For some years in the West (as late as 353 in Rome) the birth feast was appended to the baptismal feast on the 6th of January, and in Jerusalem it altogether supplanted it from about 360 to 440, when Bishop Juvenal introduced the feast of the 25th of December. The new feast was about the same time (440) finally established in Alexandria. The quadragesima of Epiphany (i.e. the feast of the presentation in the Temple, or hupapantē) continued to be celebrated in Jerusalem on the 14th of February, forty days after the 6th of January, until the reign of Justinian. In most other places it had long before been put back to the 2nd of February to suit the new Christmas. Armenian historians describe the riots, and display of armed force, without which Justinian was not able in Jerusalem to transfer this feast from the 14th to the 2nd of February.
The grounds on which the Church introduced so late as 350–440 a Christmas feast till then unknown, or, if known, precariously linked with the baptism, seem in the main to have been the following. (1) The transition from adult to infant baptism was proceeding rapidly in the East, and in the West was well-nigh completed. Its natural complement was a festal recognition of the fact that the divine element was present in Christ from the first, and was no new stage of spiritual promotion coeval only with the descent of the Spirit upon him at baptism. The general adoption of child baptism helped to extinguish the old view that the divine life in Jesus dated from his baptism, a view which led the Epiphany feast to be regarded as that of Jesus’ spiritual rebirth. This aspect of the feast was therefore forgotten, and its importance in every way diminished by the new and rival feast of Christmas. (2) The 4th century witnessed a rapid diffusion of Marcionite, or, as it was now called, Manichaean propaganda, the chief tenet of which was that Jesus either was not born at all, was a mere phantasm, or anyhow did not take flesh of the Virgin Mary. Against this view the new Christmas was a protest, since it was peculiarly the feast of his birth in the flesh, or as a man, and is constantly spoken of as such by the fathers who witnessed its institution.
In Britain the 25th of December was a festival long before the conversion to Christianity, for Bede (De temp. rat. ch. 13) relates that “the ancient peoples of the Angli began the year on the 25th of December when we now celebrate the birthday of the Lord; and the very night which is now so holy to us, they called in their tongue modranecht (môdra niht), that is, the mothers’ night, by reason we suspect of the ceremonies which in that night-long vigil they performed.” With his usual reticence about matters pagan or not orthodox, Bede abstains from recording who the mothers were and what the ceremonies. In 1644 the English puritans forbad any merriment or religious services by act of Parliament, on the ground that it was a heathen festival, and ordered it to be kept as a fast. Charles II. revived the feast, but the Scots adhered to the Puritan view.
Outside Teutonic countries Christmas presents are unknown. Their place is taken in Latin countries by the strenae, French étrennes, given on the 1st of January; this was in antiquity a great holiday, wherefore until late in the 4th century the Christians kept it as a day of fasting and gloom. The setting up in Latin churches of a Christmas crèche is said to have been originated by St Francis.
Authorities.—K. A. H. Kellner, Heortologie (Freiburg im Br., 1906), with Bibliography; Hospinianus, De festis Christianorum (Genevae, 1574); Edw. Martène, De Antiquis Ecclesiae Ritibus, iii. 31 (Bassani, 1788); J. C. W. Augusti, Christl. Archäologie, vols. i. and v. (Leipzig, 1817–1831); A. J. Binterim, Denkwürdigkeiten, v. pt. i. p. 528 (Mainz, 1825, &c.); Ernst Friedrich Wernsdorf, De originibus Solemnium Natalis Christi (Wittenberg, 1757, and in J. E. Volbeding, Thesaurus Commentationum, Lipsiae, 1847); Anton. Bynaeus, De Natali Jesu Christi (Amsterdam, 1689); Hermann Usener, Religionsgeschichtliche Untersuchungen (Bonn, 1889); Nik. Nilles, S.J., Kalendarium Manuale (Innsbruck, 1896); L. Duchesne, Origines du culte chrétien (3e éd., Paris, 1889). (F. C. C.)
CHRISTMAS ISLAND, a British possession under the government of the Straits Settlements, situated in the eastern part of the Indian Ocean (in 10° 25′ S., 105° 42′ E.), about 190 m. S. of Java. The island is a quadrilateral with hollowed sides, about 12 m. in greatest length and 9 in extreme breadth. It is probably the only tropical island that had never been inhabited by man before the European settlement. When the first settlers arrived, in 1897, it was covered with a dense forest of great trees and luxuriant under-shrubbery. The settlement in Flying Fish Cove now numbers some 250 inhabitants, consisting of Europeans, Sikhs, Malays and Chinese, by whom roads have been cut and patches of cleared ground cultivated.
The island is the flat summit of a submarine mountain more than 15,000 ft. high, the depth of the platform from which it rises being about 14,000 ft., and its height above the sea being upwards of 1000 ft. The submarine slopes are steep, and within 20 m. of the shore the depth of the sea reaches 2400 fathoms. It consists of a central plateau descending to the water in three terraces, each with its “tread” and “rise.” The shore terrace descends by a steep cliff to the sea, forming the “rise” of a submarine “tread” in the form of fringing reef which surrounds the island and is never uncovered, even at low water, except in Flying Fish Cove, where the only landing-place exists. The central plateau is a plain whose surface presents “rounded, flat-topped hills and low ridges and reefs of limestone,” with narrow intervening valleys. On its northern aspect this plateau has a raised rim having all the appearances of being once the margin of an atoll. On these rounded hills occurs the deposit of phosphate of lime which gives the island its commercial value. The phosphatic deposit has doubtless been produced by the long-continued action of a thick bed of sea-fowl dung, which converted the carbonate of the underlying limestone into phosphate. The flat summit is formed by a succession of limestones—all deposited in shallow water—from the Eocene (or Oligocene) up to recent deposits in the above-mentioned atoll with islands on its reef. The geological sequence of events appears to have been the following:—After the deposition of the Eocene (or Oligocene) limestone—which reposes upon a floor of basalts and trachytes—basalts and basic tuffs were ejected, over which, during a period of very slow depression, orbitoidal limestones of Miocene age—which seem to make up the great mass of the island—were deposited; then elapsed a long period of rest, during which the atoll condition existed and the guano deposit was formed; from then down to the present time there has succeeded a series of sea-level subsidences, resulting in the formation of the terraces and the accummulation of the detritus now seen on the first inland cliff, the old submarine slope of the island. The occurrence of such a series of Tertiary deposits appears to be unknown elsewhere. The whole series was evidently deposited in shallow water on the summit of a submarine volcano standing in its present isolation, and round which the ocean floor has probably altered but a few hundred feet since the Eocene age. Thus although the rocks of the southern coast of Java in their general character and succession resemble those of Christmas Island, there lies between them an abysmal trough 18,000 ft. in depth, which renders it scarcely possible that they were deposited in a continuous area, for such an enormous depression of the sea-floor could hardly have occurred since Miocene times without involving also Christmas Island. One of the main purposes of the exploration was to obtain light on the question of the foundation of atolls.
The flora consists of 129 species of angiosperms, 1 Cycas, 22 ferns, and a few mosses, lichens and fungi, 17 of which are endemic, while a considerable number—not specifically distinct—form local varieties nearly all presenting Indo-Malayan affinities, as do the single Cycas, the ferns and the cryptogams. As to its fauna, the island contains 319 species of animals—54 only being vertebrates—145 of which are endemic. A very remarkable distributional fact in regard to them, and one not yet fully explained, is that a large number show affinity with species in the Austro-Malayan rather than in the Indo-Malayan, their nearer, region. The ocean currents, the trade-winds blowing from the Australian mainland, and north-westerly storms from the Malayan islands, are no doubt responsible for the introduction of many, but not all, of these Malayan and Australasian species. The climate is healthy, the temperature varying from 75° to 84° F. The prevailing wind is the S.E. trade, which
