What is funny about my post with a number of published science papers showing higher sea levels earlier in the Holocene?
It's anecdotal. Duih.
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The papers?
Here are more you plan to ignore?
Marwick et al., 2017 (
full paper) Thailand,
+4 to +5 m higher than present
“Sinsakul (1992) has summarised 56 radiocarbon dates of shell and peat from beach and tidal locations to estimate a Holocene sea level curve for peninsula Thailand that starts with a steady rise in sea level until about 6 k BP, reaching a height of +4 m amsl (above [present]mean sea level). Sea levels then regressed until 4.7 k BP, then rising again to 2.5 m amsl at about 4 k BP. From 3.7 k to 2.7 k BP there was a regressive phase, with transgression starting again at 2.7 k BP to a maximum of 2 m amsl at 2.5 k BP. Regression continued from that time until the present sea levels were reached at 1.5 k BP. … Tjia (1996) collected over 130 radiocarbon ages from geological deposits of shell in abrasion platforms, sea-level notches and oyster beds and identified a +5 m [above present] highstand at ca. 5 k BP in the Thai-Malay Peninsula. … Sathiamurthy and Voris (2006) summarise the evidence described above as indicating that between 6 and 4.2 k BP, the sea level rose from 0 m to +5 m [above present] along the Sunda Shelf [+2.8 mm/yr], marking the regional mid-Holocene highstand. Following this highstand, the sea level fell gradually and reached the modern level at about 1 k BP.”
and,
Jiang et al., 2017 Southern China, +2.4 to +4.26 m higher than present
“[T]hree coastal sediments with 4 m, 3.7 m, and 2 m higher than present sea-level were deposited at 2.40 ± 0.05 ka, 2.92 ± 0.17 ka, and 4.26 ± 0.10 ka, respectively [2,400, 2,920, and 4,260 years before present], which indicate that the height of highstand relative sea-level are higher than both mean global sea-level eustacy and those records offshore southern China. … In conclusion, a beach ridge and two marine terraces sediments have been dated at eastern Hainan Island. They were well bleached and can be taken as good indicators of paleo-RSL [relative sea level] highstand records of late Holocene. Three highstand RSL [relative sea level] events occurred at 0.02-0.05 ka [200-500 years ago], 2.40-2.92 ka [2,400 to 2,920 years ago] and ~4.26 ka [4,260 years ago] with the sea-level heights of 0.5-1.5 m, 4 m, 3.7-4.0 m and 2 m [above present levels],respectively. The height of highstand RSLs are higher than both mean global sea-level euastacy and those of offshore southern China.”
and,
Khan et al., 2017 Caribbean, ~+1 m above present (rate: 1.09 meters per century)
“Only Suriname and Guyana [Caribbean] exhibited higher RSL[relative sea level] than present (82% probability), reaching a maximum height of ∼1 m [above present] at 5.2 ka [5,200 years ago]. … Because of meltwater input, the rates of RSL [relative sea level] change were highest during the early Holocene, with a maximum of 10.9 ± 0.6 m/ka [1.09 meters per century] in Suriname and Guyana and minimum of 7.4 ± 0.7 m/ka [0.74 meters per century] in south Florida from 12 to 8 ka [12,000 to 8,000 years ago].”
and,
Sander et al., 2016 Denmark, +2.2 m higher than present
“The data show a period of RSL [relative sea level] highstand at c. 2.2 m above present MSL [mean sea level] between c. 5.0 and 4.0 ka BP [5,000 to 4,000 years before present]. “
and,
Long et al., 2016 Scotland, < +1 m higher than present
“RSL [relative sea level] data from Loch Eriboll and the Wick River Valley show that RSL [relative sea level] was <1 m above present for several thousand years during the mid and late Holocene before it fell to present.”
and,
Lokier et al., 2015 Persian Gulf, > +1 m above present
“Mid-Holocene transgression of the Gulf surpassed today’s sea level by 7100–6890 cal yr BP [~7000 years ago], attaining a highstand of > 1 m above current sea level shortly after 5290–4570 cal yr BP before falling back to current levels by 1440–1170 cal yr BP. These new ages refine previously reported timings for the mid- to late Holocene sea-level highstand published for other regions.”
and,
Stategger et al., 2013 South Vietnam, +1.4 m higher than present
“The rates of sea-level rise decreased sharply after the rapid early Holocene rise and stabilized at a rate of 4.5 mm/year between 8.0 and 6.9 ka. Southeast Vietnam beachrocks reveal that the mid-Holocene sea-level highstand slightly above +1.4 m was reached between 6.7 and 5.0 ka, with a peak value close to +1.5 m around 6.0 ka.”
and,
Carson, 2011 Guam, Western Pacific, +1.5 to +2 m higher than present
“The case study in Guam may be viewed as representative of a broader region of the Remote Oceanic islands in the western Pacific, where first human settlement occurred around 1500-1000 B.C. (Bellwood, 1997; Kirch, 2000, 2010; Spriggs, 2007), generally at sites that today are broad sandy beaches but once had been small offshore islets, sand berms or spits, narrow beach fringes, and strand-like swampy settings around the end of a mid-Holocene highstand of sea level about 1.5-2 m above the present level (Carson, 2008a, 2008b; Dickinson and Burley, 2007; Gosden and Webb, 1994; Kirch, 1997; Nunn, 2005, 2007; Wickler, 2001).”
and,
Wündsch et al., 2018 South Africa, +3 m higher than present
“Holocene sea level reconstructions suggest a reduction of the speed of the sea level rise during this time [~7900–6400 cal BP]. The sea level likely reached and exceeded the height of the PSL [present sea level] by as much as 3 m .”
Is that enough for you?
Now have covered many nations coastlines in my two paper filled postings.
I have a lot more.
Your new, and apparently Bury-em-with BS (
Probably PLAGIARIZED from some denier Blog. ) reply, does NOT change my last post Porking your Link Dumps.
It's anecdotal/local and omits/ignores ie, tectonic/subsidence forces. Duh.
What is clear is sea level is rising GLOBALLY Now, and at an increasing rate.
(And of course, the OP claim was for Miami and S-E, and it's relatively faster rate)
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You are a truly stupid man, because I have a VISIBLE link for every single paper I posted, it is right there in front of you!
Here is the very first paper I posted, that you never read and will show that you are a close minded fool:
Holocene relative sea-level changes inferred from multiple proxies on the west coast of South Korea
Abstract
Understanding past relative sea-level (RSL) changes is crucial for predicting future coastal evolution, particularly within the context of accelerated melting of polar
ice sheets due to
global warming. RSL records are scarce in many regions along the Pacific coast. Here, we present a
Holocene RSL curve for the west coast of South Korea based on detailed analyses of four
sediment cores and the synthesis of existing sea-level index points without correction by tectonic, sediment compaction and other effects.
Our record shows that the local sea level rose rapidly during the early Holocene and then fell gradually toward the present position during the late Holocene. An apparent sea-level highstand of ca. 1–2 m occurred 7–4 cal kyr B.P. A rapid
sea-level rise of ~1.4 cm yr−1 during the early Holocene is a manifestation of polar ice sheet decay, while the apparent mid-Holocene sea-level highstand appears to be a signal of the hydro-isostasy of the
far-field continental shelf. The result was confirmed by a glacial isostatic adjustment (GIA) model. Holocene RSL change on the west coast of South Korea was closely linked to global temperature and ice sheet decay, especially during the early Holocene. There is a close relationship between
sea-level change in the study area and
Laurentide Ice Sheet (LIS) decay."
bolding mine