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716:). However, I've stopped making new templates temporarily to ask a question: is it okay to create a geological stage template (as in, create a template specifically for stages defined by the ics, which would go on their articles in the upper right-hand corner.)? Also, I'm thinking about removing the table-like templates that were on the epoch and stage pages before I started adding my geological epoch templates or possibly placing them in the 'subdivisions' sections of these articles. (example: 87: 63: 97: 32: 593:
pages and unfortunately needed further adjustment (pointing to "Late Cretaceous" instead of "Early Cretaceous Series of Europe"). The Cambridge Greensand is no doubt far down on the list of stubs to address, but there has apparently been some discussion about the Albian/Cenomanian boundary, and a paleogeologist could provide a full discussion of the problem.
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of the main period to provide a sense of sucession, and to avoid having lots of practically empty pages. There may be a case for some action-packed sub-periods, especially those of the Tertiary, to have a page to themselves, but in the majority I don't think there'll ever be enough interest or content to make individual articles justifiable. Comments?
251:- themes which are more relevant to the Cambrian article and better covered there. There may, eventually, be cause to create articles on late/middle/early sections of periods, but wanting an article on every faunal stage seems like demanding an article on each chapter of a novel. Further, because stages overlap, I feel that a table like the one in 214:
paleontology and regional geology. It seems to me a waste of time for the reader to give their complete descriptions in the article of the period itself, a mere mentioning of the different systems of subdivision in use/used would be enough there. I agree btw that these articles are often incomplete and not very useful, but
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into redirects. But when they would contain information about research history, stratigraphic definitions, rock formations of that specific age, etc. (I feel that's what they should do, since the articles about periods are simply too general for that...) they give the reader some background and would be a worthy addition.
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to say anything informative about sub-periods. Evolutionary trends, climate change, and plate tectonics operate, on the whole, on a period-level time scale. My vision is to have a thorough discussion on how things changed through each period, which may even be broken down on a sub-period by sub-period level
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I am not totally sure about having huge tables with many subdivions in them in every article about a period/system. When there are ten different systems of subdividing the period they get large so they may ruin the layout and disrupt the text too much(?) All these stratigraphic units are maybe just a
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is far more useful than 50 pages consisting of little more than a list of start and end dates and preceding periods, and perhaps a bit of unreferenced, poorly maintained and duplicated material; the table makes it very easy to place each faunal stage in the context of the whole article. I think that
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Glad that someone else is expressing interest in this area! I feel that the Mesozoic periods probably contain enough information to merit remaining as individual articles, although I echo your comments that a full list of taxa is a bad idea. But in the Palaeozoic we simply don't have the resolution
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I've been making progress in bringing all articles to use a consistent format, and have been thinking about subperiods. These all have their own page, most of which have practically no information on; it seems to me that it would be better to combine all information about subperiods into the article
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This post is occasioned by a change to the stub for "Cambridge Greensand", which had labeled it "Early Cretaceous". The BGS pronounced it "Cenomanian", making it early Late Cretaceous. My change was to "Middle to Late Cretaceous", a safe enough change, I'd thought, but the stub had links to category
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I am not a geologist, but recently have had occasion to make extensive use of data from the major sources of dating information (esp. the British Geological Survey). Occasionally, I've spotted discrepancies between the date range given in the Knowledge and that available from these sources, and have
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I think the ages could eventually all have their own articles, but not because of Earth history. Like you, I see no point in copying information about paleogeography or paleontology to the stages' articles. When these articles only contain information on such subjects, I don't care if they are made
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are attended to in differing ways whilst sea level gets a subsection to itself in some and not in others. Life is subdivided differently from one to another - understandable to some degree as there is more to say in certain periods than others as regards marine or terrestrial life, fauna or flora.
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the article; that way there is context for the information and duplication is minimised. If somebody wants to know what is going on in the Ordovician they don't want to have to trawl through a dozen overlapping subperiod pages. The Tommotian was one of the better articles, I'll grant you, but it
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Hi Martin, thanks for your reply. I am glad too, when nobody reacted I thought I was the only one who cared, until I found this period-project. You are right: we don't want to have too many articles that simply give the same information. I agree with you that our main concern should lie with the
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Hi, I see you're deleting the content of articles about stages/ages for some time now, redirecting those pages to pages about the period/system. I think these names are encyclopedic enough to have their own articles. If not so much as periods of time, then as units in (often local) stratigraphy,
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I noticed a few weeks ago that for the eras, eons, and periods, their pages had a template in the upper right-hand corner. the template included a timeline, among other aspects, and made the pages look more official. However, the epochs and ages didn't have such a system, and instead had a grid
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contained some (basic) information on American lithostratigraphy and could have stayed as a stub. So my proposal would be to only keep those articles when they have specialistic information on stratigraphy (weather bio-, litho-, magneto-, or chrono-) or their research history. When they have
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I note that there has only been one contribution here in the past 18 months. It's a pity as there would still seem to be a lot of work to do getting the articles on geologic(al) periods into better shape. I am constantly irked by the scrappy nature of the
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template that showed all the subdivisions of a given period. I probably should have asked before doing this, but I created and added 'geological epoch' templates to each of the epoch pages, which I though made the pages appear more uniform (example:
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The size of the measurement uncertainty does not warrant a presentation with three digits after the decimal point without uncertainty interval. Also, this is only one of several high-precision datings mentioned in the article, another one being
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Palaeogeography could do with more attention and a more global perspective taken as regards certain periods - the Carboniferous has been identified as too Americo-centric though it needs informed editors to redress these imbalances.
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What do others think? I note that attempts - at least partially sucessful have been made in the past to improve these articles as a whole and those responsible are to be commended. Is it perhaps time for another push though?
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About the table: When a subject is not yet mentioned at all, I filled in "stub". I am not sure what to do with "Events". Certainly not all periods had asteroid impacts, what else could not be covered in the other subjects?
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twice made a change in a Knowledge stub to nudge the entry closer to the current standard. (Both cited the BGS entry.) Because I'm not a geologist, someone in the field should know about these changes.
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contained unsourced statements about the palaeogeography which is in fact very poorly constrained throughout the whole Cambrian, and another unsourced section which attempted to sum up the
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periods: because they are less known than their subdivisions, and there is a lot to write about the epochs, I rather feel the focus for the last 65 mya could better be with the epochs:
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etc). On the other hand, I see no reason to have articles on the epochs with names like "Late Cretaceous" or "Early Ordovician". They seem to me artificial inventions of the ICS/IUGS.
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information on Earth history (paleogeography, paleoclimate, paleontology/evolution, etc) that information can be moved to the periods, maybe except for some obvious things (the
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I've been toying with some timeline colors. Some of these letters are hard to read, especially the T. My mobile uses slightly different colors and makes it harder (
390:) which you might wish to discuss. The stub category has been made with a name to agree with the article - if this is incorrect, please propose it for renaming at 468:), serves to break the flow of the article and gives it a messy appearance. They might better be confined to tables except where there is discussion of them. 920: 448:. There are sections on subdivisions, climate, (palaeo)geography and life in each of the periods concerned though beyond that there is less consistency. 596:
A more general question is whether or not the date ranges in stubs should be adjusted to conform to current standards (as set by the BGS, USGS, etc.).
634:) present the dating of the Permian–Triassic boundary as 251.902 Mya. Is that precision reasonable? The Subcommission on Permian Stratigraphy of the 635: 371:(with redirects from botht he US spelling and from palaeo-geo-stub). This is for historical/prehistoric geographical features and locations, e.g., 975: 970: 694: 1000: 509: 505: 150: 73: 995: 540: 513: 720:)(they might be useful if they were put in the 'subdivisions' sections of these pages). thoughts? Does what I'm saying make sense? by 17: 256:
focussing our attention on improving the period level articles should be our focus for now; sub-periods act as a (vast) distraction.
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Seth D. Burgess, Samuel Bowring, and Shu-zhong Shen (April 1, 2014). "High-precision timeline for Earth's most severe extinction".
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The listing of subdivisions within the body of the article, especially where there are large numbers of these (as (again) in the
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Hi all - thought i'd give you the heads-up that a new stub type has been created relevant to this project:
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But basically the banner got edit and then put back together. Not sure if it is correct, but the
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That said some more consistency would improve the quality of this important family of articles.
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where, perhaps reasonably given their proximity in time to the present, the emphasis is on the
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resource. If you would like to participate, you can choose to edit this article, or visit the
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I've upgraded sections of the Carboniferous to A, but as I wrote these others may disagree!
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for example contained good information that is now lost for the reader. Please also see
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is back as best I can see. But not sure if the markers are correct. Thanks,
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BTW, there seems to be a mismatch between the name of the parent article (
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on the bad state of the stratigraphic section in this Knowledge. Regards,
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Creating a template for the geological stages (as defined by the ICS)
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periods there seems to be some measure of consistency through the
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bit too specialistic to mention in the article about the period.
923:}} could be implemented into any of these colored timelines. ( 25: 279:
periods. And man, they are still messy... the task is huge.
823:), then I played around with some templates and did this: 284: 512:. These are now all classified in subcategories of 531:Jurassic page and template of time is correct? 506:WP:WikiProject Geology/Periods#Project banner 8: 981:NA-importance Project-Class Geology articles 674:: CS1 maint: multiple names: authors list ( 584:Aligning periods with authoritative sources 539:was missing it as it was removed. And the 201:Why are stages/ages not worth own articles? 921:User:JavaRogers/Template:Period font color 109:Knowledge talk:WikiProject Geology/Periods 57: 991:NA-importance Geological periods articles 986:Project-Class Geological periods articles 693:" with a hyphen redirects to the article 42:does not require a rating on Knowledge's 636:International Commission on Stratigraphy 59: 667: 424:article in particular. Looking at the 357:New stub type relevant to this project 7: 541:Template:Jurassic_graphical_timeline 514:Category:Geological periods articles 494:I have added this task force to the 31: 29: 48:It is of interest to the following 919:Do we like this change? The new {{ 24: 18:Knowledge talk:WikiProject Geology 695:Permian–Triassic extinction event 151:the Geological periods task force 644:. I think this may be based on: 95: 85: 61: 30: 976:NA-importance Geology articles 971:Project-Class Geology articles 702:10:29, 24 September 2019 (UTC) 558:Cryogenian infobox out of date 510:WP:WikiProject Geology/Periods 1: 485:20:44, 21 November 2010 (UTC) 379:. Hope it is useful to you. 131:Knowledge:WikiProject Geology 1001:WikiProject Geology articles 958:) 16:43 14 March 2024 (UTC) 718:Template:Quaternary (period) 553:09:33, 5 February 2015 (UTC) 410:00:57, 19 October 2009 (UTC) 349:16:50, 26 October 2008 (UTC) 292:can be briefly mentioned at 274:15:07, 26 October 2008 (UTC) 232:12:13, 26 October 2008 (UTC) 134:Template:WikiProject Geology 996:Geological periods articles 1017: 734:18:25, 19 March 2020 (UTC) 526:18:29, 14 March 2012 (UTC) 148:This page is supported by 691:Permian-Triassic boundary 687:Permian–Triassic boundary 608:15:12, 8 April 2018 (UTC) 579:14:43, 13 July 2015 (UTC) 290:Messinian Salinity Crisis 195:19:22, 25 July 2008 (UTC) 147: 80: 56: 941:22:55, 15 May 2021 (UTC) 662:10.1073/pnas.1317692111 388:Category:Paleogeography 566:has been changed, see 812:). I came across the 689:" is a redlink, and " 562:The timescale of the 386:), and its category ( 125:for more information. 366:Palaeogeography-stub 683:251.950 ± 0.042 Mya 641:251.902 ± 0.024 Mya 499:WikiProject Geology 415:Re-visiting Periods 220:my earlier comments 114:WikiProject Geology 816:'s color palette ( 618:Several articles ( 436:though not in the 249:small shelly fauna 245:Cambrian explosion 44:content assessment 913: 904: 614:Dating of the PTB 450:Extinction events 406: 271: 210: 192: 166: 165: 162: 161: 158: 157: 1008: 929:for the changes. 914: 911: 905: 899: 893: 886: 879: 872: 865: 858: 851: 844: 837: 830: 684: 679: 673: 665: 656:(9): 3316–3321. 642: 638:uses the dating 503: 497: 404: 370: 364: 261: 205: 182: 139: 138: 137:Geology articles 135: 132: 129: 105: 100: 99: 89: 82: 81: 76: 65: 58: 35: 34: 33: 26: 1016: 1015: 1011: 1010: 1009: 1007: 1006: 1005: 961: 960: 948: 927:User:JavaRogers 917: 916: 910: 907: 903: 898: 895: 891: 888: 884: 881: 877: 874: 870: 867: 863: 860: 856: 853: 849: 846: 842: 839: 835: 832: 828: 809:this screenshot 803: 802: 797: 792: 787: 782: 777: 772: 767: 762: 757: 752: 747: 741: 739:Timeline colors 709: 685:. By the way, " 682: 666: 645: 640: 616: 586: 560: 533: 501: 495: 492: 417: 384:Palaeogeography 368: 362: 359: 206:Copied in from 203: 171: 136: 133: 130: 127: 126: 101: 94: 71: 22: 21: 20: 12: 11: 5: 1014: 1012: 1004: 1003: 998: 993: 988: 983: 978: 973: 963: 962: 947: 944: 908: 901: 896: 889: 882: 875: 868: 861: 854: 847: 840: 833: 826: 825: 798: 793: 788: 783: 778: 773: 768: 763: 758: 753: 748: 743: 742: 740: 737: 708: 705: 615: 612: 585: 582: 559: 556: 532: 529: 491: 490:Project banner 488: 444:or indeed the 416: 413: 358: 355: 354: 353: 352: 351: 336: 301: 297: 280: 202: 199: 198: 197: 170: 167: 164: 163: 160: 159: 156: 155: 146: 143: 142: 140: 107: 106: 103:Geology portal 90: 78: 77: 66: 54: 53: 47: 36: 23: 15: 14: 13: 10: 9: 6: 4: 3: 2: 1013: 1002: 999: 997: 994: 992: 989: 987: 984: 982: 979: 977: 974: 972: 969: 968: 966: 959: 957: 953: 946:Carboniferous 945: 943: 942: 938: 934: 930: 928: 922: 915: 906: 894: 887: 880: 873: 866: 859: 852: 845: 838: 831: 824: 822: 821: 818:Downloadable 815: 811: 810: 801: 796: 791: 786: 781: 776: 771: 766: 761: 756: 751: 746: 738: 736: 735: 731: 727: 723: 719: 715: 706: 704: 703: 700: 696: 692: 688: 677: 671: 663: 659: 655: 651: 650: 643: 637: 633: 629: 625: 621: 613: 611: 609: 605: 601: 597: 594: 590: 583: 581: 580: 576: 572: 568: 565: 557: 555: 554: 550: 546: 542: 538: 530: 528: 527: 523: 519: 518:RockMagnetist 515: 511: 507: 500: 489: 487: 486: 482: 478: 473: 469: 467: 463: 462:Carboniferous 458: 454: 451: 447: 443: 439: 435: 431: 427: 423: 422:Carboniferous 414: 412: 411: 408: 407: 400: 395: 393: 389: 385: 380: 378: 374: 367: 356: 350: 346: 342: 337: 334: 330: 326: 322: 318: 314: 310: 306: 302: 298: 295: 291: 286: 281: 277: 276: 275: 272: 269: 265: 259: 254: 250: 246: 241: 236: 235: 234: 233: 229: 225: 221: 217: 211: 209: 208:User:Smith609 200: 196: 193: 190: 186: 180: 177: 176: 175: 168: 153: 152: 145: 144: 141: 124: 120: 116: 115: 110: 104: 98: 93: 91: 88: 84: 83: 79: 75: 70: 67: 64: 60: 55: 51: 45: 41: 37: 28: 27: 19: 949: 924: 918: 817: 806: 804: 710: 670:cite journal 653: 647: 617: 598: 595: 591: 587: 571:Dudley Miles 561: 534: 504:banner. See 493: 474: 470: 459: 455: 418: 402: 396: 381: 373:Wealden Lake 360: 260: 239: 212: 204: 181: 172: 149: 123:project page 112: 108: 50:WikiProjects 40:project page 39: 464:and in the 426:Phanerozoic 329:Pleistocene 111:is part of 965:Categories 952:Silica Cat 933:JavaRogers 722:Benniboi01 714:Quaternary 564:Cryogenian 477:Geopersona 466:Ordovician 430:Palaeozoic 341:Woodwalker 303:About the 224:Woodwalker 169:Subperiods 628:Paleozoic 377:Zealandia 317:Oligocene 309:Paleocene 294:Messinian 216:Tommotian 730:contribs 632:Mesozoic 624:Triassic 610:Wavery2 545:Marasama 537:Jurassic 438:Cenozoic 434:Mesozoic 399:Grutness 397:Cheers, 333:Holocene 325:Pliocene 305:Cenozoic 285:This one 264:Smith609 253:Cambrian 185:Smith609 699:Lambiam 620:Permian 600:Wavery2 475:cheers 321:Miocene 128:Geology 119:geology 74:Periods 69:Geology 446:series 442:epochs 392:WP:SFD 313:Eocene 258:Martin 240:within 179:Martin 46:scale. 38:This 16:< 956:talk 937:talk 931:) —— 925:See 829:PreꞒ 820:here 814:CGMW 807:See 745:PreꞒ 726:talk 676:link 649:PNAS 604:talk 575:talk 549:talk 522:talk 481:talk 432:and 405:wha? 345:talk 331:and 268:Talk 247:and 228:talk 189:Talk 658:doi 654:111 401:... 394:. 967:: 939:) 795:Pg 732:) 728:• 672:}} 668:{{ 652:. 630:, 626:, 622:, 606:) 577:) 551:) 524:) 516:. 502:}} 496:{{ 483:) 375:, 369:}} 363:{{ 347:) 327:, 323:, 319:, 315:, 311:, 266:– 230:) 187:– 72:: 954:( 935:( 912:N 902:G 900:P 892:K 885:J 878:T 871:P 864:C 857:D 850:S 843:O 836:Ꞓ 800:N 790:K 785:J 780:T 775:P 770:C 765:D 760:S 755:O 750:Ꞓ 724:( 678:) 664:. 660:: 602:( 573:( 547:( 520:( 479:( 343:( 270:) 262:( 226:( 191:) 183:( 154:. 52::

Index

Knowledge talk:WikiProject Geology
content assessment
WikiProjects
WikiProject icon
Geology
Periods
WikiProject icon
icon
Geology portal
WikiProject Geology
geology
project page
the Geological periods task force
Martin
Smith609
Talk
19:22, 25 July 2008 (UTC)
User:Smith609
Tommotian
my earlier comments
Woodwalker
talk
12:13, 26 October 2008 (UTC)
Cambrian explosion
small shelly fauna
Cambrian
Martin
Smith609
Talk
15:07, 26 October 2008 (UTC)

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