14 phenophases were recorded for the 20 years between 1929 and 1948. The returns were summarised each year in the Quarterly Journal of the RMS as The Phenological Reports. The 58-year data have been summarised by Jeffree (1960),[11] and show that flowering dates could be as many as 21 days early and as many as 34 days late, with extreme earliness greatest in summer flowering species, and extreme lateness in spring flowering species. In all 25 species, the timings of all phenological events are significantly related to temperature,[12][13] indicating that phenological events are likely to get earlier as climate warms.

The Phenological Reports ended suddenly in 1948 after 58 years, and Britain was without a national recording scheme for almost 50 years, just at a time when climate change was becoming evident. During this period, important contributions were made by individual dedicated observers. The naturalist and author Richard Fitter recorded the First Flowering Date (FFD) of 557 species of British flowering plants in Oxfordshire between about 1954 and 1990. Writing in ساينس in 2002, Richard Fitter and his son Alistair Fitter found that "the average FFD of 385 British plant species has advanced by 4.5 days during the past decade compared with the previous four decades."[14][15] They note that FFD is sensitive to temperature, as is generally agreed, that "150 to 200 species may be flowering on average 15 days earlier in Britain now than in the very recent past" and that these earlier FFDs will have "profound ecosystem and evolutionary consequences".

In the last decade, national recording in Britain has been resumed by the UK Phenology network [1], run by Woodland Trust and the Centre for Ecology and Hydrology and the BBC Springwatch survey.[16] There is a USA National Phenology Network [2] in which both professional scientists and lay recorders participate, a European Phenology Network that has monitoring, research and educational remits[17] and many other countries such as Canada (Alberta Plantwatch [3] and Saskatchewan PlantWatch[18]), China and Australia[19][20] have phenological programs.

In eastern North America, almanacs are traditionally used for information on action phenology (in agriculture), taking into account the astronomical positions at the time. William Felker has studied phenology in أوهايو, USA since 1973 and now publishes "Poor Will's Almanack", a phenological almanac for farmers (not to be confused with a late 18th century almanac by the same name).

Airborne sensors[عدل]

Recent technological advances in studying the earth from space have resulted in a new field of phenological research that is concerned with observing the phenology of whole نظام بيئيs and stands of غطاء نباتي on a global scale using proxy approaches. These methods complement the traditional phenological methods which recorded the first occurrences of individual species and phenophases.

The most successful of these approaches is based on tracking the temporal change of a Vegetation Index (like Normalized Difference Vegetation Index(NDVI)). NDVI makes use of the vegetation's typical low reflection in the red (red energy is mostly absorbed by growing plants for Photosynthesis) and strong reflection in the Near أشعة تحت الحمراء (Infrared energy is mostly reflected by plants due to their cellular structure). Due to its robustness and simplicity, NDVI has become one of the most popular remote sensing based products. Typically, a vegetation index is constructed in such a way that the attenuated reflected sunlight energy (1% to 30% of incident sunlight) is amplified by ratio-ing red and NIR following this equation:

The evolution of the vegetation index through time, depicted by the graph above, exhibits a strong ارتباط (إحصاء) with the typical green vegetation growth stages (emergence, vigor/growth, maturity, and harvest/senescence). These temporal curves are analyzed to extract useful parameters about the vegetation growing season (start of season, end of season, length of موسم زراعة, etc.). Other growing season وسيط (رياضيات)s could potentially be extracted, and global maps of any of these growing season parameters could then be constructed and used in all sorts of تغير المناخ studies.

A noteworthy example of the use of استشعار عن بعد based phenology is the work of Ranga Myneni[21] from جامعة بوسطن. This work[22][23] showed an apparent increase in vegetation productivity that most likely resulted from the increase in temperature and lengthening of the growing season in the تايغا.[24] Another example based on the MODIS enhanced vegetation index (EVI) reported by Alfredo Huete[25] at جامعة أريزونا and colleagues showed that the غابات الأمازون, as opposed to the long held view of a monotonous growing season or growth only during the wet rainy season, does in fact exhibit growth spurts during the dry season.[26][27]

However, these phenological parameters are only an approximation of the true biological growth stages. This is mainly due to the limitation of current space based remote sensing, especially the spatial resolution, and the nature of vegetation index. A pixel in an image does not contain a pure target (like a tree, a shrub, etc.) but contains a mixture of whatever intersected the sensor's field of view.

طالع أيضاً[عدل]


  1. ^ φαίνω, Henry George Liddell, Robert Scott, A Greek-English Lexicon, on Perseus
  2. ^ λόγος, Henry George Liddell, Robert Scott, A Greek-English Lexicon, on Perseus
  3. ^ . Diplomarbeit der Philosophisch-naturwissenschaftlichen Fakultät der Universität Bern (Thesis of Philosophy and science faculty of the University of Bern). 2007 http://web.archive.org/web/20081217053707/http://www.giub.unibe.ch/klimet/docs/diplom_nmeier.pdf |archiveurl= تحتاج عنوانا (مساعدة). تمت أرشفته من الأصل على 2008-12-17. اطلع عليه بتاريخ 2007-12-25. "Phenological grape harvest observations in Switzerland over the last 500 years have been used as a proxy indicator for reconstructing past temperature variability." 
  4. ^ رسائل بحوث جيوفيزيائية (20). Bibcode:2007GeoRL..3420705M. doi:10.1029/2007GL031381 http://www.agu.org/pubs/crossref/2007/2007GL031381.shtml |url= تحتاج عنوانا (مساعدة). "Phenological grape harvest observations in Switzerland over the last 500 years have been used as a proxy indicator for reconstructing past temperature variability." 
  5. ^ Menzel, A.؛ Sparks, T.H.; Estrella, N.; Koch, E.; Aasa, A.; Ahas, R.; Alm-kübler, K.; Bissolli, P.; Braslavská, O.; Briede, A.; Others, (2006). "European phenological response to climate change matches the warming pattern". Global Change Biology 12 (10): 1969–1976. doi:10.1111/j.1365-2486.2006.01193.x. "One of the preferred indicators is phenology, the science of natural recurring events, as their recorded dates provide a high-temporal resolution of ongoing changes." 
  6. ^ Schwartz, M. D.؛ Ahas, R.; Aasa, A. (2006). "Onset of spring starting earlier across the Northern Hemisphere". Global Change Biology 12 (2): 343–351. doi:10.1111/j.1365-2486.2005.01097.x. "SI first leaf dates, measuring change in the start of ‘early spring’ (roughly the time of shrub budburst and lawn first greening), are getting earlier in nearly all parts of the Northern Hemisphere. The average rate of change over the 1955–2002 period is approximately -1.2 days per decade." 
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  13. ^ SpringerLink - Abstract
  14. ^ Fitter، A.H., Fitter، R.S.R. (2002). "Rapid changes in flowering time in British plants". Science 296 (5573): 1689–1691. Bibcode:2002Sci...296.1689F. doi:10.1126/science.1071617. PMID 12040195. 
  15. ^ Rapid Changes in Flowering Time in British Plants 296. SCIENCE. 31 May 2002. تمت أرشفته من الأصل على 2008-12-17. اطلع عليه بتاريخ 2010-05-25. 
  16. ^ BBC - Science & Nature - UK Wildlife - Springwatch survey
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روابط خارجية[عدل]